A probe for sampling interstitial waters of stream sediments and bog soils is described. Samples can be obtained within a stratigraphic interval of 2–3 cm, to a depth of 60–80 cm, and with little or no contamination of the samples by sediment or air.
The first naturally occurring terrestrial example of vapor-liquid-solid (VLS) growth has been observed in condensates from gases released by burning coal in culm banks. Scanning electron microscopy, X-ray diffraction, and energy dispersive analysis indicate that the crystals consist of elongated rods (≈ 100 μm) of germanium sulfide capped by bulbs depleted in germanium.
From experimental studies of gamma rays from fast and thermal neutron reactions in hydrogeneous and non-hydrogeneous, semi-infinite samples and from Monte Carlo calculations on soil of a composition which might typically be encountered on planetary surfaces, it is found that gamma rays from fast or inelastic scattering reactions would dominate the observed spectra. With the exception of gamma rays formed by inelastically scattered neutrons on oxygen, useful spectra would be limited to energies below 3 MeV. Other experiments were performed which show that if a gamma-ray detector were placed within 6 m of an isotopic neutron source in a spacecraft, it would be rendered useless for gamma-ray spectrometry below 3 MeV because of internal activation produced by neutron exposure during space travel. Adequate shielding is not practicable because of the size and weight constraints for planetary missions. Thus, it is required that the source be turned off or removed to a safe distance during non-measurement periods. In view of these results an accelerator or an off-on isotopic source would be desirable for practical gamma-ray spectral analysis on planetary surfaces containing but minor amounts of hydrogen.
PUBLISHED reconstructions of Gondwana continent1 (Fig. la) show a gap in fit near the junction of the Americas and Africa. To study this critical area, the Unitedgeo I made geophysical measurements and collected rock samples across the continental margin of Liberia (USGS-IDOE cruise leg 5) in November 1971. Figure Ib indicates the location of the 5,400 km of ship track on a generalised bathymetric map2. We shall discuss the data in detail elsewhere. Here we present the evidence for the existence of three fracture zones, two of which have not been reported previously, intersecting the continental margin at the north end of the South Atlantic, which remained closed probably until Cretaceous time. We suggest that Precambrian structures on the African continent controlled the location of these fracture zones. Figure Ic compares gravity and magnetic profiles and interpretations of the seismic profiles for three selected lines (27, 30 and 34) crossing the Grand Cess, Cape Palmas and St Paul fracture zones, respectively.
Water potential in Sonoran Desert shrubs was recorded from September 1968 through September 1969. Special attention was paid to recording maximum and minimum potentials on a seasonal basis and diurnal fluctuations during the wettest and driest periods of the year. Franseria deltoidea developed the lowest potential (—85 bar) of the shrubs recorded and also showed the greatest degree of response to changes in soil moisture on a seasonal basis and evaporative power of the air on a diurnal basis. Of the species tested, Eriogonum fasciculatum showed a high degree of response to changing conditions; Larrea tridentata, Krameria gravi, and Simmondsia chinesis showed a moderate response; and Cercidium microphyllum showed only a slight response to diurnal or seasonal changes.
","language":"English","publisher":"Ecological Society of America","doi":"10.2307/1934632","usgsCitation":"Halvorson, W., and Patten, D.T., 1974, Seasonal water potential changes in Sonoran Desert shrubs in relation to topography: Ecology, v. 55, p. 173-177, https://doi.org/10.2307/1934632.","productDescription":"5 p.","startPage":"173","endPage":"177","numberOfPages":"5","costCenters":[{"id":651,"text":"Western Ecological Research Center","active":true,"usgs":true}],"links":[{"id":130406,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"55","noUsgsAuthors":false,"publicationDate":"1974-01-01","publicationStatus":"PW","scienceBaseUri":"4f4e4a0ce4b07f02db5fc2e3","contributors":{"authors":[{"text":"Halvorson, William L.","contributorId":97194,"corporation":false,"usgs":true,"family":"Halvorson","given":"William L.","affiliations":[],"preferred":false,"id":315853,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Patten, Duncan T.","contributorId":124573,"corporation":false,"usgs":false,"family":"Patten","given":"Duncan","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":315852,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70009795,"text":"70009795 - 1974 - The regolith at the Apollo 15 site and its stratigraphic implications","interactions":[],"lastModifiedDate":"2021-02-04T15:12:43.485181","indexId":"70009795","displayToPublicDate":"1974-01-01T00:00:00","publicationYear":"1974","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 regolith at the Apollo 15 site and its stratigraphic implications","docAbstract":"Regolith samples from the Apollo 15 landing site are described in terms of two major fractions, a homogeneous glass fraction and a non-homogeneous glass fraction. The proportions of different components in the homogeneous glass fraction were determined directly by chemical analyses of individual particles. They are mainly green glass, a mare-like glass, and different types of Fra Mauro and Highland type glasses. The proportions of various components in the remainder of each of the soils were determined indirectly by finding the mix of components that best fits their bulk compositions. The mixing model suggests that the Apennine Front consists mainly of rocks of low-K Fra Mauro basalt composition. These may overlie rocks with the composition of anorthositic gabbro. Green glass, which occurs widely throughout the site is believed to be derived from a green glass layer which darkens upland surfaces and lies beneath the local mare surface.
