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,{"id":70213007,"text":"70213007 - 1936 - The diurnal fluctuation in the ground‐water and flow of the Santa Ana River and its meaning","interactions":[],"lastModifiedDate":"2020-09-08T15:27:29.575745","indexId":"70213007","displayToPublicDate":"1936-09-03T13:34:33","publicationYear":"1936","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1578,"text":"Eos, Transactions, American Geophysical Union","onlineIssn":"2324-9250","printIssn":"0096-394","active":true,"publicationSubtype":{"id":10}},"title":"The diurnal fluctuation in the ground‐water and flow of the Santa Ana River and its meaning","docAbstract":"<p>In the time alloted for this subject it will be impossible to discuss, in its entirety, all phases of the methods used in computing the loss of water by transpiration from native plant‐life along the Santa Ana River. The results of this work are published in Bulletin 44 of the Division of Water Resources, State of California. The present paper is confined to a discussion of the diurnal fluctuations that occur in the flow of the Santa Ana River and the adjacent ground‐water.</p><p>On Figure 1 have, been plotted the gage‐height records for a short period (July 5–8, 1935) for eight southern California streams. These records have been selected at random from the large number of records filed in the local office of the United States Geological Survey. Some of these streams have a large drainage‐area, others are small; some are short and steep, others flat and long. The points of measurement range from 15 to 2950 feet above sea‐level. One of the streams (Mojave River) is in the desert‐region; the others drain into the Pacific Ocean. The object of Figure 1 is to demonstrate, that the diurnal fluctuation exists and is, to a large degree, similar at most points of measurement. As a rule, the maximum discharge occurs about 10 o'clock in the morning, and the minimum late in the afternoon. It is readily recognized that these fluctuations are in the main caused by the evaporation and transpiration‐loss in or adjacent to the stream‐channel.</p>","language":"English","publisher":"American Geophysical Union","doi":"10.1029/TR017i002p00496","usgsCitation":"Troxell, H.C., 1936, The diurnal fluctuation in the ground‐water and flow of the Santa Ana River and its meaning: Eos, Transactions, American Geophysical Union, v. 17, no. 2, p. 496-504, https://doi.org/10.1029/TR017i002p00496.","productDescription":"9 p.","startPage":"496","endPage":"504","costCenters":[],"links":[{"id":378149,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"California","otherGeospatial":"Santa Ana River","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -117.7679443359375,\n              33.858442151927896\n            ],\n            [\n              -117.71026611328125,\n              33.89093747081252\n            ],\n            [\n              -117.77000427246094,\n              33.91202429999497\n            ],\n            [\n              -117.84278869628908,\n              33.86699475113557\n            ],\n            [\n              -117.9045867919922,\n              33.81110228864701\n            ],\n            [\n              -117.93754577636719,\n              33.713488158266806\n            ],\n            [\n              -117.96501159667967,\n              33.646063909385845\n            ],\n            [\n              -117.97050476074219,\n              33.62719851659249\n            ],\n            [\n              -117.94784545898436,\n              33.61919376817004\n            ],\n            [\n              -117.88330078125,\n              33.751176960544875\n            ],\n            [\n              -117.83729553222655,\n              33.830497692052425\n            ],\n            [\n              -117.7679443359375,\n              33.858442151927896\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"17","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Troxell, Harold C.","contributorId":33354,"corporation":false,"usgs":true,"family":"Troxell","given":"Harold","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":797963,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70213001,"text":"70213001 - 1936 - The channel‐storage method of determining effluent seepage","interactions":[],"lastModifiedDate":"2020-09-03T17:22:03.032834","indexId":"70213001","displayToPublicDate":"1936-09-03T12:15:28","publicationYear":"1936","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1578,"text":"Eos, Transactions, American Geophysical Union","onlineIssn":"2324-9250","printIssn":"0096-394","active":true,"publicationSubtype":{"id":10}},"title":"The channel‐storage method of determining effluent seepage","docAbstract":"<p>Some years ago the senior author, in collaboration with Norah Dowell Stearns, undertook to make a monthly inventory of the water‐supply of the Pomperaug River Basin, in Connecticut, from a study of data obtained by A. J. Ellis from 1913 to 1916. For this purpose approximate determinations or estimates were made of the ground‐water runoff, that is, of the part of the daily discharge of the river that consisted of water derived from the zone of saturation by effluent seepage. The determinations or estimates were essentially based on the assumption that after a week of fair weather the storm‐water was all discharged and that until the next rain the runoff was essentially all ground‐water (U.S. Geol, Surv. Water‐Supply Paper 597, pp. 107–116 and pi. 19, 1929). In the discussion of the methods and results of this investigation, the following statement was made (Water‐Supply Paper 597, pp. 145–146):</p><p>“In this investigation the estimates of ground‐water runoff were based on the discharge of the Pomperaug at Bennetts Bridge—that is, on the discharge during the periods between rains, when there was virtually no direct runoff left in the stream‐system. Much better results could be obtained by basing the estimates on periods beginning as soon after rains as all of the direct runoff has reached the streams. With this method the ground‐water runoff during any particular day would be the total runoff minus the decrease in stream‐storage. The decrease in stream‐storage could be estimated by maintaining gages at several points on the trunk‐stream and on selected tributaries and making surveys of the stream‐system showing the approximate water‐areas of different parts of the system at different gage‐heights.”