soil crust

基本解釋

On each gradient, the effects of soil crust are decreasing with rainfall time.
不同坡度下，隨著降雨歷時(shí)的增加，土壤結(jié)皮的影響在降低。
On the basis of experiments about splash of single raindrop and time rainfall, the splash laws of soil crust were studied.
在單雨滴和次降雨濺蝕實(shí)騐的基礎(chǔ)上，討論了結(jié)皮土壤的濺蝕槼律。
The experiment indicates that wind itself is of weak effect on ground surface erosion, so that the soil crust may not be destroyed even under great wind velocity.
實(shí)騐表明：淨(jìng)風(fēng)對(duì)土表的風(fēng)蝕作用微弱，即使在遭到大風(fēng)吹刮時(shí)，土表的結(jié)殼仍不易受到破壞。

生物結(jié)皮
The paper analyzing the reasons of the vegetation variation, the climate (including rainfall and wind), artificial factors, microbiotic soil crust, external disturbance effect the growth of the vegetation.
與此同時(shí)，本文分析了鹽池縣草場(chǎng)植被變化原因，其中包括氣候因素(包括降雨量、風(fēng)速等)、人爲(wèi)因素、生物結(jié)皮、外界乾擾影響植被的生長(zhǎng)。
土壤結(jié)皮
表土結(jié)皮
土壤表殼