The Du Noir Addition to the Washakie Wilderness area consists of 34,200 acres (13,840 hectares) of scenic mountainous terrain that adjoins the Teton Wilderness and Washakie Wilderness areas. The area was studied in 1973 by the U.S. Geological Survey and U.S. Bureau of Mines to evaluate its mineral, fuel, and geothermal energy potential. This evaluation is based on a search of the geologic literature, claim and production records, and fieldwork including mapping, inspection of claims and prospects, interpretation of aeromagnetic maps, and analyses of bedrock and stream-sediment samples.
Flat-lying Eocene volcaniclastic rocks of the Absaroka volcanic field are exposed in about two-thirds of the Du Noir Addition. These volcanics unconformably overlie the deeply eroded, northwest-trending Du Noir anticline in which Paleozoic marine strata of Devonian through Permian age are exposed. Of lesser importance are small deposits of Eocene non-volcanic conglomerate, and basaltic intrusive and extrusive rocks of late Pliocene and possibly younger age.
The results of this study indicate that the mineral, fuel, and geothermal potential of the Du Noir Addition are minimal. Low-grade copper-molybdenum mineralization occurs outside the addition, associated with intrusive rocks, but no indications of alteration or mineralization were found within the study area. Anomalous, but not economically important, concentrations of molybdenum and uranium were found in Permian and Eocene carbonaceous shales. Phosphate rock in the Phosphoria Formation occurs in beds too thin to constitute a resource. Large amounts of very pure limestone are present in the Madison Limestone, but equally pure limestone, much closer to transportation facilities, is found throughout this part of Wyoming. That part of the Du Noir anticline in the addition is too deeply eroded to be a likely reservoir of oil and gas. Present data indicates a low potential for geothermal energy in or near the addition.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr74133","usgsCitation":"Prostka, H.J., Antweiler, J., Bieniewski, C.L., and Kleinkopf, M.D., 1974, Mineral resources of Du Noir Addition, Washakie Wilderness area, Fremont County, Wyoming: U.S. Geological Survey Open-File Report 74-133, 34 p., https://doi.org/10.3133/ofr74133.","productDescription":"34 p.","costCenters":[],"links":[{"id":425892,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1974/0133/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":147778,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1974/0133/report-thumb.jpg"}],"country":"United States","state":"Wyoming","county":"Fremont County","otherGeospatial":"Washakie Wilderness area","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -109.97801721114597,\n 43.90547231590443\n ],\n [\n -109.97801721114597,\n 43.57966336178319\n ],\n [\n -109.11468697657382,\n 43.57966336178319\n ],\n [\n -109.11468697657382,\n 43.90547231590443\n ],\n [\n -109.97801721114597,\n 43.90547231590443\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a1ae4b07f02db60641d","contributors":{"authors":[{"text":"Prostka, Harold J.","contributorId":52185,"corporation":false,"usgs":true,"family":"Prostka","given":"Harold","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":171259,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Antweiler, J.C.","contributorId":35722,"corporation":false,"usgs":true,"family":"Antweiler","given":"J.C.","email":"","affiliations":[],"preferred":false,"id":171258,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Bieniewski, Carl L.","contributorId":56236,"corporation":false,"usgs":true,"family":"Bieniewski","given":"Carl","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":171260,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Kleinkopf, M. D.","contributorId":10036,"corporation":false,"usgs":true,"family":"Kleinkopf","given":"M.","middleInitial":"D.","affiliations":[],"preferred":false,"id":171257,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":70010916,"text":"70010916 - 1974 - Kaolinite synthesis at 25°C","interactions":[],"lastModifiedDate":"2015-06-15T11:26:05","indexId":"70010916","displayToPublicDate":"1974-01-01T00:00:00","publicationYear":"1974","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3338,"text":"Science","active":true,"publicationSubtype":{"id":10}},"title":"Kaolinite synthesis at 25°C","docAbstract":"The addition of quercetin, an organic flavone (C15H10O7), to aqueous solutions containing silica and aluminum and adjusted to final pH's from 6.5 to 8.5 produced a 1 : 1 alumninosilicate precipitate which, after 6 to 16 months of aging in solution at 25°C, contained as much as 5 percent well-formed kaolinite plates. Similar solutions containing no organic material produced relatively amorphous precipitates with the same composition and stability (standard free energy of formation = -897±1 kilocalories per mole) but with substantially smaller amounts of crystaline material even after 2 years of aging.
