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1)  sandy soil
沙丘土壤
1.
The soil physical composition,organic matter,total nitrogen,total phosphorus, total potassium and pH of Salix psammophila ccheckerboard and contrast sand of Dalate county were investigated in 2005,the effects of Salix psammophila checkerboard on physical and chemical characteristics of sandy soil were analyzed.
设置沙柳沙障后沙丘土壤有机质含量是对照地的1。
2)  buried soil under sand dunes
沙丘埋藏土壤
1.
It has been long held that the buried soil under sand dunes on the major sand lands in northern China formed due to the climatic changes of the Holocene, which could be used as a proxy record to reconstruct the past climate in warm-humid periods.
本文对我国东北沙地沙丘埋藏土壤的形成原因重新进行了探讨。
3)  dunesand
沙丘沙土
4)  hilly soils
丘陵土壤
1.
On antierodibility of hilly soils in Zhejiang Province:;
浙江省丘陵土壤的抗蚀性
5)  hill soil
丘陵地土壤
6)  Soil desertification
土壤沙化
1.
Grassland degradation, land salinization and soil desertification(DSD) are typical ecoenvironmental problems in the west of Jilin Province.
基于地理信息系统平台,对吉林省西部1986年、1996年和2000年的土壤沙化、盐碱化和草原退化(简称"三化")专题数据、土地利用状况数据、基础地理数据、人文和经济统计数据等进行融合处理和分析。
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。
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