1970
DOI: 10.4141/cjss70-004
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Effect of Nonerodible Aggregates and Wheat Stubble on Initiation of Soil Drifting

Abstract: The wind velocity required to initiate movement of soil with varying amounts of standing wheat stubble and varying proportions of erodible and nonerodible soil aggregates was determined in a wind tunnel. The relationship between these variables was calculated as logeI = 6.0438 + 0.0001774 S + 0.02332 C where I is the initiating velocity in cm/sec as measured at a height of 30.5 cm above the soil surface, S is the amount of standing wheat stubble (approximately 15 cm tall) in kg/ha, and C is the percentage of s… Show more

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Cited by 22 publications
(17 citation statements)
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“…The maximum soil erosion hazard is in the spring at the end of a fallow period (Bisal and Ferguson 1970). About 200 g m -2 of plant residue are required to protect fine-textured soils from erosion (Bisal and Ferguson 1970).…”
Section: Discussionmentioning
confidence: 99%
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“…The maximum soil erosion hazard is in the spring at the end of a fallow period (Bisal and Ferguson 1970). About 200 g m -2 of plant residue are required to protect fine-textured soils from erosion (Bisal and Ferguson 1970).…”
Section: Discussionmentioning
confidence: 99%
“…About 200 g m -2 of plant residue are required to protect fine-textured soils from erosion (Bisal and Ferguson 1970). Both the FRYE and SRYE cover crops left sufficient total plant residue to protect the soil from erosion but there was insufficient residue following the NCOV treatment.…”
Section: Discussionmentioning
confidence: 99%
“…An average of 28% of the non-grain residue of HY320, and 2lVo of thatof \eepawa, was chaff (Cutforth et al 1988). Estimated stubble weight did not reach the 2000 ltg ha-' suggested as necessary for erosion protection in the Bisal and Ferguson (1970) For personal use only. environments.…”
mentioning
confidence: 95%
“…The amount of non-grain residue influences potential soil loss caused by wind erosion (Bisal and Ferguson 1970), and affects the efficiency of soil water storage during the fallow period by reducing evaporation and runoff, and trapping of snow (Smika and Unger 1986). McCalla and Army (1961) estimated that the amount of residue required to provide adequate erosion protection is approximately 800 kg ha-r for medium-textured soils, 1400 kg ha-' for fine-textured soils, and 2000 kg ha-r for coarse-textured soils.…”
mentioning
confidence: 99%
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