","language":"English","publisher":"AAAS","doi":"10.1126/science.184.4142.1171","issn":"00368075","usgsCitation":"Hem, J., and Lind, C.J., 1974, Kaolinite synthesis at 25°C: Science, v. 184, no. 4142, p. 1171-1173, https://doi.org/10.1126/science.184.4142.1171.","productDescription":"3 p.","startPage":"1171","endPage":"1173","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":221630,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"184","issue":"4142","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a405de4b0c8380cd64cdb","contributors":{"authors":[{"text":"Hem, J.D.","contributorId":54576,"corporation":false,"usgs":true,"family":"Hem","given":"J.D.","affiliations":[],"preferred":false,"id":359891,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lind, Carol J.","contributorId":36110,"corporation":false,"usgs":true,"family":"Lind","given":"Carol","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":359890,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":1013670,"text":"1013670 - 1974 - In vitro and in vivo efficacy of potentiated sulfonamide in control of furunculosis in salmonids","interactions":[],"lastModifiedDate":"2025-03-04T16:35:17.706034","indexId":"1013670","displayToPublicDate":"1974-01-01T00:00:00","publicationYear":"1974","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2543,"text":"Journal of the Fisheries Research Board of Canada","active":true,"publicationSubtype":{"id":10}},"title":"In vitro and in vivo efficacy of potentiated sulfonamide in control of furunculosis in salmonids","docAbstract":"In vitro and in vivo efficacy of a potentiated sulffonamide, Ro5–0037, for inhibition of Aeromonas salmonicida, causative agent of fish furunculosis was determined. The components of the potentiated sulfonamide, sulfadimethoxine, and ormetoprim were tested alone and in combination. In vitro results showed that both sulfonamide-resistant and sensitive strains of A. salmonicida had greater sensitivity to Ro5–0037 than to either of its components. Also, sulfonamide-sensitive strains developed resistance to ormetoprim and sulfadimethoxine more rapidly than to Ro5–0037. Efficacy studies with small numbers of artificially infected trout revealed that Ro5–0037 effectively controlled furunculosis at 50 mg/kg of fish/day, one fourth the usual sulfonamide dosage level. Extensive field trials also showed the 50 mg/kg level of Ro5–0037 gave effective control of hatchery outbreaks of furunculosis. As found in the in vitro studies, all in vivo trials indicated the combination of ormetoprim and sulfadimethoxine was more efficient in inhibiting A. salmonicida than either component alone.
","language":"English","publisher":"Canadian Science Publishing","doi":"10.1139/f74-011","usgsCitation":"Bullock, G.L., Stuckey, H.M., Collis, D., Herman, R.L., and Maestrone, G., 1974, In vitro and in vivo efficacy of potentiated sulfonamide in control of furunculosis in salmonids: Journal of the Fisheries Research Board of Canada, v. 31, no. 1, p. 75-82, https://doi.org/10.1139/f74-011.","productDescription":"8 p.","startPage":"75","endPage":"82","numberOfPages":"8","costCenters":[{"id":365,"text":"Leetown Science Center","active":true,"usgs":true}],"links":[{"id":131447,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"31","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49fce4b07f02db5f5bc3","contributors":{"authors":[{"text":"Bullock, G. L.","contributorId":69498,"corporation":false,"usgs":true,"family":"Bullock","given":"G.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":319012,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Stuckey, H. M.","contributorId":60157,"corporation":false,"usgs":true,"family":"Stuckey","given":"H.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":319010,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Collis, D.","contributorId":21501,"corporation":false,"usgs":true,"family":"Collis","given":"D.","email":"","affiliations":[],"preferred":false,"id":319009,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Herman, R. L.","contributorId":21101,"corporation":false,"usgs":true,"family":"Herman","given":"R.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":319008,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Maestrone, G.","contributorId":60158,"corporation":false,"usgs":true,"family":"Maestrone","given":"G.","email":"","affiliations":[],"preferred":false,"id":319011,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}} ,{"id":1013904,"text":"1013904 - 1974 - You asked for it! Answers to questions from persons interested in fish farming: Part I","interactions":[],"lastModifiedDate":"2012-08-24T01:02:05","indexId":"1013904","displayToPublicDate":"1974-01-01T00:00:00","publicationYear":"1974","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1277,"text":"Commercial Fish Farmer and Aquaculture News","active":true,"publicationSubtype":{"id":10}},"title":"You asked for it! Answers to questions from persons interested in fish farming: Part I","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Commercial