1) soil water storage
土壤贮水量
1.
Through the multipoint location determination on soil water storage of different vegetation types in the middle and lower reaches of Nenjiang River Valley,the results show that the soil water storage of Pinus sylvestris var.
通过对嫩江中下游地区不同植被类型土壤贮水量进行的多点定位观测,定量研究了不同森林植被对土壤贮水量的影响关系,结果表明:樟子松林分土壤贮水量大于小黑杨林分土壤贮水量,其幅度为3-56 mm,且两者都显著大于对照农田的土壤贮水量。
2.
Based on the observational material from the experimental plots, we describe the roles of dynamic changes in rainfall, evapotranspiration, surface runoff, subdrainage and soil water storage on soil water cycle in latosolic red soil.
根据定位点的实测资料，阐述了南亚热带丘陵赤红壤试区的降雨、蒸散、地表径流、深层贮水和土壤贮水量的动态变化在土壤水分循环中的作用。
3.
Soil water storage decreased 12.
利用门源气象站1982-2005年农业气象观测资料,统计分析得出:1982-2005年0-50cm 门源油菜地土壤贮水量以16。
2) available water content of soil
土壤有效贮水量
3) Soil water-holding
土壤贮水
1.
research on characteristics of soil water-holding and infiltration were carried out.
700 t/hm3;土壤贮水量随土壤容重和孔隙度变化的差异不显著,土壤持水率随土壤容重和孔隙度变化的差异极显著。
2.
③Characteristics of soil capillary,non-capillary porosity water-holding capacity,soil total absorption precipitation and effective precipitation show this order: Robinia pseudoacacia > Populus euramericana > Fraxinus chinensis > bare land,and soil water-holding capacity in 0-20 cm is better than that of 20-40 cm.
以无林地为对照,对黄河三角洲滩地3种林分类型的土壤水文物理性状、土壤入渗特性及土壤贮水性能进行研究。
4) root-zone water storage
植物根区土壤贮水量
1.
In soil-plant-atmosphere continuum,plant root-zone water storage is an important water source.
在土壤-植物-大气连续统中,植物根区土壤贮水量是一个重要水源。
5) soil carbon storage
土壤碳贮量
1.
tereticornis and Acacia mangium plantations on the soil physical properties and soil carbon storage in Hainan Island, China is studied in the paper.
天然林被人工林取代后对土壤水文物理性质及土壤碳贮量有重要的影响。
6) carbon reserves of forest soil
森林土壤碳贮量
补充资料：土壤水分运动基本方程(见土壤水运动)
土壤水分运动基本方程(见土壤水运动)
turang shuifen yundong iiben土壤水分运动基本方程fangeheng见土壤水运动。
说明：补充资料仅用于学习参考，请勿用于其它任何用途。
参考词条