土壤水分特征曲线在作物非充分灌溉适宜水分下限确定中的应用
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2007
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Resumo |
SPAC系统中水总是从水势高处流向水势低处,土壤水势的高低是影响植物根系吸水速率的主要因素。相对于土壤含水量来说,用土壤水势作作物非充分灌溉的下限指标更具科学性,更利于水分下限指标的推广应用。试验结果表明,对于整个生育期来说,-200 kPa是比较适宜的大棚番茄土壤水势下限。在这一指标的推广过程中,须先测定当地土壤水分特征曲线,并从曲线上找出该适宜水势对应的土壤含水量,通过控制土壤含水量达到控制土壤水势的目的,从而实现精量灌溉。 Water always flows from higher water potential to the lower one in SPAC system.And water potential is the main element that influences the plant water uptake rate.Compared with the soil water content,it will be much more scientific to use the soil water potential as the lowest limit index of crop non-sufficient irrigation and be easier to be applied and extended.The experimental results show that-200 kPa is a more suitable lower limit of soil water potential to the tomato in greenhouse.During application of... |
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Idioma(s) |
中文 |
Fonte |
刘超, 汪有科, 张立强.土壤水分特征曲线在作物非充分灌溉适宜水分下限确定中的应用.灌溉排水学报,2007,6:76-78 |
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期刊论文 |