{"pageNumber":"6774","pageRowStart":"169325","pageSize":"25","recordCount":184863,"records":[{"id":70010572,"text":"70010572 - 1962 - Elastic constants of calcite","interactions":[],"lastModifiedDate":"2020-09-17T19:49:47.39236","indexId":"70010572","displayToPublicDate":"1962-01-01T00:00:00","publicationYear":"1962","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2171,"text":"Journal of Applied Physics","active":true,"publicationSubtype":{"id":10}},"title":"Elastic constants of calcite","docAbstract":"
The recent measurements of the elastic constants of calcite by Reddy and Subrahmanyam (1960) disagree with the values obtained independently by Voigt (1910) and Bhimasenachar (1945). The present authors, using an ultrasonic pulse technique at 3 Mc and 25°C, determined the elastic constants of calcite using the exact equations governing the wave velocities in the single crystal. The results are C11=13.7, C33=8.11, C44=3.50, C12=4.82, C13=5.68, and C14=−2.00, in units of 1011 dyn/cm2. Independent checks of several of the elastic constants were made employing other directions and polarizations of the wave velocities. With the exception of C13, these values substantially agree with the data of Voigt and Bhimasenachar.

","language":"English","publisher":"American Institute of Physics","doi":"10.1063/1.1702572","issn":"00214922","usgsCitation":"Peselnick, L., and Robie, R.A., 1962, Elastic constants of calcite: Journal of Applied Physics, v. 33, no. 9, p. 2889-2892, https://doi.org/10.1063/1.1702572.","productDescription":"4 p.","startPage":"2889","endPage":"2892","numberOfPages":"4","costCenters":[],"links":[{"id":480375,"rank":1,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1063/1.1702572","text":"Publisher Index Page"},{"id":219020,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"33","issue":"9","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a0880e4b0c8380cd51b4b","contributors":{"authors":[{"text":"Peselnick, L.","contributorId":66825,"corporation":false,"usgs":true,"family":"Peselnick","given":"L.","affiliations":[],"preferred":false,"id":359200,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Robie, R. A.","contributorId":71237,"corporation":false,"usgs":true,"family":"Robie","given":"R.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":359201,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":2002594,"text":"2002594 - 1962 - Common parasites of fishes","interactions":[],"lastModifiedDate":"2012-02-02T00:15:03","indexId":"2002594","displayToPublicDate":"1962-01-01T00:00:00","publicationYear":"1962","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":1,"text":"Federal Government Series"},"seriesTitle":{"id":14,"text":"Circular","active":false,"publicationSubtype":{"id":1}},"seriesNumber":"144","title":"Common parasites of fishes","docAbstract":"No abstract available at this time","language":"English","publisher":"U.S. Fish and Wildlife Service","collaboration":"113/FH","usgsCitation":"Hoffman, G.L., and Sindermann, C., 1962, Common parasites of fishes: Circular 144, 17 p.","productDescription":"17 p.","startPage":"0","endPage":"17","numberOfPages":"17","costCenters":[{"id":365,"text":"Leetown Science Center","active":true,"usgs":true}],"links":[{"id":198226,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":91854,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://www.archive.org/details/fisherycircular144unit","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b24e4b07f02db6ae5e6","contributors":{"authors":[{"text":"Hoffman, G. L.","contributorId":70713,"corporation":false,"usgs":true,"family":"Hoffman","given":"G.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":326624,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Sindermann, C.J.","contributorId":106603,"corporation":false,"usgs":true,"family":"Sindermann","given":"C.J.","email":"","affiliations":[],"preferred":false,"id":326625,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":2000020,"text":"2000020 - 1962 - A photoelectric amplifier as a dye detector","interactions":[],"lastModifiedDate":"2013-01-28T14:07:08","indexId":"2000020","displayToPublicDate":"1962-01-01T00:00:00","publicationYear":"1962","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":3,"text":"Organization Series"},"seriesTitle":{"id":222,"text":"Technical Report","active":false,"publicationSubtype":{"id":3}},"seriesNumber":"4","title":"A photoelectric amplifier as a dye detector","docAbstract":"A dye detector, based on a modified photoelectric amplifier, has been planned, built, and tested. It was designed to record automatically the time of arrival of fluorescein dye at predetermined points in a stream system. Laboratory tests and stream trials proved the instrument to be efficient. Small changes in color can be detected in turbid or clear water. The unit has been used successfully for timing intervals of more than 17 hours; significant savings of time and manpower have resulted. Replacement of the clock, included in the original device, with a recording milliammeter increases the efficiency of the unit by contin,!ously recording changes in turbidity. The addition of this component would increase the cost from $75 to approximately $105.","language":"English","publisher":"Great Lakes Fishery Commission","usgsCitation":"Ebel, W.J., 1962, A photoelectric amplifier as a dye detector: Technical Report 4, p. 19-26.","productDescription":"p. 19-26","startPage":"19","endPage":"26","numberOfPages":"8","costCenters":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"links":[{"id":198043,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":92069,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://www.glfc.org/pubs/TechReports/Tr04.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1fe4b07f02db6ab801","contributors":{"authors":[{"text":"Ebel, Wesley J.","contributorId":88307,"corporation":false,"usgs":true,"family":"Ebel","given":"Wesley","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":324938,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":2000037,"text":"2000037 - 1962 - Estimation of the brook and sea lamprey ammocoete populations of three streams","interactions":[],"lastModifiedDate":"2023-04-07T15:33:11.106821","indexId":"2000037","displayToPublicDate":"1962-01-01T00:00:00","publicationYear":"1962","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":3,"text":"Organization Series"},"seriesTitle":{"id":222,"text":"Technical Report","active":false,"publicationSubtype":{"id":3}},"seriesNumber":"4","title":"Estimation of the brook and sea lamprey ammocoete populations of three streams","docAbstract":"

Marking experiments on three streams in the Upper Peninsula of Michigan yielded quantitative estimates of populations of larval and transforming lampreys. The estimates not only gave an idea as to the numbers of ammocetes in the streams, but also confirmed the judgments of abundance based on earlier surveys with electric-shocking equipment and provided valuable information on the movement of larvae during chemical treatment. The estimated numbers of ammocetes in the three streams were 4,300 in Furnace Creek, 30,600 in Snyder Creek, and 336,700 in the Ogontz River.

