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1)  ecological store water capacity of soil
土壤生态蓄水量
1.
The paper obtained chloride concentration of precipitation and soil moisture in lab firstly,and according to chemical conservation law,which is the chloride mass-balance law of precipitation and soil moisture of unsaturated zone,calculated ecological store water capacity of soil in three sorts of landforms,mound,tableland and bench in Changchun.
通过实验测得降水及土壤水的氯离子浓度,依据化学守恒原理,即降水与包气带土壤水中氯离子的质量守恒关系,计算出长春市丘陵、台地、阶地3类不同地貌区土壤一年内所得水量,该水量为土壤生态蓄水量
2)  soil water storage
土壤蓄水量
1.
The results showed that there was a significant difference in the soil water storage among different months,and the dynamics of soil water could be divided into the phases of reduction,increase,and more reduction.
结果表明:不同月份间土壤蓄水量差异极显著(P<0。
2.
Comparative experiments on the function of soil water storage and characteristics of runoff and sediment loss under Vernica fordii plantation and Eucommia ulmoides plantation in the hilly red soil region were applied.
结果表明:杜仲人工林林冠枝叶最大持水容量及林地凋落物吸水容量均高于油桐人工林;杜仲林地0~140cm土层年均土壤蓄水量达到239。
3.
The results showed that there was a significant difference in the soil water storage among different months, and the dynamics of soil water could be described as the phases of accumulation, depletion, and stabilization.
结果表明:不同月份间土壤蓄水量差异达极显著水平,研究时段内土壤水分动态变化可划分为土壤水分积累期、土壤水分消耗期和土壤水分稳定期3个时期;油桐人工林土壤水分垂直变化显著,且不同季节的变化规律各异;土壤蓄水量与大气相对湿度(RH)、大气温度(t)、饱和水汽压差(VPD)、降雨量(R)等气象因子显著相关(P<0。
3)  soil water storage capacity
土壤蓄水量
1.
In comparison with farmlands,total soil water storage capacity on woodlands.
0—40 cm土层土壤蓄水量为228。
2.
Based on the indexes including soil moisture constant,soil water storage capacity and soil water storage capacity surplus-deficit status defined by its attribute extent of farmland soil moisture,the objective zoning of surplus-deficit status of farmland soil moisture of Heilongjiang Province was created.
依据对农田土壤水分状况的表征程度 ,确定了包括土壤水分常数、土壤蓄水量以及土壤蓄水量盈亏值三类共计 9个指标 ,对黑龙江省农田土壤水分盈亏状况进行了较为客观的分区。
3.
The geographical distribution,vertical distribution,growing seasonal distribution and the surplus-deficit status of soil moisture in regional farm land are analyzed by using the index of soil water storage capacity based on the field real data.
在农田土壤水分实测资料的基础上,以土壤蓄水量为指标研究了黑龙江省区域农田土壤水分的地理分布特征、垂直分布特征、随生长季的变化规律以及盈亏状况。
4)  effective soil water store capacity
土壤有效蓄水量
5)  initial soil water content
旬初土壤蓄水量
1.
The ten-day correlation forecast model of rainfall and runoff based on BP neural network was established by taking actual initial soil water content and ten-day rainfall as its inputs and the actual ten-day runoff as its output,according to the watershed characteristics of rainfall and runoff correlation.
参照流域暴雨与径流相关的特点,以实际的旬初土壤蓄水量、旬降雨量为输入条件,以实际的旬径流量为输出条件,建立BP神经网络旬降雨径流相关模型。
6)  soil water conservation
土壤蓄水
补充资料:环境土壤和植物生态生物化学
由我国著名土壤生物学家、原中国农业科学院土肥所所长、国务院特殊津贴获得者闵九康教授担任总编的大型农科专著《环境土壤和植物生态生物化学》诚邀科目主编和参编学者.有意者请与中国高端论文网联系.
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