Soil N retention and nitrate leaching in three types of dunes in the Mu Us desert of China

被引:34
|
作者
Jin, Zhao [1 ]
Zhu, Yajuan [2 ]
Li, Xiangru [1 ]
Dong, Yunshe [3 ]
An, Zhisheng [1 ]
机构
[1] Chinese Acad Sci, Inst Earth Environm, State Key Lab Loess & Quaternary Geol, Xian 710061, Peoples R China
[2] Chinese Acad Forestry, Inst Desertificat Studies, Beijing 100091, Peoples R China
[3] Chinese Acad Sci, Inst Geog Sci & Nat Resources Res, Beijing 100101, Peoples R China
来源
SCIENTIFIC REPORTS | 2015年 / 5卷
基金
中国国家自然科学基金;
关键词
GLOBAL PATTERNS; INNER-MONGOLIA; ORDOS PLATEAU; MOJAVE DESERT; NITROGEN; ECOSYSTEM; WATER; DEPOSITION; IMPRINT; ARIDITY;
D O I
10.1038/srep14222
中图分类号
O [数理科学和化学]; P [天文学、地球科学]; Q [生物科学]; N [自然科学总论];
学科分类号
07 ; 0710 ; 09 ;
摘要
A large reservoir of soil nitrate in desert subsoil zones has been demonstrated in previous studies; however, information on the subsoil nitrate reservoir and its distribution characteristics in the deserts of China is still limited. This study investigated the distribution patterns of soil total nitrogen (N), nitrate, ammonium, and stable isotopic ratios of N-15 (delta N-15) in shallow (1 m) and subsoil (5 m) profiles in three types of dunes in the Mu Us desert of China. We found that soil N retention of the fixed and semi-fixed dunes followed a progressive nutrient depletion pattern in shallow soil profiles, whereas the subsoil nitrate of the fixed, semi-fixed and mobile dunes maintained a conservative accumulation pattern. The results indicate that the subsoil of the Mu Us desert may act as a reservoir of available nitrate. Furthermore, a soil delta N-15 analysis indicate that the nitrate content of the fixed dune is likely derived from soil nitrification, whereas the nitrate content in the mobile dune is derived from atmospheric nitrate deposition. Within the context of looming climate change and intensifying human activities, the subsoil nitrate content in the deserts of northern China could become mobilized and increase environmental risks to groundwater.
引用
收藏
页数:8
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