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[中国洋河小流域不同土地利用类型土壤中硒的空间分布及其影响因素]

[Spatial distribution of Se in soils from different land use types and its influencing factors within the Yanghe Watershed, China].

作者信息

Shang Jing-min, Luo Wei, Wu Guang-hong, Xu Lan, Gao Jia-jia, Kong Pei-ru, Bi Xiang, Cheng Zhi-gang

出版信息

Huan Jing Ke Xue. 2015 Jan;36(1):301-8.

Abstract

Based on different land use types, altitudes, soil and vegetation types etc, 171 representative topsoils (0-10 cm) were collected within the Yanghe watershed, China for determining the total concentrations, spatial distribution and influencing factors of selenium (Se). The results showed that the total selenium concentrations in soils within the watershed ranged from 0.02 to 3.24 mg x kg(-1) dry weight (dw). The geometric mean of Se in soils within the watershed was 0.30 mg x kg(-1), which was higher than those in Beijing plain (0.20 mg x kg(-1)), Hebei plain (0.19 mg x kg(-1)) and China (0.29 mg x kg(-1)). Soils which lacked Se (0.13-0.18 mg x kg(-1)) were mainly distributed in Huaian, Xuanhua, and Huailai counties. Se concentrations in most areas within the watershed were sufficient (0.18-0.45 mg x kg(-1)). In addition, Wanquan, Xinghe, Tianzhen and Yanggao counties also had some selenium-rich areas. Concentrations of Se were different under different land use types. They were of the following order: forest land > industrial and mining land > grassland > agricultural land. Agricultural land had the lowest concentrations of Se, with a mean concentration of 0.28 mg x kg(-1). We also found that parent materials and soil types had no significant effects on soil Se concentrations within the Yanghe Watershed. The results indicated that Se concentrations were positively and significantly correlated with clay contents and altitudes, but negatively and significantly with pH values. Furthermore, TOC, Fe and Al concentrations were also important factors influencing the Se concentrations in soils within the Yanghe Watershed.

摘要

基于不同的土地利用类型、海拔高度、土壤和植被类型等,在中国洋河集水区采集了171份代表性表层土壤(0 - 10厘米),以测定硒(Se)的总浓度、空间分布及影响因素。结果表明,该集水区土壤中硒的总浓度范围为0.02至3.24毫克/千克干重。该集水区土壤中硒的几何平均值为0.30毫克/千克,高于北京平原(0.20毫克/千克)、河北平原(0.19毫克/千克)和中国(0.29毫克/千克)。缺硒土壤(0.13 - 0.18毫克/千克)主要分布在怀安县、宣化区和怀来县。集水区内大部分地区的硒浓度充足(0.18 - 0.45毫克/千克)。此外,万全县、兴和县、天镇县和阳高县也有一些富硒地区。不同土地利用类型下的硒浓度不同,顺序如下:林地>工矿用地>草地>农用地。农用地的硒浓度最低,平均浓度为0.28毫克/千克。我们还发现,母质和土壤类型对洋河集水区内土壤硒浓度没有显著影响。结果表明,硒浓度与粘粒含量和海拔高度呈显著正相关,但与pH值呈显著负相关。此外,总有机碳、铁和铝的浓度也是影响洋河集水区土壤硒浓度的重要因素。

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