","language":"English","publisher":"Great Lakes Fishery Commission","usgsCitation":"Smith, B.R., and McLain, A.L., 1962, Estimation of the brook and sea lamprey ammocoete populations of three streams: Technical Report 4, 18 p.","productDescription":"18 p.","costCenters":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"links":[{"id":198781,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":92071,"rank":2,"type":{"id":15,"text":"Index Page"},"url":"https://www.glfc.org/glfc-publications-reports.php","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Michigan","otherGeospatial":"Furnace Creek, Ogontz River, Snyder Creek, Upper Peninisula","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -86.9103521098381,\n 46.47603146409622\n ],\n [\n -86.9103521098381,\n 45.750180380916646\n ],\n [\n -86.25593446454421,\n 45.750180380916646\n ],\n [\n -86.25593446454421,\n 46.47603146409622\n ],\n [\n -86.9103521098381,\n 46.47603146409622\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ae4b07f02db5fb1e2","contributors":{"authors":[{"text":"Smith, Bernard R.","contributorId":38924,"corporation":false,"usgs":true,"family":"Smith","given":"Bernard","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":324966,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"McLain, Alberton L.","contributorId":15561,"corporation":false,"usgs":true,"family":"McLain","given":"Alberton","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":324965,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":2000024,"text":"2000024 - 1962 - Collection and analysis of commercial fishery statistics in the Great Lakes","interactions":[],"lastModifiedDate":"2023-04-07T14:55:19.462398","indexId":"2000024","displayToPublicDate":"1962-01-01T00:00:00","publicationYear":"1962","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":3,"text":"Organization Series"},"seriesTitle":{"id":222,"text":"Technical Report","active":false,"publicationSubtype":{"id":3}},"seriesNumber":"5","title":"Collection and analysis of commercial fishery statistics in the Great Lakes","docAbstract":"

No abstract available.

","language":"English","publisher":"Great Lakes Fishery Commission","usgsCitation":"Hile, R., 1962, Collection and analysis of commercial fishery statistics in the Great Lakes: Technical Report 5, ii, 31 p.","productDescription":"ii, 31 p.","costCenters":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"links":[{"id":198622,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":92070,"rank":2,"type":{"id":15,"text":"Index Page"},"url":"https://www.glfc.org/glfc-publications-reports.php","linkFileType":{"id":5,"text":"html"}}],"country":"Canada, United States","otherGeospatial":"Great Lakes","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -75.91552734375,\n 44.28453670601888\n ],\n [\n -76.4813232421875,\n 44.319918120477425\n ],\n [\n -77.113037109375,\n 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States","interactions":[],"lastModifiedDate":"2020-11-19T17:17:10.952456","indexId":"70010465","displayToPublicDate":"1962-01-01T00:00:00","publicationYear":"1962","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1759,"text":"Geochimica et Cosmochimica Acta","active":true,"publicationSubtype":{"id":10}},"title":"K/Na ratio of Cenozoic igneous rocks of the western United States","docAbstract":"

The potassium and sodium content of chemically analysed Cenozoic igneous rocks from about 150 areas of the western United States has been examined. For each area a plot of the molecular proportion K2O(K2O + Na2O)\">K2O(K2O + Na2O) [Niggli's k-value] is shown, and the projected k-value determined at 50 and 60 weight per cent SiO2. The k-values are plotted and contoured on maps of the western United States.

These maps show that potassium is least abundant relative to total alkali (when rocks of the same SiO2 content are compared) in a zone along the Pacific Coast, becomes more abundant eastward, and is highest in the Colorado Plateau and Northern Rocky Mountains.

These k-value variations can be related to regional variations in the abundance of certain trace elements and of different types of older granitic rocks, and to Bouguer gravity maps. This correspondence indicates that the alkali ratio of Cenozoic igneous rocks is closely related to the character of the crust where the rocks are formed.

","language":"English","publisher":"Elsevier","doi":"10.1016/0016-7037(62)90009-1","usgsCitation":"Moore, J., 1962, K/Na ratio of Cenozoic igneous rocks of the western United States: Geochimica et Cosmochimica Acta, v. 26, no. 1, p. 101-130, https://doi.org/10.1016/0016-7037(62)90009-1.","productDescription":"30 p.","startPage":"101","endPage":"130","numberOfPages":"30","costCenters":[],"links":[{"id":219009,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Arizona, California, Colorado, Idaho, Montana, Nevada, New Mexico, Oregon, Texas, Utah, Washington, Wyoming","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -94.04296874999999,\n 29.84064389983441\n ],\n [\n -94.2626953125,\n 33.61461929233378\n ],\n [\n -99.931640625,\n 34.74161249883172\n ],\n [\n -100.283203125,\n 36.491973470593685\n ],\n [\n -102.919921875,\n 36.59788913307022\n ],\n [\n -102.9638671875,\n 37.09023980307208\n ],\n [\n -102.1728515625,\n 37.09023980307208\n ],\n [\n -102.1728515625,\n 41.0130657870063\n ],\n [\n -104.1064453125,\n 41.1455697310095\n ],\n [\n -104.23828125,\n 48.951366470947725\n ],\n [\n -123.22265625000001,\n 48.980216985374994\n ],\n [\n -122.87109375,\n 48.16608541901253\n ],\n [\n -124.892578125,\n 48.28319289548349\n ],\n [\n -124.27734374999999,\n 45.49094569262732\n ],\n [\n -124.76074218749999,\n 42.391008609205045\n ],\n [\n -124.76074218749999,\n 40.58058466412761\n ],\n [\n -120.10253906249999,\n 34.161818161230386\n ],\n [\n -117.158203125,\n 32.43561304116276\n ],\n [\n -115.13671875,\n 32.731840896865684\n ],\n [\n -114.7412109375,\n 32.509761735919426\n ],\n [\n -111.3134765625,\n 31.353636941500987\n ],\n [\n -108.1494140625,\n 31.42866311735861\n ],\n [\n -108.19335937499999,\n 31.728167146023935\n ],\n [\n -106.6552734375,\n 31.690781806136822\n ],\n [\n -104.32617187499999,\n 29.726222319395504\n ],\n [\n -103.53515625,\n 28.844673680771795\n ],\n [\n -102.4365234375,\n 29.726222319395504\n ],\n [\n -101.3818359375,\n 29.6880527498568\n ],\n [\n -100.1953125,\n 28.265682390146477\n ],\n [\n -99.228515625,\n 26.902476886279832\n ],\n [\n -97.20703125,\n 25.958044673317843\n ],\n [\n -97.42675781249999,\n 27.488781168937997\n ],\n [\n -95.80078125,\n 28.806173508854776\n ],\n [\n -94.04296874999999,\n 29.84064389983441\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"26","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a4044e4b0c8380cd64c1f","contributors":{"authors":[{"text":"Moore, J.G.","contributorId":67496,"corporation":false,"usgs":true,"family":"Moore","given":"J.G.","email":"","affiliations":[],"preferred":false,"id":358985,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70010448,"text":"70010448 - 1962 - The solubility of quartz in water in the temperature interval from 25° to 300° C","interactions":[],"lastModifiedDate":"2015-06-22T09:01:28","indexId":"70010448","displayToPublicDate":"1962-01-01T00:00:00","publicationYear":"1962","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1759,"text":"Geochimica et Cosmochimica Acta","active":true,"publicationSubtype":{"id":10}},"title":"The solubility of quartz in water in the temperature interval from 25° to 300° C","docAbstract":"

The solubility of quartz in water was investigated by three sets of experiments

\n
    \n
  1. at 1000 atm PH2O and temperatures ranging from 45° to 300°C
    2. \n
  2. at water pressures appropriate for the coexistence of three phases, gaseous water, liquid, and quartz, at temperatures ranging from 69° to 240°C
    3. \n
  3. a long term study of the dissolution of quartz grains which were continuously tumbled in water at room temperature.
    4. \n
\n

Saturated silica solutions in equilibrium with quartz were obtained in a few days at temperatures above 100°C. Equilibrium is shown by reproducible results for runs of different durations and by the precipitation of quartz from initially supersaturated solutions. The differential heat of solution derived from the data obtained at 1000 atm pressure is 5.38 kcal/mole.

