1) bare soil
裸土
1.
A laboratory simulated rain experiment shows that the water retention capacity of green land is higher than that of bare soil with the same rainfall intensity,especially with a low rainfall intensity of 20～25 mL/min.
通过实验室模拟降雨,初步得出结论:在相同降雨强度的情况下,绿地相对于裸土而言具有较大滞水量。
2) bare soil index
裸土指数
3) bare loess slope
黄土裸坡
1.
With artificial simulation rainfall tests, runoff processes on the bare loess slope are studied and the following results are obtained: (1) Runoff rate varied with rainfall course and could be described with logarithmic (equations).
采用人工模拟降雨试验法对黄土裸坡降雨产流过程进行了研究。
4) evaporation of uncovered soil
裸土蒸发
5) soil bareness
土壤裸露
1.
Landscape fragmentation and soil bareness study in north Shaanbei Loess Plateau;
陕北黄土高原景观破碎化及其土壤裸露效应
2.
The Tower region of the Yan an City in the Loess Plateau is used as typical area for the studies of soil bareness, types and structure of landscape.
土壤裸露是水土流失具体的空间表现,同时又是导致进一步水土流失的重要因素。
6) Loess Denudation
黄土裸露
1.
On the Administrative Countermeasure of Loess Denudation in the Park of Baoan Distrisct in Shenzhen
深圳市宝安区公园黄土裸露管理对策探讨
补充资料：净裸裸
【净裸裸】
（杂语）又云赤裸裸。天真独朗无纤毫情尘之称。碧岩九则评唱曰：“须是透过关捩子，出得荆棘林，净裸裸，赤洒洒。”
（杂语）又云赤裸裸。天真独朗无纤毫情尘之称。碧岩九则评唱曰：“须是透过关捩子，出得荆棘林，净裸裸，赤洒洒。”
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