</p>","language":"English","publisher":"American Geophysical Union","doi":"10.1029/TR017i002p00415","usgsCitation":"Meinzer, O.E., Cady, R., Leggette, R., and Fishel, V., 1936, The channel‐storage method of determining effluent seepage: Eos, Transactions, American Geophysical Union, v. 17, no. 2, p. 415-418, https://doi.org/10.1029/TR017i002p00415.","productDescription":"4 p.","startPage":"415","endPage":"418","costCenters":[],"links":[{"id":378141,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"17","issue":"2","noUsgsAuthors":false,"publicationDate":"2014-08-18","publicationStatus":"PW","contributors":{"authors":[{"text":"Meinzer, Oscar E.","contributorId":83436,"corporation":false,"usgs":true,"family":"Meinzer","given":"Oscar","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":797950,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Cady, R.C.","contributorId":44905,"corporation":false,"usgs":true,"family":"Cady","given":"R.C.","email":"","affiliations":[],"preferred":false,"id":797951,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Leggette, R.M.","contributorId":87525,"corporation":false,"usgs":true,"family":"Leggette","given":"R.M.","email":"","affiliations":[],"preferred":false,"id":797952,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Fishel, V.C.","contributorId":6126,"corporation":false,"usgs":true,"family":"Fishel","given":"V.C.","email":"","affiliations":[],"preferred":false,"id":797953,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70213000,"text":"70213000 - 1936 - Several methods of studying fluctuations of ground‐water levels","interactions":[],"lastModifiedDate":"2020-09-03T17:03:47.454516","indexId":"70213000","displayToPublicDate":"1936-09-03T11:58:47","publicationYear":"1936","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1578,"text":"Eos, Transactions, American Geophysical Union","onlineIssn":"2324-9250","printIssn":"0096-394","active":true,"publicationSubtype":{"id":10}},"title":"Several methods of studying fluctuations of ground‐water levels","docAbstract":"<p><span>As a result of increased interest in ground‐water conditions in recent years, records of water‐levels in wells are now being collected in many places in the United States for the primary purpose of determining the relation of precipitation and other natural factors to fluctuations in water‐level. In the past, records of ground‐water levels have been collected chiefly in connection with intensive investigations in areas where the water‐levels were affected by artificial withdrawals and it has not been generally possible to correlate water‐level fluctuations closely with natural factors. It now appears probable that certain methods of studying water‐level fluctuations may be utilized advantageously in areas unaffected by heavy artificial withdrawals, but these methods generally do not yield satisfactory results in areas where there is considerable pumping or artesian flow. Three such methods are presented in this paper. The methods have not been given intensive study and their practical use is therefore not yet fully known. It is hoped that their application will be further investigated. Illustrations of the methods have been taken from records of ground‐water levels in the Platte River Valley, Nebraska, collected by the United States Geological Survey in cooperation with the Conservation and Survey Division of the University of Nebraska.</span></p>","publisher":"American Geophysical Union","doi":"10.1029/TR017i002p00400","usgsCitation":"Wenzel, L., 1936, Several methods of studying fluctuations of ground‐water levels: Eos, Transactions, American Geophysical Union, v. 17, no. 2, p. 400-405, https://doi.org/10.1029/TR017i002p00400.","productDescription":"6 p.","startPage":"400","endPage":"405","costCenters":[],"links":[{"id":378140,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"17","issue":"2","noUsgsAuthors":false,"publicationDate":"2014-08-18","publicationStatus":"PW","contributors":{"authors":[{"text":"Wenzel, Leland K.","contributorId":46077,"corporation":false,"usgs":true,"family":"Wenzel","given":"Leland K.","affiliations":[],"preferred":false,"id":797949,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70212999,"text":"70212999 - 1936 - Introduction: Some problems relating to fluctuations of ground‐water level","interactions":[],"lastModifiedDate":"2020-09-03T16:51:13.584707","indexId":"70212999","displayToPublicDate":"1936-09-03T11:34:28","publicationYear":"1936","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1578,"text":"Eos, Transactions, American Geophysical Union","onlineIssn":"2324-9250","printIssn":"0096-394","active":true,"publicationSubtype":{"id":10}},"title":"Introduction: Some problems relating to fluctuations of ground‐water level","docAbstract":"<p><span>When the program for the meeting of the Section of Hydrology a year ago was in preparation, it was suggested that a symposium be presented on the subject of the effects of the recent drought on ground‐water levels. The proposal was not carried out largely because at that time not enough accurate information on the subject was yet available. It has, however, seemed that this year a worth‐while group of papers could be developed on the broader subject of fluctuations of ground‐water levels.