\n

At room temperature and pressure, highly supersaturated silica solutions were obtained by continuously rotating quartz grains and water in plastic bottles at 75 rev/min. In one run the amount of silica in solution increased to a maximum value of 395 p.p.m. after 370 days. Another run reached 80 p.p.m. silica after 386 days and then dropped to 6 p.p.m. silica. It is concluded that quartz was precipitated at room temperature from this supersaturated solution and that 6 p.p.m. is essentially the true solubility of quartz at 25°C.

\n

In contrast to the runs rotated at 75 rev/min, quartz grains, and also silica glass grains, continuously rotated in water at\"\" rev/min, each contributed less than 1 p.p.m. colorimetric silica into solution after 1 year. Thus, vigorous agitation of the liquid is necessary to remove dissolved silica from the vicinity of surfaces of both quartz and glass.

\n

Two significant factors that may have contributed to the formation of supersaturated silica solutions in the runs rotated at 75 rev/min at room temperature are

\n
    \n
  1. stresses and structural irregularities at the surfaces of the crushed quartz grains, which contributed silica into solution more readily than well crystallized quartz
    2. \n
  2. the very slow rate at which dissolved silica polymerizes to species appropriate to act as nuclei for quartz growth. At the termination of the runs rotated at 75 rev/min, spikelike projections were present on many of the quartz grains. These are interpreted as indicating that abrasion was not the dominant cause for the great supersaturations which were obtained.
    3. \n
\n

 

","language":"English","publisher":"Elsevier","doi":"10.1016/0016-7037(62)90027-3","issn":"00167037","usgsCitation":"Morey, G., Fournier, R., and Rowe, J., 1962, The solubility of quartz in water in the temperature interval from 25° to 300° C: Geochimica et Cosmochimica Acta, v. 26, no. 10, p. 1029-1040, https://doi.org/10.1016/0016-7037(62)90027-3.","productDescription":"12 p.","startPage":"1029","endPage":"1040","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":218798,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"26","issue":"10","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bb043e4b08c986b324d40","contributors":{"authors":[{"text":"Morey, G.W.","contributorId":108155,"corporation":false,"usgs":true,"family":"Morey","given":"G.W.","email":"","affiliations":[],"preferred":false,"id":358950,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Fournier, R.O.","contributorId":73584,"corporation":false,"usgs":true,"family":"Fournier","given":"R.O.","email":"","affiliations":[],"preferred":false,"id":358949,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Rowe, J.J.","contributorId":29460,"corporation":false,"usgs":true,"family":"Rowe","given":"J.J.","affiliations":[],"preferred":false,"id":358948,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70010449,"text":"70010449 - 1962 - The effect of CO2 at low temperature and pressure on solutions supersaturated with silica in the presence of limestone and dolomite","interactions":[],"lastModifiedDate":"2020-09-09T13:52:34.253102","indexId":"70010449","displayToPublicDate":"1962-01-01T00:00:00","publicationYear":"1962","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1759,"text":"Geochimica et Cosmochimica Acta","active":true,"publicationSubtype":{"id":10}},"displayTitle":"The effect of CO2 at low temperature and pressure on solutions supersaturated with silica in the presence of limestone and dolomite","title":"The effect of CO2 at low temperature and pressure on solutions supersaturated with silica in the presence of limestone and dolomite","docAbstract":"

The effect of 1 atm of CO2 over initially neutral solutions supersaturated with silica, at room temperature, as contrasted with 1 atm of air was determined over a period of 5 months, together with changes brought about by the introduction of calcite and dolomite to these solutions in the form of either chips or finely ground powder. In the absence of CO2 all solutions quickly reached equilibrium and no silica precipitated. In the presence of CO2 approximately two-thirds of the silica precipitated as silica gel within the first 2 months; the amount of silica precipitated was not affected by the presence of limestone or dolomite. Silica gel precipitated as a fine powder in the presence of finely ground calcite and dolomite, but as a cloudy gelatinous mass in the presence of coarse chips of dolomite and calcite, and in the absence of either calcite or dolomite. Preferential leaching of calcium from dolomite took place, both in the presence of air and in the presence of CO2, but was more pronounced in the presence of air. There was no evidence of physical replacement of either limestone or dolomite by precipitated silica.

","language":"English","publisher":"Elsevier","doi":"10.1016/0016-7037(62)90039-X","usgsCitation":"Lovering, T., and Patten, L., 1962, The effect of CO2 at low temperature and pressure on solutions supersaturated with silica in the presence of limestone and dolomite: Geochimica et Cosmochimica Acta, v. 26, no. 7, p. 787-796, https://doi.org/10.1016/0016-7037(62)90039-X.","productDescription":"12 p.","startPage":"787","endPage":"796","costCenters":[],"links":[{"id":218799,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"26","issue":"7","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bab0fe4b08c986b322bb5","contributors":{"authors":[{"text":"Lovering, T.G.","contributorId":55014,"corporation":false,"usgs":true,"family":"Lovering","given":"T.G.","affiliations":[],"preferred":false,"id":358952,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Patten, L.E.","contributorId":34257,"corporation":false,"usgs":true,"family":"Patten","given":"L.E.","email":"","affiliations":[],"preferred":false,"id":358951,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70010794,"text":"70010794 - 1962 - Aromatic fluorine compounds. X. The 2,3- and 2,6-difluoropyridines","interactions":[],"lastModifiedDate":"2020-11-19T17:43:15.215708","indexId":"70010794","displayToPublicDate":"1962-01-01T00:00:00","publicationYear":"1962","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2408,"text":"Journal of Organic Chemistry","active":true,"publicationSubtype":{"id":10}},"title":"Aromatic fluorine compounds. X. The 2,3- and 2,6-difluoropyridines","docAbstract":"

The preparation of difluoropyridines by the Schiemann reaction was investigated. 2-Amino-6-fluoropyridine (IIIa), necessary for the synthesis of 2,6-difluoropyridine (IVa) by the Schiemann reaction, was conveniently prepared by the Curtius degradation of 6-fluoropicolinic hydrazide (IIa) and by the Hofmann reaction on 6-fluoropicolinamide (IId). Since an α-fluorine on a pyridine nucleus is preferentially replaced by hydrazine when it is either adjacent to or opposite a carbomethoxy group, the hydrazides necessary for the synthesis of 3-amino-2- and 6-fluoropyridine could not be prepared. These amines were prepared from the appropriate 2-fluoropyridinecarboxamide by the Hofmann reaction. The preparation of difluoropyridines was successful with two of the aminofluoropyridines and led to the following new compounds: 2,3-difluoro(IVb) and 2,6-difluoropyridine (IVa).

