Wheat stubble height effects on soil water capture and retention during long fallow

2021 ◽  
Vol 256 ◽  
pp. 107117
Author(s):  
William F. Schillinger ◽  
Stewart B. Wuest
Keyword(s):  
2009 ◽  
Vol 60 (8) ◽  
pp. 730 ◽  
Author(s):  
P. R. Ward ◽  
K. Whisson ◽  
S. F. Micin ◽  
D. Zeelenberg ◽  
S. P. Milroy

In Mediterranean-type climates, dryland soil water storage and evaporation during the hot and dry summer are poorly understood, particularly for sandy-textured soils. Continued evaporation during summer, and any effects of crop stubble management, could have a significant impact on annual components of the water balance and crop yield. In this research, the effect of wheat stubble management on summer evaporation and soil water storage was investigated for a sandy soil in south-western Australia, during the summers of 2005–06 and 2006–07. Treatments comprised: retained standing stubble; retained flattened stubble; removed stubble; and removed stubble followed by burying the crowns with topsoil from an adjacent area. Under ‘dry’ conditions, evaporation continued at ~0.2 mm/day. In contrast to previous results for finer textured soil types, stubble retention did not decrease the rate of evaporation, but marginally (10–30%) increased evaporation on 7 out of 14 days when measurements were taken. Significant differences due to stubble management were observed in two successive summers, but only for relatively dry soil conditions. There were no significant differences observed for several days after irrigation or rainfall. Under dry conditions in the absence of rainfall, total decrease in water storage during a 90-day summer period could be ~20 mm, but differences attributable to stubble management are likely to be a few mm.


1983 ◽  
Vol 23 (122) ◽  
pp. 302 ◽  
Author(s):  
BJ Radford ◽  
RGH Nielsen

The practices of stubble mulching and water injection were tested to determine what extension of crop sowing time they provided during dry weather at four sites on the Darling Downs, Queensland (Acland, Toowoomba, Moola and Dalby). Crops tested were wheat, sunflower, sorghum and maize. Crop residues (wheat, barley and sorghum) retained on the soil surface as mulches reduced soil water loss from the seedbed after prolonged soil drying. This resulted in a lower rainfall requirement to refill a mulched seedbed, despite some absorption of rainfall by the mulch itself. A lower rainfall requirement could make sowing possible on a mulched but not an unmulched seedbed, given a suitably marginal sowing rain. Higher soil water contents under mulch increased seedling emergence of wheat, sunflower, sorghum and maize after prolonged soil drying. This effectively extended sowing time. On the assumption that sowing time was the period that resulted in crop emergence > 50%, extensions of sowing time were determined from graphs of emergence vs time. For example, about 2000 kg/ha of wheat stubble at Acland extended the sowing time of sunflower (6 cm deep) by 4.0 d. Water injection at 60 ml/m extended sorghum, sunflower and maize sowing time by up to 2.5 d in dry soil but reduced sowing time of these three crops at high soil water levels (under mulch). It was concluded that the additional periods of sowing time obtained during dry weather from stubble mulching or water injection could help distribute the peak demand for labour during sowing operations more evenly.


Author(s):  
M.C.H.Mouat Pieter Nes

Reduction in water content of a soil increased the concentration of ammonium and nitrate in solution, but had no effect on the concentration of phosphate. The corresponding reduction in the quantity of phosphate in solution caused an equivalent reduction in the response of ryegrass to applied phosphate. Keywords: soil solution, soil water content, phosphate, ryegrass, nutrition.


2010 ◽  
Vol 59 (1) ◽  
pp. 157-164 ◽  
Author(s):  
E. Tóth ◽  
Cs. Farkas

Soil biological properties and CO2emission were compared in undisturbed grass and regularly disked rows of a peach plantation. Higher nutrient content and biological activity were found in the undisturbed, grass-covered rows. Significantly higher CO2fluxes were measured in this treatment at almost all the measurement times, in all the soil water content ranges, except the one in which the volumetric soil water content was higher than 45%. The obtained results indicated that in addition to the favourable effect of soil tillage on soil aeration, regular soil disturbance reduces soil microbial activity and soil CO2emission.


2005 ◽  
Vol 33 (1) ◽  
pp. 185-188 ◽  
Author(s):  
Csilla Farkas ◽  
Roger Randriamampianina ◽  
Juraj Majerčak

2005 ◽  
Vol 33 (1) ◽  
pp. 251-254 ◽  
Author(s):  
Éva Lehoczky ◽  
András Kismányoky ◽  
Tamás Kismányoky

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