Soil Organic Carbon and Nutrients along an Alpine Grassland Transect across Northern Tibet
Soil Organic Carbon and Nutrients along an Alpine Grassland Transect across Northern Tibet作者机构：Institute of Mountain Hazards&Environment Chinese Academy of Sciences Graduate University of Chinese Academy of Sciences
出 版 物：《Journal of Mountain Science》 (山地科学学报（英文）)
年 卷 期：2013年第10卷第4期
页 面：564-573页
核心收录：
基 金：supported by the Western Action Plan Project of the Chinese Academy of Sciences(Grant No.KZCX2-XB3-08) the Strategic Pilot Science and Technology Projects of Chinese Academy of Sciences(Grant No.XDB03030505) the One Hundred Young Persons Project of the Institute of Mountain Hazards and Environment(Grant No.SDSQB-2010-02)
主 题：Soil organic carbon Total nitrogen Total phosphorus Particle size distribution Alpinegrassland Tibet
摘 要：Soil carbon and nutrient contents and their importance in advancing our understanding of biogeochemical cycling in terrestrial ecosystem, has motivated ecologists to find their spatial patterns in various geographical area. Few studies have focused on changes in the physical and chemical properties of soils at high altitudes. Our aim was to identify the spatial distribution of soil physical and chemical properties in cold and arid climatic region. We also tried to explore relationship between soil organic carbon （SOC） and total nitrogen （TN）, total phosphorus （TP）, available nitrogen （AN）, available phosphorus （AP）, soil particle size distribution （PSD）. Samples were collected at 44 sites along a 300 km transect across the alpine grassland of northern Tibet. The study results showed that grassland type was the main factor influencing SOC, TN and TP distribution along the Gangdise Mountain-Shenzha-Shuanghu Transect. SOC, TN and TP contents were significantly higher in alpine meadow than alpine steppe ecosystems. SOC, TN, TP and AN contents in two soil layers （0-15 cm and 15-3o cm） showed no significant differences, while AP content in top soft （0-15 cm） was significantly higher than that in sub-top soil （15-30cm）. SOC content was correlated positively with TN and TP content （r = 0.901and 0.510, respectively）. No correlations were detected for clay content and fractal dimension of particle size distribution （D）. Our study results indicated the effects of vegetation on soil C, N and P seem to be more important than that of rocks itself along latitude gradient on the northern Tibetan Plateau. However, we did not found similar impacts of vegetation on soil properties in depth. Inaddition, this study also provided an interesting contribution to the global data pool on soil carbon stocks.
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