","language":"English","publisher":"American Chemical Society","doi":"10.1021/jo01058a050","usgsCitation":"Finger, G.C., Starr, L.D., Roe, A., and Link, W.J., 1962, Aromatic fluorine compounds. X. The 2,3- and 2,6-difluoropyridines: Journal of Organic Chemistry, v. 27, no. 11, p. 3965-3968, https://doi.org/10.1021/jo01058a050.","productDescription":"4 p.","startPage":"3965","endPage":"3968","numberOfPages":"4","costCenters":[],"links":[{"id":218734,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"27","issue":"11","noUsgsAuthors":false,"publicationDate":"2002-05-01","publicationStatus":"PW","scienceBaseUri":"5059ed81e4b0c8380cd49851","contributors":{"authors":[{"text":"Finger, G. C.","contributorId":89277,"corporation":false,"usgs":true,"family":"Finger","given":"G.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":359662,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Starr, L. D.","contributorId":74872,"corporation":false,"usgs":true,"family":"Starr","given":"L.","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":359660,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Roe, A.","contributorId":67214,"corporation":false,"usgs":true,"family":"Roe","given":"A.","email":"","affiliations":[],"preferred":false,"id":359659,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Link, W. J.","contributorId":76877,"corporation":false,"usgs":true,"family":"Link","given":"W.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":359661,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":70010492,"text":"70010492 - 1962 - Kerogen in the Chattanooga shale","interactions":[],"lastModifiedDate":"2019-12-13T07:43:25","indexId":"70010492","displayToPublicDate":"1962-01-01T00:00:00","publicationYear":"1962","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3338,"text":"Science","active":true,"publicationSubtype":{"id":10}},"title":"Kerogen in the Chattanooga shale","docAbstract":"Study of its origin and composition suggests why these shales are not source beds for petroleum.","language":"English","publisher":"Science","doi":"10.1126/science.137.3525.221","issn":"00368075","usgsCitation":"Breger, I.A., and Brown, A., 1962, Kerogen in the Chattanooga shale: Science, v. 137, no. 3525, p. 221-224, https://doi.org/10.1126/science.137.3525.221.","productDescription":"4 p.","startPage":"221","endPage":"224","numberOfPages":"4","costCenters":[],"links":[{"id":219307,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"137","issue":"3525","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a4073e4b0c8380cd64d91","contributors":{"authors":[{"text":"Breger, Irving A.","contributorId":65205,"corporation":false,"usgs":true,"family":"Breger","given":"Irving","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":359053,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Brown, A.","contributorId":27825,"corporation":false,"usgs":true,"family":"Brown","given":"A.","affiliations":[],"preferred":false,"id":359052,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70010793,"text":"70010793 - 1962 - Spectrophotometric catalytic determination of small amounts of rhenium in mineralized rocks and molybdenite","interactions":[],"lastModifiedDate":"2020-11-19T17:21:51.495943","indexId":"70010793","displayToPublicDate":"1962-01-01T00:00:00","publicationYear":"1962","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":761,"text":"Analytical Chemistry","active":true,"publicationSubtype":{"id":10}},"title":"Spectrophotometric catalytic determination of small amounts of rhenium in mineralized rocks and molybdenite","docAbstract":"

Rhenium is determined by spectrophotometry of the tellurium sol formed by the reduction of tellurate by stannous chloride under the catalytic influence of rhenium. A detailed investigation of the conditions for high sensitivity and stability at lowest concentration levels of rhenium is presented as well as the behavior of 26 ions. The method is applied to the determination of some tenths of 1 p.p.m. or more of rhenium in a 1-mg. aliquot of mineralized rocks, mixtures of molybdenite and rocks, and molybdenite concentrates. The practical quantity limit of detection is 2x-10 gram of rhenium. Samples are decomposed with a mixture of CaO, CaCl2, and MgO. On leaching, most constituents of the sample are precipitated either as calcium salts or hydroxides, except for rhenium and a small amount of molybdenum which pass into the filtrate. Residual molybdenum is removed by extraction with 8-quinolinol in chloroform. Better than 95% recoveries are obtained with two fusions with flux.

","language":"English","publisher":"ACS Publications","doi":"10.1021/ac60191a003","usgsCitation":"Simon, F., and Grimaldi, F.S., 1962, Spectrophotometric catalytic determination of small amounts of rhenium in mineralized rocks and molybdenite: Analytical Chemistry, v. 34, no. 11, p. 1361-1364, https://doi.org/10.1021/ac60191a003.","productDescription":"4 p.","startPage":"1361","endPage":"1364","numberOfPages":"4","costCenters":[],"links":[{"id":218733,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"34","issue":"11","noUsgsAuthors":false,"publicationDate":"2002-05-01","publicationStatus":"PW","scienceBaseUri":"505b95a6e4b08c986b31b030","contributors":{"authors":[{"text":"Simon, F.O.","contributorId":41808,"corporation":false,"usgs":true,"family":"Simon","given":"F.O.","email":"","affiliations":[],"preferred":false,"id":359657,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Grimaldi, F. S.","contributorId":94286,"corporation":false,"usgs":true,"family":"Grimaldi","given":"F.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":359658,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70010571,"text":"70010571 - 1962 - Temperature dependence of decay time and intensity of alpha pulses in pure and thallium-activated cesium iodide","interactions":[],"lastModifiedDate":"2020-11-19T17:46:33.453266","indexId":"70010571","displayToPublicDate":"1962-01-01T00:00:00","publicationYear":"1962","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3276,"text":"Review of Scientific Instruments","active":true,"publicationSubtype":{"id":10}},"title":"Temperature dependence of decay time and intensity of alpha pulses in pure and thallium-activated cesium iodide","docAbstract":"

The intensity and decay time of Po210 alpha particle scintillations produced in pure and thallium‐activated cesium iodide have been measured with a fast electronic system as a function of temperature down to 77°K. Three modes of decay due to alpha excitation have been observed for CsI(Tl), and two for CsI. Other than the 7‐ and 0.55‐μsec modes (at room temperature) reported in the literature for CsI(Tl), an additional temperature‐independent mode of about 1.3 μsec has been detected between 77 and 150°K. In CsI a fast temperature‐dependent mode of decay (≈100 nsec) was observed between 100–200°K in addition to the known principal mode.

","language":"English","publisher":"AIP Publishing","doi":"10.1063/1.1717979","usgsCitation":"Senftle, F.E., Martinez, P., and Alekna, V.P., 1962, Temperature dependence of decay time and intensity of alpha pulses in pure and thallium-activated cesium iodide: Review of Scientific Instruments, v. 33, no. 8, p. 819-822, https://doi.org/10.1063/1.1717979.","productDescription":"4 p.","startPage":"819","endPage":"822","numberOfPages":"4","costCenters":[],"links":[{"id":219019,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"33","issue":"8","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505ba4c1e4b08c986b320570","contributors":{"authors":[{"text":"Senftle, F. E.","contributorId":47788,"corporation":false,"usgs":true,"family":"Senftle","given":"F.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":359199,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Martinez, P.","contributorId":38706,"corporation":false,"usgs":true,"family":"Martinez","given":"P.","email":"","affiliations":[],"preferred":false,"id":359198,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Alekna, V. P.","contributorId":35459,"corporation":false,"usgs":true,"family":"Alekna","given":"V.","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":359197,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70171161,"text":"70171161 - 1962 - Light penetration in the Great Lakes","interactions":[],"lastModifiedDate":"2016-05-24T10:43:55","indexId":"70171161","displayToPublicDate":"1962-01-01T00:00:00","publicationYear":"1962","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Light penetration in the Great Lakes","docAbstract":"

No abstract available.

