首页|青藏高原高寒草原生态系统土壤氮磷比的分布特征

青藏高原高寒草原生态系统土壤氮磷比的分布特征

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采用野外调查和室内分析相结合的方法,研究了青藏高原高寒草原生态系统土壤N/P的分布特征。结果表明:青藏高原高寒草原生态系统土壤N/P总体上呈现出西高东低、斑块状交错分布的格局,N/P的高值区主要集中在藏北高原腹地和喜马拉雅北麓湖盆区,不同草地类型和不同自然地带土壤N/P差异显著。不同草地类型土壤N/P自上而下可分为低-高-低-高型、低-高-低型、低-高型、高-低-高-低型和高-低-高型等5个类型,表土层与底土层N/P差异显著。土壤N/P与0~20 cm土壤容重、20~ 30 cm土壤含水量、速效钾、全氮含量显著正相关,与20~ 30 cm土壤容重、土壤速效磷和全磷含量显著负相关。
Soil N/P ratio distribution characteristics of alpine grassland ecosystem in Qinghai-Tibet Plateau
The distribution characteristics of soil N/P ratio in alpine grassland ecosystem of Qinghai-Tibet Plateau were surveyed by field investigation and laboratory analysis.Horizontally,soil N/ P ratio was generally higher in west and lower in east in a manner of staggered patch distribution,with higher N/P ratios mainly centralized in the hinterland of northern part of Tibet Plateau and in the lake basin area of the northern foot of Himalayas.Significant differences in soil N/P ratio were observed among grassland types and natural transects.Vertically,the distribution of N/P ratio along the soil profile from aboveground to underground among different grass types could be categorized into five patterns,including low-high-low-high,low-high-low,low-high,high-low-high-low,and high-low-high.The N/P ratio showed a significant positive correlation with soil bulk density at 0-20 cm depth,soil water content at 20-30 cm depth,contents of soil available K and total nitrogen,respectively.However,it showed significant negative correlation with soil bulk density at 20-30 cm depth,contents of soil available P and total P,respectively.

Qinghai-Tibet Plateaualpine grasslandsoilN/P ratio

王建林、钟志明、王忠红、陈宝雄、张宪洲、沈振西、胡兴祥、大次卓嘎

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西藏农牧学院植物科学学院,西藏林芝860000

中国科学院地理科学与资源研究所,北京100101

青藏高原 高寒草原 土壤 N/P

国家自然科学基金“十二五”国家科技支撑计划项目

410610082011BAD17B05-4

2013

应用生态学报
中国生态学学会 中国科学院沈阳应用生态研究所

应用生态学报

CSTPCDCSCD北大核心
影响因子:2.114
ISSN:1001-9332
年,卷(期):2013.24(12)
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