Nitrogen isotopic composition of plants and soil in an arid mountainous terrain: south slope versus north slope
Chongjuan Chen,Yufu Jia,Yuzhen Chen,Imran Mehmood,Yunting Fang,and Guoan Wang
Chongjuan Chen
Beijing Key Laboratory of Farmland Soil Pollution Prevention-control
and Remediation, Department of Environmental Sciences and Engineering,
College of Resources and Environmental Sciences, China Agricultural
University, Beijing, 100193, China
Yufu Jia
Beijing Key Laboratory of Farmland Soil Pollution Prevention-control
and Remediation, Department of Environmental Sciences and Engineering,
College of Resources and Environmental Sciences, China Agricultural
University, Beijing, 100193, China
Yuzhen Chen
Beijing Key Laboratory of Farmland Soil Pollution Prevention-control
and Remediation, Department of Environmental Sciences and Engineering,
College of Resources and Environmental Sciences, China Agricultural
University, Beijing, 100193, China
Imran Mehmood
Key Laboratory of Plant-Soil Interactions, MOE, Department of Plant
Nutrition, College of Resources and Environmental Sciences, China
Agricultural University, Beijing, 100193, China
Beijing Key Laboratory of Farmland Soil Pollution Prevention-control
and Remediation, Department of Environmental Sciences and Engineering,
College of Resources and Environmental Sciences, China Agricultural
University, Beijing, 100193, China
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The south slope of Tian Shan differs from the north slope in environment. The study showed that leaf δ15N, soil δ15N and △δ15Nleaf-soil on the south slope were greater than those on the north slope. The significant influential factors of leaf and soil δ15N on the south slope were different from those on the north slope. The results suggested that the south slope has higher soil N transformation rates than the north slope and relationships between leaf and soil δ15N and environment are localized.
The south slope of Tian Shan differs from the north slope in environment. The study showed that...
