Discussion of “pedological relations of infiltration phenomena”
W. C. Rasmussen, W. O. Smith
1951, Eos, Transactions, American Geophysical Union (32) 282-283
Smith provides an illuminating consideration of infiltration through soil in relation to the structure and texture of the soil its moisture content, and the variation of infiltration for A, B, and C soil zones. The organic nature of soil might also be stressed. Rotting rootlets provide passageways for water in...
Water resources of southeastern Bucks County, Pennsylvania
Jack B. Graham, John W. Mangan, Walter F. White
1951, Circular 104
This report has been prepared as a contribution to the development of southeastern Bucks County, Pa. It summarizes available information on the water resources of this 90-square mile area and evaluates current supplies. Future development of the area may change both the available quantity and the quality of the water...
Surface-water supplies of the Mesabi Iron Range
U.S. Geological Survey
1951, Bulletin 5
No abstract available....
Preliminary statement of the analyses of ground water from the Morrison Formation, southwestern Colorado and southeastern Utah
David A. Phoenix
1951, Trace Elements Memorandum 137
As part of a study of the carnotite deposits of the Colorado Plateau,, samples of ground water from the Salt Wash sandstone and Brushy Basin shale members of the Morrison formation have been analyzed to determine their chemical character and metal content. The Salt Wash ground water is largely a...
Ground water in alluvial deposits in Oklahoma
S.L. Schoff, E.W. Reed
1951, Economic Geology (46) 76-83
Alluvium along main streams in Oklahoma has long been recognized as a generally dependable aquifer. Pumping tests made in recent years afford a means of comparing one area with another. They indicate coefficients of transmissibility on the order of 70,000 gallons per day per foot in the Arkansas River alluvium near Fort Gibson, and 60,000 in the North Canadian...
Preliminary report on the geology and ground-water supply of the Newark, New Jersey, area
Henry Herpers, Henry C. Barksdale
1951, Special Report (New Jersey Division of Water Policy and Supply) 10
In the Newark area, ground water is used chiefly for industrial cooling, air-conditioning, general processing, and for sanitary purposes. A small amount is used in the manufacture of beverages. Total ground-water pumpage in Newark is estimated at not less than 20,000,000 gallons daily. The Newark area is underlain by formations of...
Fluorometric determination of zirconium in minerals
W.C. Alford, L. Shapiro, C. E. White
1951, Analytical Chemistry (23) 1149-1152
The increasing use of zirconium in alloys and in the ceramics industry has created renewed interest in methods for its determination. It is a common constituent of many minerals, but is usually present in very small amounts. Published methods tend to be tedious, time-consuming, and uncertain as to accuracy. A...
Geology and ground-water resources of the Santa Maria Valley area, California, with a section on surface-water resources
George Frank Worts, H. G. Thomasson Jr.
1951, Water Supply Paper 1000
No abstract available....
Kansas-Missouri floods of July 1951
Water Resources Division, U.S. Geological Survey
1951, Circular 151
No abstract available....
An aquarium experiment on the American eel as a predator on larval lampreys
Alfred Perlmutter
1951, Copeia (1951) 173-174
The parasitic sea lamprey, Petromyzon marinus, has in recent years spread throughout Lakes Huron and Michigan and is now firmly established in these waters (Applegate, 1949, Mich. Cons., 18 (4): 13-15). Coincident with their spread, the abundance of lake trout, Salvelinus namaycush, has declined...
Downstream movement of recently transformed sea lampreys, Petromyzon marinus, in Carp Lake River, Michigan
Vernon C. Applegate, Clifford L. Brynildson
1951, Transactions of the American Fisheries Society (81) 275-290
In order to obtain more precise information concerning the downstream movement of recently transformed sea lampreys, a trapping device was operated in the Carp Lake River, Emmet County, Michigan, from October, 1948, to July, 1951. The period of downstream migration typically extends from the latter part of October to...
Conservation: Where we stand: Review of Water, land, and people
Luna Bergere Leopold
1951, The Living Wilderness (36)
A distinguished conservationist, just returned from more than a year in those Pacific islands held in trust by the United States, reports that representatives of the government there are nearly completely concerned with the maintenance of an administrative organization. Actual advances in matters of land use, of maintaining the material...
Vegetation of Southwestern watersheds in the nineteenth century
Luna Bergere Leopold
1951, Geographical Review (41) 295-316
The recollections of many old-timers who tell of grass “stirrup high” have given rise to the idea that vegetation in the Southwest was uniformly better in the middle of the last century than it is at present. The change is usually attributed to overgrazing, which timed if it did not...
Ground-water situation in Oregon
R. C. Newcomb
1951, Report
The water that occurs beneath the land surface follows definite and well-known rules of hydraulics, the same as water on the surface. However, ground water must be studied by methods, some of which are unique to that type of water occurrence, in order to evaluate the part it plays in...
A state‐wide program of periodic measurements of ground‐water level In Nebraska
L.K. Wenzel
1951, Eos, Transactions, American Geophysical Union (16) 495-498
The precipitation in Nebraska has been considerably less than normal in the last four years, and in consequence the ground‐water level in many parts of the State has declined to a marked extent. Moreover, in some parts of Nebraska the ground‐water level has declined as the result of land‐drainage, and in other parts it has risen as the result of irrigation with water diverted from streams. These changes in ground‐water level produced by drainage, irrigation, and decreased precipitation have caused...
Ground water in the Escalante Valley, Beaver, Iron, and Washington Counties, Utah
Philip F. Fix, W.B. Nelson, B. E. Lofgren, R.G. Butler
1950, Technical Publication 6
Escalante Valley in southwestern Utah is one of the largest and most important ground-water areas of the State, with 1,300 square miles of arid land and an additional 1,500 square miles in its tributary drainage basin. Ground water is obtained from gravel and sand beds in the unconsolidated valley fill....
Subsurface reconnaissance of glacial deposits in northeastern Kansas
J.C. Frye, K.L. Walters
1950, Kansas Geological Survey Bulletin (86) 141-158
Pollution in the lower Columbia Basin in 1948 with particular reference to the Willamette River
F. F. Fish, R.R. Rucker
1950, Special Scientific Report - Fisheries 30
Development of the salmon resources of the lower Columbia River Basin appears as sound insurance against the threat of a serious reduction in the runs to the upper river areas through the multiple-purpose programs of water development now under way by the Corps of Engineers, the Bureau of Reclamation, and...
Geology and ground-water resources of Rice County, Kansas:
O. S. Fent
1950, Kansas Geological Survey Bulletin (85)
Subsurface reconnaissance of glacial deposits in northeastern Kansas
J.C. Frye, K.L. Walters
1950, Kansas Geological Survey Bulletin (86) 141-158
Preliminary report on the ground-water resources of southwestern Skagit County, Washington
Jack E. Sceva
1950, Ground-water Report 1
The ground-water resources of Montgomery County, New York
R.M. Jeffords
1950, Bulletin GW-23
The ground-water resources of Schoharie County, New York
J.M. Berdan
1950, Bulletin GW-22
The ground-water resources of Rensselaer County, New York
R.V. Cushman
1950, Bulletin GW-21
Toxicity and repellency to rats of actidione
R. Traub, J.B. DeWitt, J.F. Welch, D. Newman
1950, Journal of the American Pharmaceutical Association, Scientific Edition (39) 552-555
The antibiotic actidione was found to be highly repellent to laboratory rats and to significantly reduce gnawing attacks upon treated paperboards. Rats refused to accept food or water containing this material even under conditions of acute starvation and died of starvation and thirst rather than accept water containing 1.0 mg. of...