Xenia Slavica 1975
DOI: 10.1515/9783111396835-015
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The OCS Aorists: A Problem in Generative Description

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“…However, our results demonstrate the strong influence soil moisture has on soil properties as indicated by the negative relationships between soil water content and ρ b or SPR (Table 4). This is consistent with past research that has showed decreased potential for soil compaction as soil moisture decreases below field capacity (Boufford & Carrow, 1980; Lunt, 1952; Swartz & Kardos, 1963).…”
Section: Resultssupporting
confidence: 92%
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“…However, our results demonstrate the strong influence soil moisture has on soil properties as indicated by the negative relationships between soil water content and ρ b or SPR (Table 4). This is consistent with past research that has showed decreased potential for soil compaction as soil moisture decreases below field capacity (Boufford & Carrow, 1980; Lunt, 1952; Swartz & Kardos, 1963).…”
Section: Resultssupporting
confidence: 92%
“…Soil water content at the time of traffic can play a large role in the amount of compaction. Specifically, maximum soil compaction usually occurs when soil water content is near field capacity, but the potential for compaction decreases as soil moisture decreases below or increases above field capacity (Lunt, 1952; Swartz & Kardos, 1963). Boufford and Carrow (1980) confirmed this in a stand of ‘Kentucky 31’ tall fescue [ Festuca arundinacea Schreb.…”
Section: Introductionmentioning
confidence: 99%