","largerWorkType":{"id":24,"text":"Conference Paper"},"largerWorkTitle":"Proceedings of the 5th Conference on Great Lakes Research","largerWorkSubtype":{"id":19,"text":"Conference Paper"},"conferenceTitle":"5th Conference on Great Lakes Research","conferenceDate":"April 9-10, 1962","conferenceLocation":"Toronto, Canada","language":"English","publisher":"University of Michigan","usgsCitation":"Beeton, A.M., 1962, Light penetration in the Great Lakes, in Proceedings of the 5th Conference on Great Lakes Research, Toronto, Canada, April 9-10, 1962, p. 68-76.","productDescription":"9 p.","startPage":"68","endPage":"76","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"links":[{"id":321601,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"574d65a6e4b07e28b66845ef","contributors":{"authors":[{"text":"Beeton, Alfred M.","contributorId":94247,"corporation":false,"usgs":true,"family":"Beeton","given":"Alfred","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":630142,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70010450,"text":"70010450 - 1962 - Summary of new data on rock samples G-1 and W-1","interactions":[],"lastModifiedDate":"2020-11-19T17:11:56.64249","indexId":"70010450","displayToPublicDate":"1962-01-01T00:00:00","publicationYear":"1962","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1759,"text":"Geochimica et Cosmochimica Acta","active":true,"publicationSubtype":{"id":10}},"title":"Summary of new data on rock samples G-1 and W-1","docAbstract":"

Published and unpublished analyses for major and minor constituents that have become available since April, 1960, are collected for the granite G-1 and diabase W-1. “Best values” are suggested for some of the elements.

","language":"English","publisher":"Elsevier","doi":"10.1016/0016-7037(62)90103-5","usgsCitation":"Fleischer, M., and Stevens, R., 1962, Summary of new data on rock samples G-1 and W-1: Geochimica et Cosmochimica Acta, v. 26, no. 5, p. 525-543, https://doi.org/10.1016/0016-7037(62)90103-5.","productDescription":"19 p.","startPage":"525","endPage":"543","numberOfPages":"19","costCenters":[],"links":[{"id":218800,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"26","issue":"5","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505b9e9be4b08c986b31dffa","contributors":{"authors":[{"text":"Fleischer, M.","contributorId":84069,"corporation":false,"usgs":true,"family":"Fleischer","given":"M.","email":"","affiliations":[],"preferred":false,"id":358954,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Stevens, R.E.","contributorId":62954,"corporation":false,"usgs":true,"family":"Stevens","given":"R.E.","email":"","affiliations":[],"preferred":false,"id":358953,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70045415,"text":"wdrCO621 - 1962 - Surface Water Records of Colorado","interactions":[],"lastModifiedDate":"2013-05-22T14:43:50","indexId":"wdrCO621","displayToPublicDate":"1962-01-01T00:00:00","publicationYear":"1962","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":340,"text":"Water Data Report","code":"WDR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"CO-62-1","title":"Surface Water Records of Colorado","docAbstract":"The surface-water records for the 1962 water year for gaging stations and miscellaneous sites within the State of Colorado are given in this report. For convenience there are also included records for a few pertinent gaging stations in bordering States. The records were collected and computed by the Water Resources Division of the U.S. Geological Survey, under the direction of J. W. Odell, district engineer, Surface Water Branch.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Denver, CO","doi":"10.3133/wdrCO621","collaboration":"Prepared in cooperation with Colorado Water Conservation Board, Office of the State Engineer, Southeastern Colorado Water Conservancy District, Arkansas River Compact Administration, Colorado Agricultural Experiment Station, Colorado River Water Conservation District, County of Boulder, Board of County Cotmnissioners, City and County of Denver Board of Water Conunissioners, City of ·Colorado Springs Department of Public Utilities, U.S. Army Corps of Engineers, U.S. Bureau of Reclamation, U.S. Soil Conservation Service","usgsCitation":"U.S. Geological Survey, W.R., 1962, Surface Water Records of Colorado: U.S. Geological Survey Water Data Report CO-62-1, xii, 335 p., https://doi.org/10.3133/wdrCO621.","productDescription":"xii, 335 p.","numberOfPages":"356","additionalOnlineFiles":"N","temporalStart":"1961-10-01","temporalEnd":"1962-09-30","costCenters":[],"links":[{"id":272538,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wdr/1962/co-62/report.pdf"},{"id":270918,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wdr/1962/co-62/report-thumb.jpg"}],"country":"United States","state":"Colorado","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -109.000,37.0000 ], [ -109.000,41.0000 ], [ -102.000,41.0000 ], [ -102.000,37.0000 ], [ -109.000,37.0000 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"516d216ce4b0411d430a8a31","contributors":{"authors":[{"text":"U.S. Geological Survey, Water Resources Division","contributorId":102359,"corporation":false,"usgs":true,"family":"U.S. Geological Survey","given":"Water","email":"","middleInitial":"Resources Division","affiliations":[],"preferred":false,"id":477467,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70010718,"text":"70010718 - 1962 - Oxygen adsorption and the magnetic susceptibility of ice at low temperatures","interactions":[],"lastModifiedDate":"2020-11-19T17:48:20.117143","indexId":"70010718","displayToPublicDate":"1962-01-01T00:00:00","publicationYear":"1962","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2840,"text":"Nature","active":true,"publicationSubtype":{"id":10}},"title":"Oxygen adsorption and the magnetic susceptibility of ice at low temperatures","docAbstract":"

WHEN dealing with the magnetic susceptibility of tumour tissue1, we reported the magnetic susceptibility of ice at various temperatures from 273° K. down to 77° K. Since this publication, the authors have made many susceptibility measurements of ice, using the same equipment, and have obtained similar results, that is, a relatively large increase in diamagnetism below 150° K. Normal diamagnetism is not dependent on temperature, and hence further experiments were made of the magnetic susceptibility of ice at low temperatures in an attempt to determine some extraneous cause of the increased diamagnetism.