</span></p>","language":"English","publisher":"American Geophysical Union","doi":"10.1029/TR017i002p00337","usgsCitation":"Thompson, D.G., 1936, Introduction: Some problems relating to fluctuations of ground‐water level: Eos, Transactions, American Geophysical Union, v. 17, no. 2, p. 337-341, https://doi.org/10.1029/TR017i002p00337.","productDescription":"5 p.","startPage":"337","endPage":"341","costCenters":[],"links":[{"id":378139,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"17","issue":"2","noUsgsAuthors":false,"publicationDate":"2014-08-18","publicationStatus":"PW","contributors":{"authors":[{"text":"Thompson, D. G.","contributorId":95050,"corporation":false,"usgs":true,"family":"Thompson","given":"D.","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":797948,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70212977,"text":"70212977 - 1936 - Suspended matter in several small streams","interactions":[],"lastModifiedDate":"2020-09-02T16:22:43.22912","indexId":"70212977","displayToPublicDate":"1936-09-02T11:11:29","publicationYear":"1936","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1578,"text":"Eos, Transactions, American Geophysical Union","onlineIssn":"2324-9250","printIssn":"0096-394","active":true,"publicationSubtype":{"id":10}},"title":"Suspended matter in several small streams","docAbstract":"<p><span>The measurement of the loads of suspended matter carried past 34 gaging‐stations located on streams in eight regional projects of the Soil Conservation Service has required greater precision in the measurement of discharge and a more intensive program for the collection of samples of suspended matter than has been found necessary by the Geological Survey in making similar measurements on the larger streams on which measurements have been made in the past. It was found early in the work that much the greater part of the annual load of suspended matter was carried in a relatively few days of high water for almost all the streams on which measurements were made. In order that these loads might be determined with reasonable accuracy it was found necessary to collect samples every hour and occasionally every half‐hour on rising and rapidly changing stages during floods. Some floods occurring at night were missed in part or entirely because the resident observer did not realize that a flood was in progress. Twenty‐four‐hour sampling programs, together with the aid of electric‐alarm systems at some stations, have made possible the collection of an adequate number of samples during most floods.</span></p>","language":"English","publisher":"American Geophysical Union","doi":"10.1029/TR017i002p00447","usgsCitation":"Love, S.K., 1936, Suspended matter in several small streams: Eos, Transactions, American Geophysical Union, v. 17, no. 2, p. 447-452, https://doi.org/10.1029/TR017i002p00447.","productDescription":"6 p.","startPage":"447","endPage":"452","costCenters":[],"links":[{"id":378112,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"17","issue":"2","noUsgsAuthors":false,"publicationDate":"2014-08-18","publicationStatus":"PW","contributors":{"authors":[{"text":"Love, Samuel K.","contributorId":77845,"corporation":false,"usgs":true,"family":"Love","given":"Samuel","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":797879,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70212920,"text":"70212920 - 1936 - Fluctuations of ground‐water levels in Utah","interactions":[],"lastModifiedDate":"2020-09-01T19:39:53.339645","indexId":"70212920","displayToPublicDate":"1936-09-01T14:35:39","publicationYear":"1936","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1578,"text":"Eos, Transactions, American Geophysical Union","onlineIssn":"2324-9250","printIssn":"0096-394","active":true,"publicationSubtype":{"id":10}},"title":"Fluctuations of ground‐water levels in Utah","docAbstract":"<p><span>Long‐time continuous records of the fluctuations of ground‐water levels have been obtained at relatively few locations in the United States. Among the few available records for Utah that extend continuously over a period of a year or more are those made in the Jordan River and Ogden valleys by the United States Geological Survey in cooperation with Salt Lake City and Ogden. A few of the records of water‐levels, with records of stream‐flow and precipitation, are shown in Figure 1. Most of these records were begun during 1931 or 1932. A State‐wide program of well‐observations was begun during the summer of 1935 and is now in progress, the work being done by the Geological Survey in cooperation with the Utah State Engineer.</span></p>","language":"English","publisher":"American Geophysical Union","doi":"10.1029/TR017i002p00378","usgsCitation":"Taylor, G., 1936, Fluctuations of ground‐water levels in Utah: Eos, Transactions, American Geophysical Union, v. 17, no. 2, p. 378-382, https://doi.org/10.1029/TR017i002p00378.","productDescription":"5 p.","startPage":"378","endPage":"382","costCenters":[],"links":[{"id":378070,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"17","issue":"2","noUsgsAuthors":false,"publicationDate":"2014-08-18","publicationStatus":"PW","contributors":{"authors":[{"text":"Taylor, G.H.","contributorId":85158,"corporation":false,"usgs":true,"family":"Taylor","given":"G.H.","email":"","affiliations":[],"preferred":false,"id":797814,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
]}