inner mongolia typical steppe

基本解釋

The available P in calcareous soil is usually low because of the interaction between P and calcium in the typical steppe in Inner Mongolia.
在土壤中，由於磷元素與土壤組分的相互作用，特別是在石灰性土壤中常使得土壤中磷的有傚性降低。
From 1992~1995, the effects of experimental grazing pressures on the community of Scarabaeoidea Larvae in Inner Mongolia typical steppe was studied.
研究了不同放牧強(qiáng)度下內(nèi)矇古典型草原蠐螬群落特征的變化。
Soil respiration was measured with a closed static chamber method for continuous two years (2001~2002) in fenced and grazing typical Leymus chinensis steppe, Inner Mongolia, China.
基於靜態(tài)箱式法，在內(nèi)矇古典型羊草草原圍欄與自由放牧樣地對(duì)土壤呼吸作用及其影響因子進(jìn)行連續(xù)兩年野外對(duì)比觀測(cè)。