","language":"English","publisher":"Nature Publications","doi":"10.1038/194673a0","usgsCitation":"Senftle, F.E., and Thorpe, A., 1962, Oxygen adsorption and the magnetic susceptibility of ice at low temperatures: Nature, v. 194, no. 4829, p. 673-674, https://doi.org/10.1038/194673a0.","productDescription":"2 p.","startPage":"673","endPage":"674","numberOfPages":"2","costCenters":[],"links":[{"id":219552,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"194","issue":"4829","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a7277e4b0c8380cd76af6","contributors":{"authors":[{"text":"Senftle, F. E.","contributorId":47788,"corporation":false,"usgs":true,"family":"Senftle","given":"F.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":359484,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Thorpe, A.","contributorId":70534,"corporation":false,"usgs":true,"family":"Thorpe","given":"A.","affiliations":[],"preferred":false,"id":359485,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70010569,"text":"70010569 - 1962 - Study of natural glasses through their behaviour as membrane electrodes","interactions":[],"lastModifiedDate":"2020-11-19T17:49:37.931207","indexId":"70010569","displayToPublicDate":"1962-01-01T00:00:00","publicationYear":"1962","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2840,"text":"Nature","active":true,"publicationSubtype":{"id":10}},"title":"Study of natural glasses through their behaviour as membrane electrodes","docAbstract":"

THE low-temperature chemical alteration of natural glass occurs in two stages: an initial stage in which it remains glassy but absorbs as much as 6 per cent water1, and a final stage in which devitrification to clay minerals, with release of silica, occurs2,3. During the first stage the composition of the glass may change, with gain of K2O and water and loss of Na2O (Smith, R. L., personal communication). This change is due to ion exchange.

","language":"English","publisher":"Nature Publications","doi":"10.1038/194077b0","usgsCitation":"Truesdell, A., 1962, Study of natural glasses through their behaviour as membrane electrodes: Nature, v. 194, no. 4823, p. 77-79, https://doi.org/10.1038/194077b0.","productDescription":"3 p.","startPage":"77","endPage":"79","numberOfPages":"3","costCenters":[],"links":[{"id":218971,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"194","issue":"4823","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505b9cd8e4b08c986b31d4e3","contributors":{"authors":[{"text":"Truesdell, A.H.","contributorId":52566,"corporation":false,"usgs":false,"family":"Truesdell","given":"A.H.","email":"","affiliations":[{"id":6672,"text":"former: USGS Southwest Biological Science Center, Colorado Plateau Research Station, Flagstaff, AZ. Current address: TN-SCORE, Univ of Tennessee, Knoxville, TN, e-mail: jennen@gmail.com","active":true,"usgs":false}],"preferred":false,"id":359192,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":1017049,"text":"1017049 - 1962 - Dangers of electric fishing: precautions to take","interactions":[],"lastModifiedDate":"2012-02-02T00:04:34","indexId":"1017049","displayToPublicDate":"1962-01-01T00:00:00","publicationYear":"1962","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1091,"text":"Bulletin Francaise De Pisciculture","active":true,"publicationSubtype":{"id":10}},"title":"Dangers of electric fishing: precautions to take","docAbstract":"No abstract available at this time","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Bulletin Francaise De Pisciculture","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","collaboration":"123/FH","usgsCitation":"Cuinat, R., 1962, Dangers of electric fishing: precautions to take: Bulletin Francaise De Pisciculture, v. 204, p. 125-131.","productDescription":"p. 125-131","startPage":"125","endPage":"131","numberOfPages":"7","costCenters":[{"id":365,"text":"Leetown Science Center","active":true,"usgs":true}],"links":[{"id":132765,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"204","edition":"Translation","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4acce4b07f02db67e5e1","contributors":{"authors":[{"text":"Cuinat, R.","contributorId":37289,"corporation":false,"usgs":true,"family":"Cuinat","given":"R.","email":"","affiliations":[],"preferred":false,"id":324588,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70195893,"text":"70195893 - 1962 - Artesian water from glacial drift near Lehr, Logan and McIntosh Counties, North Dakota","interactions":[],"lastModifiedDate":"2018-03-08T09:28:58","indexId":"70195893","displayToPublicDate":"1962-01-01T00:00:00","publicationYear":"1962","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"seriesTitle":{"id":5646,"text":"North Dakota Ground Water Studies","active":true,"publicationSubtype":{"id":2}},"seriesNumber":"38","title":"Artesian water from glacial drift near Lehr, Logan and McIntosh Counties, North Dakota","docAbstract":"

No abstract available.

","language":"English","publisher":"North Dakota State Water Conservation Commission","usgsCitation":"Adolphson, D.G., 1962, Artesian water from glacial drift near Lehr, Logan and McIntosh Counties, North Dakota: North Dakota Ground Water Studies 38, 22 p.","productDescription":"22 p.","costCenters":[{"id":478,"text":"North Dakota Water Science Center","active":true,"usgs":true},{"id":34685,"text":"Dakota Water Science Center","active":true,"usgs":true}],"links":[{"id":352287,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5aff6345e4b0da30c1bfdf0a","contributors":{"authors":[{"text":"Adolphson, D. G.","contributorId":106081,"corporation":false,"usgs":true,"family":"Adolphson","given":"D.","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":730411,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70190791,"text":"70190791 - 1962 - Records of selected wells and springs, selected drillers' logs of wells, and chemical analyses of ground and surface waters, northern Utah Valley, Utah County, Utah","interactions":[],"lastModifiedDate":"2017-09-14T11:00:56","indexId":"70190791","displayToPublicDate":"1962-01-01T00:00:00","publicationYear":"1962","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"seriesTitle":{"id":5497,"text":"Utah Basic-Data Report","active":false,"publicationSubtype":{"id":2}},"seriesNumber":"2","title":"Records of selected wells and springs, selected drillers' logs of wells, and chemical analyses of ground and surface waters, northern Utah Valley, Utah County, Utah","docAbstract":"

This report is intended to serve two purposes: (1) to make available to the public basic ground-water data useful in planning and studying development of water resources and (2) to supplement an interpretive report that will be published later.

Records were collected during the period 1956-59 by the U.S. Geological Survey in cooperation with the Utah State Engineer as a part of the investigation of the ground-water resources of northern Utah Walley in Utah County, Utah. Some earlier data and other information in the tables are from published reports on the ground-water resources of northern Utah Walley. The interpretive material will be published cooperatively by the U.S. Geological Survey and the Utah State Engineer in a companion report by Seymour Subitzky.

This report is most useful in predicting conditions likely to be found in areas that are being considered as well sites. The person considering the new well can spot the proposed site on plate 1 and examine the records of nearby wells as shown on the tables. From tables 1, 2, and h he can note the type of material that yields water to wells in the vicinity; from table 2 he can note (1) the depth and diameter of wells in the vicinity and the yield of some of those wells, and (2) the depth to water or the feet of water pressure in the vicinity; from table 3 and plate 1 he may note the location of springs and the conditions related to the occurrence of these springs; and from tables 5 and 6 he may note the chemical quality of the water from wells and from some surface sources, and the uses of these waters. If the reader decides from his examination that conditions are favorable, he may place an application to drill a well with the State Engineer. If the State Engineer believes unappropriated water is available, the application may be approved after minimum statutory requirements have been satisfied.

The report is also useful when planning large-scale developments of water supply. This and other uses of the report will be helped by use of the interpretive report upon its release.

