封丘地区土壤水分平衡研究Ⅲ.根层边界的水分通量
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RESEARCH ON SOIL WATER BALANCE IN FENGQIU REGION Ⅲ.WATER FLUX PASS THROUGH THE BOUNDARY OF ROOT ZONE
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    摘要:

    本文用一组张力计和中子水分计同步监测的剖面土水势和含水量的资料,通过零通量面法计算根层边界的水分通量;在剖面没有零通量面出现时,则用根层边界附近的土水势资料和预先测定的土壤导水率资料,通过达西公式计算其水流通量。结果表明,在水位较浅条件下,根层边界不仅有向上水流发生,而且在附近抽水灌溉引起水位急剧下降条件下,也有短期的向下水流发生,使深层土壤水分流出根层边界,对根系供水产生负的影响。

    Abstract:

    Under conditions of shallow water table,water flux pass through the root zone boundary is an unneglected component on calculation of water balance.With simultaneous measurements of soil water potential by a serise of tensiometers and of soil water content by neutron probe meter in soil profile,water flux pass through the boundary of root zone can be calculated by zero flux place method.However,if zero flux plane isn't appeared in the profile,it can be calculated by Darcy's formula with measurements of soil water potential near the boundary and soil water conductivities which are obtained beforehand.In a process of irrigation of wheat field by pumping water from well,zero flux plane was found in nonirrigated wheat field near the boundary of root zone,and its depth was followed by the fluctuation of water table.There fore,there was not only upward flux pass through the boundary during this process but also downward flux which was unfavourable for water supply to root system.

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陈志雄,Vauclin Michel.封丘地区土壤水分平衡研究Ⅲ.根层边界的水分通量[J].土壤学报,1991,28(1):66-72. Chen Zhixiong, Vauclin Michel. RESEARCH ON SOIL WATER BALANCE IN FENGQIU REGION Ⅲ. WATER FLUX PASS THROUGH THE BOUNDARY OF ROOT ZONE[J]. Acta Pedologica Sinica,1991,28(1):66-72.

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  • 在线发布日期: 2013-02-25
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