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- W2276770107 abstract "Randall clay (fine, smectitic, thermic Ustic Epiaquerts) is typical of the soils found in the bottomof playa lakes that are sometimes used as catchments for feedyard runoff in the Texas Panhandle. Theobjective of this research was to document the time-related sealing properties of cracked Randall Claywhen subjected to a rapid infiltration event. Soil cores that were 7.6 cm in diameter by 15 cm deep werecollected from two playa lakes in Randall County, Texas. The cores were air dried for one month, andcracking was documented using computer-aided tomography. The soil cores were subjected to infiltrationand saturated hydraulic conductivity tests in a flexible wall permeameter. The modified Kostiakovequation was used to describe the infiltration characteristics of each soil core. Cumulative infiltration after60 minutes varied from 0.15 to 1.60 cm, and the cores effectively sealed before water traveled more than8 cm. These infiltration rates are lower than values reported in earlier research. Saturated hydraulicconductivities varied from 3.2 x 10 -4 to 7.2 x 10 -7 cm/min with geometric means of 4.1 x 10 -6 and 1.4 x 10 -5cm/min at the two playas." @default.
- W2276770107 created "2016-06-24" @default.
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- W2276770107 date "2001-01-01" @default.
- W2276770107 modified "2023-09-26" @default.
- W2276770107 title "Infiltration Characteristics of Cracked Clay Soils in Bottoms of Feedyard Playa Catchments" @default.
- W2276770107 doi "https://doi.org/10.13031/2013.3520" @default.
- W2276770107 hasPublicationYear "2001" @default.
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