","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Salt Lake City, UT","collaboration":"Prepared in cooperation with the Utah State Engineer","usgsCitation":"Subitsky, S., 1962, Records of selected wells and springs, selected drillers' logs of wells, and chemical analyses of ground and surface waters, northern Utah Valley, Utah County, Utah: Utah Basic-Data Report 2, 14 p.","productDescription":"14 p.","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":345756,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":345754,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://www.waterrights.utah.gov/cgi-bin/docview.exe?Folder=TP21-1-040&Title=Basic+Data+Report+2"}],"country":"United States","state":"Utah","county":"Utah County","otherGeospatial":"Utah Valley","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"59bb953ce4b091459a57823e","contributors":{"authors":[{"text":"Subitsky, Seymour","contributorId":77227,"corporation":false,"usgs":true,"family":"Subitsky","given":"Seymour","email":"","affiliations":[],"preferred":false,"id":710415,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70171141,"text":"70171141 - 1962 - Distribution and detoxication of toxaphene in Clayton Lake, New Mexico","interactions":[],"lastModifiedDate":"2016-05-23T17:23:31","indexId":"70171141","displayToPublicDate":"1962-01-01T00:00:00","publicationYear":"1962","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3624,"text":"Transactions of the American Fisheries Society","active":true,"publicationSubtype":{"id":10}},"title":"Distribution and detoxication of toxaphene in Clayton Lake, New Mexico","docAbstract":"

The fate of toxaphene, applied in three treatments at a total calculated concentration of 0.05 p.p.m. to Clayton Lake, New Mexico, was followed over a 1.5-year period. A detailed description of the chromatographic method of analysis is given. Water concentrations of toxaphene were higher in leeshore samples than in windward samples for 2 weeks after the application; toxaphene levels then appeared to reach a constant value of about 0.001 p.p.m. for at least an additional 250 days. Total body concentrations of toxaphene were determined in trout and bullheads present in the lake during the poisoning and in trout placed in the lake in live-cars subsequently. Trout were more susceptible to toxaphene and accumulated lower body levels than bullheads. Bullheads which showed symptoms of toxaphene poisoning when collected had higher levels than did normal-appearing individuals. No difference in levels was observed in live-car trout collected dead as compared to survivors. Aquatic vegetation accumulated high concentrations of toxaphene; low concentrations were found in some sediment samples. The significance of these findings is discussed.

","language":"English","publisher":"Taylor & Francis","doi":"10.1577/1548-8659(1962)91[14:DADOTI]2.0.CO;2","usgsCitation":"Kallman, B.J., Cope, O.B., and Navarre, R.J., 1962, Distribution and detoxication of toxaphene in Clayton Lake, New Mexico: Transactions of the American Fisheries Society, v. 91, no. 1, p. 14-22, https://doi.org/10.1577/1548-8659(1962)91[14:DADOTI]2.0.CO;2.","productDescription":"9 p.","startPage":"14","endPage":"22","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":192,"text":"Columbia Environmental Research Center","active":true,"usgs":true}],"links":[{"id":321555,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"New Mexico","otherGeospatial":"Clayton Lake","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -103.31233978271483,\n 36.58245213849012\n ],\n [\n -103.31130981445312,\n 36.573216031837795\n ],\n [\n -103.31062316894531,\n 36.57128595955732\n ],\n [\n -103.29414367675781,\n 36.57004517333383\n ],\n [\n -103.29465866088867,\n 36.58148722380944\n ],\n [\n -103.2963752746582,\n 36.58617383928255\n ],\n [\n -103.31216812133789,\n 36.586587350516545\n ],\n [\n -103.31233978271483,\n 36.58245213849012\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"91","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"574d64a7e4b07e28b66839ef","contributors":{"authors":[{"text":"Kallman, Burton J.","contributorId":169580,"corporation":false,"usgs":false,"family":"Kallman","given":"Burton","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":630094,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Cope, Oliver B.","contributorId":13290,"corporation":false,"usgs":true,"family":"Cope","given":"Oliver","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":630095,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Navarre, Richard J.","contributorId":169581,"corporation":false,"usgs":false,"family":"Navarre","given":"Richard","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":630096,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":6308,"text":"pp342 - 1962 - Geology and ore deposits of the Globe-Miami district, Arizona","interactions":[{"subject":{"id":51373,"text":"ofr53216 - 1953 - Geologic map of a portion of the Inspiration quadrangle, Arizona","indexId":"ofr53216","publicationYear":"1953","noYear":false,"title":"Geologic map of a portion of the Inspiration quadrangle, Arizona"},"predicate":"SUPERSEDED_BY","object":{"id":6308,"text":"pp342 - 1962 - Geology and ore deposits of the Globe-Miami district, Arizona","indexId":"pp342","publicationYear":"1962","noYear":false,"title":"Geology and ore deposits of the Globe-Miami district, Arizona"},"id":1}],"lastModifiedDate":"2023-11-07T19:34:14.377195","indexId":"pp342","displayToPublicDate":"1962-01-01T00:00:00","publicationYear":"1962","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"342","title":"Geology and ore deposits of the Globe-Miami district, Arizona","docAbstract":"The rocks of the Globe-Miami district range from lower Precambrian to Recent. The oldest formation, the Pinal schist, comprises several varieties of schist formed by dynamic and thermal metamorphism of shale and feldspathic sandstone during the early Precambrian Mazatzal revolution. During the later stages of this revolution, the schist was intruded by a complex of dioritic rocks and by plutons of granite and quartz monzonite. There were extensive intrusions of a biotite-quartz diorite, known as the Madera diorite, mainly south of the district. In the northern part of the mapped area, the schist was invaded by an extensive mass, the Ruin granite, which is a coarse-grained rock most commonly of quartz monzonitic composition. There are also smaller sill-like masses of slightly gneissic muscovite granite.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/pp342","usgsCitation":"Peterson, N.P., 1962, Geology and ore deposits of the Globe-Miami district, Arizona: U.S. Geological Survey Professional Paper 342, Report: vi, 151 p.; 8 Plates: 44.79 x 30.92 inches or smaller, https://doi.org/10.3133/pp342.","productDescription":"Report: vi, 151 p.; 8 Plates: 44.79 x 30.92 inches or smaller","numberOfPages":"157","costCenters":[],"links":[{"id":271114,"rank":9,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0342/plate-6.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":271113,"rank":7,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0342/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":271111,"rank":6,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0342/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":271112,"rank":5,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0342/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":275837,"rank":10,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0342/plate-8.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":271109,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0342/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":422430,"rank":11,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_4334.htm","linkFileType":{"id":5,"text":"html"}},{"id":271115,"rank":8,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0342/plate-7.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":271110,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0342/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":139786,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0342/report-thumb.jpg"},{"id":268960,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0342/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Arizona","county":"Pinal County","otherGeospatial":"Globe-Miami district","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -111,\n 33.5\n ],\n [\n -111,\n 33.25\n ],\n [\n -110.875,\n 33.25\n ],\n [\n -110.875,\n 33.375\n ],\n [\n -110.75,\n 33.375\n ],\n [\n -110.75,\n 33.5\n ],\n [\n -111,\n 33.5\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad7e4b07f02db68449a","contributors":{"authors":[{"text":"Peterson, N. P.","contributorId":29827,"corporation":false,"usgs":true,"family":"Peterson","given":"N.","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":152484,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":1000071,"text":"1000071 - 1962 - Comparative toxicity of 3-trifluormethyl-4-nitrophenol (TFM) to larval lampreys and eleven species of fishes","interactions":[],"lastModifiedDate":"2016-03-07T12:11:42","indexId":"1000071","displayToPublicDate":"1962-01-01T00:00:00","publicationYear":"1962","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3624,"text":"Transactions of the American Fisheries Society","active":true,"publicationSubtype":{"id":10}},"title":"Comparative toxicity of 3-trifluormethyl-4-nitrophenol (TFM) to larval lampreys and eleven species of fishes","docAbstract":"

