高山草甸土

青海高山草甸土的形成及其肥力评价

Formation and fertility of the alpine meadow soil in Qinghai Province

土壤类型多属于高山草甸土，主要理化性质各样地间存在一定差异。

The soil type belongs to the alpine meadow soil , there is difference among various kinds of plots in Soil characteristics .

不同植被类型高山草甸土呼吸作用的研究

Studies on respiration of soils under different vegetations of the alpine meadow

长期定位连施化肥的增产培肥效应研究亚高山草甸土青稞肥料效应与优化施肥研究

Effect of long-term located continuous fertilizer application on yield increasing and soil fertility developing

亚高山草甸土的土壤有机碳储量最多，为2660.22万吨。

Subalpine meadow soil organic carbon storage in the soil the most , 26,602,200 tons .

超高硝酸铵负载凝胶态缓释肥的节肥节水效应亚高山草甸土青稞肥料效应与优化施肥研究

The Effect of Superhigh Ammonium Nitrate Loading Gel-State Slow Release Fertilizer on Fertilizer and Water Saving

亚高山草甸土青稞肥料效应与优化施肥研究不同施肥模式下潮棕壤微量元素含量及其变化状况

Effects of Different Fertilization Treatments on Contents and Changes of Trace Elements in Aquic Brown Soil

亚高山草甸土纤维素分解过程及与环境因子的对应关系

Decomposition process of cellulose in sub-high mountainous meadow soil and effects of climatic factors on the decomposition

高山草甸土C~（14）测定的绝对年令距今为1860±95年。

The absolute age of alpine meadow soil which was determined by C ~ ( 14 ) is 1860 ± 95 year .

再次为高山草甸土、山地黑钙土和山地栗钙土，它们的土壤有机碳含量很相近，分别为699.5万吨，878.98万吨，778.37万吨。

Again for the alpine meadow soil , mountain chernozem and chestnut soil , the soil organic carbon content are very similar , were 6.995 million tons , 8.7898 million tons , 7.7837 million tons .

单位土壤水文效应亚高山灌丛草甸土>山地森林灰褐土>山地栗钙土；

Hydrology effect of soil unit depth was sub-alpine shrub meadow soil > forest gray-brown soil > chestnut soil ;

高山土区（高山草甸土及高山草原土）。最后文章对中国农业土壤集约耕作的发展前景进行了初步展望。

Finally , the prospectives for the development of intensive cultivation of agricultural soils in China are discussed .