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

机译:中国毛乌素沙漠三种沙丘的土壤固氮和硝态氮淋失

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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 15N (δ15N) 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 δ15N 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.
机译:在先前的研究中已经证明了在沙漠地下土壤区域中有大量的土壤硝酸盐。然而,关于中国地下土壤硝酸盐储层及其分布特征的信息仍然有限。这项研究调查了土壤总氮(N),硝酸盐,铵和 15 N(δ 15 N)的稳定同位素比的分布模式(1 m)中国毛乌素沙漠三种沙丘的土壤和底土(5μm)剖面。我们发现,固定和半固定沙丘的土壤氮保留量在浅层土壤剖面中遵循逐步的养分消耗模式,而固定,半固定和移动沙丘的底土硝酸盐保持着保守的积累模式。结果表明,毛乌素沙漠的底土可作为有效硝酸盐的储集层。此外,土壤δ 15 N分析表明,固定沙丘的硝酸盐含量可能来自土壤硝化作用,而流动沙丘中的硝酸盐含量来自大气中的硝酸盐沉积。在迫在眉睫的气候变化和人类活动加剧的背景下,中国北方沙漠中的地下土壤硝酸盐含量可能会动员起来,并增加对地下水的环境风险。

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