The tolerances of larval lampreys, rainbow trout, and 10 species of warmwater fishes to 3-trifluormethyl-4-nitrophenol (TFM), a selective lamprey larvicide, were determined in three dilution waters of different physical and chemical characteristics. Differential toxic effects of the chemical to larval lampreys and test fishes varied broadly with the species of fish. Smallmouth bass and other centrarchids were most tolerant of the chemical; walleye, yellow perch, bullheads, and white suckers were most susceptible. The toxicity of TFM to both lampreys and fishes diminished as the conductivity and alkalinity of the dilution water increased. The differential action of the chemical was retained in all waters, however.

","language":"English","publisher":"Taylor & Francis","doi":"10.1577/1548-8659(1962)91[342:CTOTTT]2.0.CO;2","usgsCitation":"Applegate, V.C., and King, E.L., 1962, Comparative toxicity of 3-trifluormethyl-4-nitrophenol (TFM) to larval lampreys and eleven species of fishes: Transactions of the American Fisheries Society, v. 91, no. 4, p. 342-345, https://doi.org/10.1577/1548-8659(1962)91[342:CTOTTT]2.0.CO;2.","productDescription":"4 p.","startPage":"342","endPage":"345","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"links":[{"id":128996,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"91","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b24e4b07f02db6ae471","contributors":{"authors":[{"text":"Applegate, Vernon C.","contributorId":39317,"corporation":false,"usgs":true,"family":"Applegate","given":"Vernon","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":308029,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"King, Everett L.","contributorId":54922,"corporation":false,"usgs":true,"family":"King","given":"Everett","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":308030,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70009799,"text":"70009799 - 1962 - Behaviour of calcium carbonate in sea water","interactions":[],"lastModifiedDate":"2020-09-09T13:46:35.413922","indexId":"70009799","displayToPublicDate":"1962-01-01T00:00:00","publicationYear":"1962","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1759,"text":"Geochimica et Cosmochimica Acta","active":true,"publicationSubtype":{"id":10}},"title":"Behaviour of calcium carbonate in sea water","docAbstract":"

Anomalies in the behaviour of calcium carbonate in natural solutions diminish when considered in context. Best values found by traditional oceanographie methods for the apparent solubility product constant K'CaCO3 in sea water at atmospheric pressure are consistent mineralogically—at 36 parts per thousand salinity and T-25°C, K'aragonlte is estimated as 1.12 × 10−6 and K'calcite as 0.61 × 10−6. At 30°C the corresponding values are 0.98 × 10−6 for aragonite and 0.53 × 10−6 for calcite. Because the K' computations do not compensate for ionic activity, however, they cannot give thermodynamically satisfactory results. It is of interest, therefore, that approximate methods and information now available permit the estimation from the same basic data of an activity product constant KCaCO3 close to that found in solutions to which Debye-Hückel theory applies. Such methods indicate approximate Karagonite 7.8 × 10−9 for surface sea water at 29°C; Kcalcite would be proportionately lower.

Field data and experimental results indicate that the mineralogy of precipitated CaCO3 depends primarily on degree of supersaturation, thus also on kinetic or biologic factors that facilitate or inhibit a high degree of supersaturation. The shallow, generally hypersaline bank waters west of Andros Island yield aragonitic sediments with O18O16\">O18O16 ratios that imply precipitation mainly during the warmer months, when the combination of a high rate of evaporation, increasing salinity (and ionic strength), maximal temperatures and photosynthetic removal of CO2 result in high apparent supersaturation. The usual precipitate from solutions of low ionic strength is calcite, except where the aragonite level of supersaturation is reached as a result of diffusion phenomena (e.g. dripstones), gradual and marked evaporation, or biologic intervention. Published data also suggest the possibility of distinct chemical milieus for crystallographic variations in skeletal calcium carbonate. It appears that in nature aragonite precipitates from solutions that are supersaturated with respect to both calcite and aragonite and calcite between saturation levels for the two species. Such a relation is consistent with Ostwald's rule of successive reactions.

Aragonitc of marine origin persists in contact with supersaturated interstitial solutions at ordinary temperature and pressure. Conversion to calcite follows transfer to solutions undersaturated with respect to aragonite or upon exposure to the moist atmosphere.

","language":"English","publisher":"Elsevier","doi":"10.1016/0016-7037(62)90117-5","usgsCitation":"Cloud, P.E., 1962, Behaviour of calcium carbonate in sea water: Geochimica et Cosmochimica Acta, v. 26, no. 8, p. 867-884, https://doi.org/10.1016/0016-7037(62)90117-5.","productDescription":"19 p.","startPage":"867","endPage":"884","costCenters":[],"links":[{"id":218757,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"26","issue":"8","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059f0abe4b0c8380cd4a84d","contributors":{"authors":[{"text":"Cloud, P. E. Jr.","contributorId":6507,"corporation":false,"usgs":true,"family":"Cloud","given":"P.","suffix":"Jr.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":357173,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70171160,"text":"70171160 - 1962 - Dissolved oxygen in Lake Erie, past and present","interactions":[],"lastModifiedDate":"2016-05-24T10:41:05","indexId":"70171160","displayToPublicDate":"1962-01-01T00:00:00","publicationYear":"1962","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Dissolved oxygen in Lake Erie, past and present","docAbstract":"

No abstract available.

","largerWorkType":{"id":24,"text":"Conference Paper"},"largerWorkTitle":"Proceedings of the 5th Conference on Great Lakes Research","largerWorkSubtype":{"id":19,"text":"Conference Paper"},"conferenceTitle":"5th Conference on Great Lakes Research","conferenceDate":"April 9-10","conferenceLocation":"Toronto, Canada","language":"English","publisher":"University of Michigan","usgsCitation":"Carr, J., 1962, Dissolved oxygen in Lake Erie, past and present, in Proceedings of the 5th Conference on Great Lakes Research, Toronto, Canada, April 9-10, p. 1-14.","productDescription":"14 p.","startPage":"1","endPage":"14","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"links":[{"id":321600,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"574d64a7e4b07e28b66839e6","contributors":{"authors":[{"text":"Carr, John F.","contributorId":67471,"corporation":false,"usgs":true,"family":"Carr","given":"John F.","affiliations":[],"preferred":false,"id":630141,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ]}