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首页> 外文期刊>Journal of the Indian Society of Soil Science >Development of Pedotransfer Functions for Penetration Resistance of Few Soils under Major Soil Orders of India
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Development of Pedotransfer Functions for Penetration Resistance of Few Soils under Major Soil Orders of India

机译:印度主要土壤次序下几种土壤抗渗透能力的Pedo传递函数的发展

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Pedotransfer functions for soil penetration resistance were developed for soils belonging to soil orders Inceptisols, Alfisols and Vertisols. For upland crops grown on Inceptisol and Alfisol, soil water content (SWC) along with bulk density (BD) accounted for nearly 72-85% variation in penetration resistance (PR). However, under saturated soil water conditions during lowland rice cultivation on Inceptisols and Vertisols, the correlation between PR and BD was between 64-78%. It was further observed that for most BD's, at lower SWG, PR was higher under Alfisols than Inceptisols but trend reversed at relatively higher SWC. Above developed pedotransfer functions are of great importance in calculating soil water content at 2MPa soil strength (SWC_(2MPa))which is the soil water content below which plant experiences severe stress and is now being considered as the critical soil water content at which irrigation should be recommended. They are also useful in calculating the soil water stress period experienced by growing upland crops under different irrigation schedules. Computation of SWC_(2MPa) from above developed regression equations showed an increase with increase in bulk density and clay content. There was an increase of 4-5% in the value of SWC_(2MPa) at maturity over its value at initial stage.
机译:已开发了针对土壤渗透阻力的Pedotransfer函数,用于属于土壤阶Inceptisols,Alfisol和Vertisols的土壤。对于在Inceptisol和Alfisol上生长的旱作作物,土壤含水量(SWC)和堆积密度(BD)构成了抗穿透力(PR)的近72-85%。然而,在低陆稻米上使用Inceptisols和Vertisols进行的饱和土壤水分条件下,PR和BD之间的相关性在64-78%之间。进一步观察到,对于大多数BD,在SWG较低时,Alfisol下的PR高于Inceptisols,但在相对较高的SWC下趋势却相反。以上开发的pedotransfer函数对于计算2MPa土壤强度(SWC_(2MPa))下的土壤含水量非常重要,SWC_(2MPa)是低于该土壤含水量的植物,在该土壤含水量承受严重压力的情况下,现在被认为是灌溉时的临界土壤含水量。被推荐。它们还可以用于计算在不同灌溉时间表下种植旱地作物所经历的土壤水分胁迫期。从上面开发的回归方程计算SWC_(2MPa)随堆密度和黏土含量的增加而增加。成熟时SWC_(2MPa)的值比初始值增加了4-5%。

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