Zobrazeno 1 - 10
of 21
pro vyhledávání: '"J. R. Hoover"'
Autor:
J. R. Hoover
Publikováno v:
Transactions of the ASAE. 33:1843-1850
A field cross-section instrumented with transducer water potential sensors and with seep and runoff detectors was used to evaluate the size of the area contributing surface runoff to a stream. Runoff and seep detectors were designed as water-activate
Publikováno v:
Transactions of the ASAE. 23:1424-1427
THE effects of soil air entrapment and subsurface drainage on infiltration into a sand were investigated in the laboratory under simulated rainfall conditions. When soil air was free to escape from the sample through a subsurface drain, the drain sta
Publikováno v:
Transactions of the ASAE. 28:1598-1601
THE effect of entrapped soil air on soil erosion during simulated rainfall was investigated. A rotating disc rainfall simulator generated laboratory rainstorms of 220 mm/h intensity with raindrop characteristics similar to those of natural rainfall.
Publikováno v:
Transactions of the ASAE. 31:0761-0768
AFTER exposure to several different initial rainfall durations and rainfall sequences, the constant-head cumulative infiltration of water into disturbed Hagerstown silt loam Ap horizon soil samples of two aggregate sizes was measured. The Green-Ampt
Publikováno v:
Transactions of the ASAE. 27:0093-0098
THE effects of soil air entrapment on erosion and infiltration were investigated by two laboratory studies, one with a fallow soil and one with a grass cover. Both the fallow soil and the grass cover experiment had a zone which restricted the downwar
Autor:
A. R. Jarrett, J. R. Hoover
Publikováno v:
Transactions of the ASAE. 28:179-182
INFILTRATION rate tests were run on a sand and on a loam soil after the natural soil air was evacuated and replaced with C02 gas. When the C02 was free to escape at atmospheric pressure, the infiltration rates were 50% higher in the sand and 56% high
Autor:
W. J. Grant, J. R. Hoover
Publikováno v:
Transactions of the ASAE. 26:1401-1408
A procedure is described to calculate the coefficients of the Gardner (1958) hydraulic conductivity and Taylor and Luthin (1969) moisture content equations from soil moisture characteristic data. A computer program fits the equations K = d/(hC3 + C2)
Publikováno v:
Transactions of the ASAE. 28:1878-1884
TIME dependent relationships between soil detachment and splash, soil shear strength and the depth of ponded water on the soil surface are developed for Hagerstown silt loam under simulated rainfall. Soil splash rate was highly correlated to soil she
Publikováno v:
Transactions of the ASAE. 30:0158-0161
SOIL loss from 99-mm diameter laboratory samples of Hagerstown silty clay loam soil was measured under 55 mm/h simulated rainfall. The soil losses from two aggregate size distributions of the same soil were compared. When rain was applied in differen
Autor:
J. R. Hoover, A. R. Jarrett
Publikováno v:
Transactions of the ASAE. 32:1358-1364
The effect of soil air entrapment on surface runoff rate and quantity was evaluated in the field using shallow subsurface drainage and tillage treatments to modify the amount of air trapped in a fragipan soil. The volume of pore space filled with air