Fish Farmer and Aquaculture News","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Richard V. Gallagher","publisherLocation":"Arden, NC","collaboration":"None/FF","usgsCitation":"Giudice, J., 1974, You asked for it! Answers to questions from persons interested in fish farming: Part I: Commercial Fish Farmer and Aquaculture News, v. 1, no. 2, p. 46-47.","productDescription":"2 p.","startPage":"46","endPage":"47","numberOfPages":"2","costCenters":[{"id":365,"text":"Leetown Science Center","active":true,"usgs":true}],"links":[{"id":132174,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"1","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49d6e4b07f02db5de30d","contributors":{"authors":[{"text":"Giudice, J.J.","contributorId":50841,"corporation":false,"usgs":true,"family":"Giudice","given":"J.J.","email":"","affiliations":[],"preferred":false,"id":319426,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70011077,"text":"70011077 - 1974 - Martian planetwide crater distributions: Implications for geologic history and surface processes","interactions":[],"lastModifiedDate":"2021-01-15T13:55:17.854115","indexId":"70011077","displayToPublicDate":"1974-01-01T00:00:00","publicationYear":"1974","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1963,"text":"Icarus","active":true,"publicationSubtype":{"id":10}},"title":"Martian planetwide crater distributions: Implications for geologic history and surface processes","docAbstract":"Population-density maps of craters in three size ranges (0.6 to 1.2 km, 4 to 10 km, and >20 km in diameter) were compiled for most of Mars from Mariner 9 imagery. These data provide: historical records of the eolian processes (0.6 to 1.2 km craters); stratigraphic, relative, and absolute timescales (4 to 10 km craters); and a history of the early postaccretional evolution of the uplands (> 20 km craters).
Based on the distribution of large craters (>20 km diameters), Mars is divisible into two general classes of terrain, densely cratered and very lightly cratered—a division remarkably like the uplands-maria dichotomy of the moon. It is probable that this bimodal character in the density distribution of large craters arose from an abrupt transition in the impact flux rate from an early intense period associated with the tailing off of accretion to an extended quiescent epoch, not from a void in geological activity during much of Mars' history. Radio-isotope studies of Apollo lunar samples show that this transition occurred on the moon in a short time.
The intermediate-sized craters (4 to 10 km diameter) and the small-sized craters (0.6 to 1.2 km diameter) appear to be genetically related. The smaller ones are apparently secondary impact craters generated by the former. Most of the craters in the larger of these two size classes appear fresh and uneroded, although many are partly buried by dust mantles. Poleward of the 40° parallels the small fresh craters are notably absent owing to these mantles. The density of small craters is highest in an irregular band centered at 20°S. This band coincides closely with (1) the zone of permanent low-albedo markings; (2) the “wind equator” (the latitude of zero net north or south transport at the surface); and (3) a band that includes a majority of the small dendritic channels. Situated in the southermost part of the equatorial unmantled terrain which extends from about 40°N to 40°S, this band is apparently devoid of even a thin mantle. Because this belt is also coincident with the latitutde of maximum solar insolation (periapsis occurs near summer solstice), we suggest that this band arises from the asymmetrical global wind patterns at the surface and that the band probably follows the latitude of maximum heating which migrates north and south from 25°N to 25°S within the unmantled terrain on a 50,000 year timescale.
The population of intermediate-sized craters (4–10 km diameter) appears unaffected by the eolian mantles, at least within the ±45° latitudes. Hence the local density of these craters is probably a valid indicator of the relative age of surfaces generated during the period since the uplands were intensely bombarded and eroded. It now appears that the impact fluxes at Mars and the moon have been roughly the same over the last 4 b.y. because the oldest postaccretional, mare-like surfaces on Mars and the moon display about the same crater density. If so, the nearness of Mars to the asteroid belt has not generated a flux 10 to 25 times greater than the lunar flux. Whereas the lunar maria show a variation of about a factor of three in crater density from the oldest to the youngest major units, analogous surfaces on Mars show a variation between 30 and 50. This implies that periods of active eolian erosion, tectonic evolution, volcanic eruption, and possibly fluvial modification have been scattered throughout Martian history since the formation and degradation of the martian uplands and not confined to small, ancient or recent, epochs. These processes are surely active on the planet today.
