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土壤呼吸作用及其影響因子進行連續(xù)兩年野外對比觀測。