Author
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HALVORSON, J - WASHINGTON STATE UNIV. |
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McCool, Donald |
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PANNKUK, C - WASHINGTON STATE UNIV. |
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GATTO, L - DOD |
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KING, L - WASHINGTON STATE UNIV. |
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NISSEN, P - DOD |
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Submitted to: Agronomy Abstracts
Publication Type: Abstract Only Publication Acceptance Date: 5/1/1998 Publication Date: N/A Citation: N/A Interpretive Summary: Technical Abstract: Studies at Yakima Training Center (YTC) suggest freeze-thaw cycles reduce effects of soil compaction by military vehicles. However, we know little about the details of soil freezing and its effects. We monitored soil freezing during winter 1997-1998 at YTC using electrical resistivity probes. We also measured bulk density, penetration resistance and steady- state runoff rates in recently tracked and untracked soils, before and after winter. Patterns of freezing and thawing were most similar in compacted and uncompacted soil near the surface. At greater depths, freezing did not occur in compacted soil or occurred later than in uncompacted soil. Compacted soil had significantly higher surface bulk density, penetration resistance, and runoff rates than uncompacted soil soon after tracking. Data collected in spring 1998 document changes in soil parameters and stead-state surface runoff attributable to winter 1997- -1998. |