","language":"English","publisher":"Elsevier","doi":"10.1016/0019-1035(74)90175-4","issn":"00191035","usgsCitation":"Soderblom, L., Condit, C., West, R., Herman, B., and Kreidler, T.J., 1974, Martian planetwide crater distributions: Implications for geologic history and surface processes: Icarus, v. 22, no. 3, p. 239-263, https://doi.org/10.1016/0019-1035(74)90175-4.","productDescription":"25 p.","startPage":"239","endPage":"263","numberOfPages":"25","costCenters":[],"links":[{"id":221151,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"22","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a5234e4b0c8380cd6c23d","contributors":{"authors":[{"text":"Soderblom, L.A. 0000-0002-0917-853X","orcid":"https://orcid.org/0000-0002-0917-853X","contributorId":6139,"corporation":false,"usgs":true,"family":"Soderblom","given":"L.A.","affiliations":[],"preferred":false,"id":360230,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Condit, C.D.","contributorId":60250,"corporation":false,"usgs":true,"family":"Condit","given":"C.D.","email":"","affiliations":[],"preferred":false,"id":360234,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"West, R.A.","contributorId":51019,"corporation":false,"usgs":true,"family":"West","given":"R.A.","email":"","affiliations":[],"preferred":false,"id":360232,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Herman, B.M.","contributorId":24494,"corporation":false,"usgs":true,"family":"Herman","given":"B.M.","email":"","affiliations":[],"preferred":false,"id":360231,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Kreidler, T. J.","contributorId":57460,"corporation":false,"usgs":true,"family":"Kreidler","given":"T.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":360233,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}} ,{"id":1013669,"text":"1013669 - 1974 - Corynebacterial kidney disease of salmonids: Growth and serological studies on the causative bacterium","interactions":[],"lastModifiedDate":"2023-09-13T14:06:47.527017","indexId":"1013669","displayToPublicDate":"1974-01-01T00:00:00","publicationYear":"1974","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":843,"text":"Applied Microbiology","active":true,"publicationSubtype":{"id":10}},"title":"Corynebacterial kidney disease of salmonids: Growth and serological studies on the causative bacterium","docAbstract":"Comparative growth studies of 10 isolates of the Corynebacterium of salmonid kidney disease were quantified on four media. Greatest cell yield was obtained from Mueller-Hinton medium with 0.1% L-cysteine hydrochloride. Serological tests, in which rabbit antisera used against typical bacteria strains showed all to be antigenically homologous, provided a reliable method of identification.
","language":"English","publisher":"American Society for Microbiology","doi":"10.1128/am.28.5.811-814.1974","usgsCitation":"Bullock, G.L., Stuckey, H.M., and Chen, P.K., 1974, Corynebacterial kidney disease of salmonids: Growth and serological studies on the causative bacterium: Applied Microbiology, v. 28, no. 5, p. 811-814, https://doi.org/10.1128/am.28.5.811-814.1974.","productDescription":"4 p.","startPage":"811","endPage":"814","costCenters":[{"id":365,"text":"Leetown Science Center","active":true,"usgs":true}],"links":[{"id":480649,"rank":2,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1128/am.28.5.811-814.1974","text":"Publisher Index Page"},{"id":131446,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"28","issue":"5","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad6e4b07f02db684253","contributors":{"authors":[{"text":"Bullock, G. L.","contributorId":69498,"corporation":false,"usgs":true,"family":"Bullock","given":"G.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":319007,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Stuckey, H. M.","contributorId":60157,"corporation":false,"usgs":true,"family":"Stuckey","given":"H.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":319006,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Chen, P. K.","contributorId":6008,"corporation":false,"usgs":true,"family":"Chen","given":"P.","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":319005,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":1014238,"text":"1014238 - 1974 - Effect of feeding brown trout (Salmo trutta) a diet pelleted in dry and moist forms","interactions":[],"lastModifiedDate":"2025-03-04T16:25:37.160216","indexId":"1014238","displayToPublicDate":"1974-01-01T00:00:00","publicationYear":"1974","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2543,"text":"Journal of the Fisheries Research Board of Canada","active":true,"publicationSubtype":{"id":10}},"title":"Effect of feeding brown trout (Salmo trutta) a diet pelleted in dry and moist forms","docAbstract":"Growth rate, body composition, and intake of either dry matter or energy did not differ significantly (P > 0.05) between two groups of juvenile brown trout (Salmo trutta) fed either a low- or high-moisture semipurified diet at different rates to compensate for a diet energy density gradient. Feed/gain efficiency, on an as-fed basis, was significantly greater (P < 0.01) in fish fed the low-moisture diet, but did not differ (P > 0.05) when compared on the basis of dry matter or energy intake.
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