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广西横州市岩溶与非岩溶区耕层土壤Zn通量特征

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以广西横州市岩溶区和非岩溶区为研究区,针对耕层土壤Zn的输送途径和年输送通量密度进行对比研究。结果表明,受成土母质影响,岩溶区表层土壤Zn含量明显高于非岩溶区,岩溶区和非岩溶区土壤Zn的输入量受人类活动影响较大,主要输入途径均为大气沉降,年输入通量密度均值分别为494。15和484。99g/(hm2·a);主要输出途径为农作物收割,年输出通量密度分别为490。63和580。12g/(hm2·a),受铁锰结核和灌溉水影响,非岩溶区年输出通量密度略高;研究区年净输入通量整体表现为Zn累积状态。
Characteristics of Zn flux in cultivated soil layer in karst and non-karst areas of Hengzhou,Guangxi
A comparative study was conducted to analyze the import and export pathways,as well as the annual input and output flux density of Zn in cultivated soil,in both karst and non-karst areas of Hengzhou,Guangxi.The results showed that the content of Zn in soil in karst area was significantly higher than that in non-karst area under the influence of the parent material.The input of soil Zn in both karst and non-karst areas was significantly affected by human activities,with atmospheric deposition being the primary input pathway.The average annual input flux densities were 494.15 and 484.99g/(hm2·a)in karst and non-karst areas,respectively.The main output pathway was through harvesting,with the annual output flux densities being 490.63 and 580.12g/(hm2·a)in karst and non-karst areas,respectively.The annual output flux density in non-karst area was slightly higher due to the influence of Fe-Mn nodulation and irrigation water.Overall,the annual input flux showed Zn accumulation.

soil zinc(Zn)annual input flux densitykarst areasGuangxi Hengzhou

杨烨宇、李程、杨忠芳、张起钻、王磊、邹胜章、韦华周、莫佳蓉

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中国地质科学院岩溶地质研究所,广西岩溶资源环境工程技术研究中心,联合国教科文组织国际岩溶研究中心,广西桂林 541004

广西平果喀斯特生态系统国家野外科学观测研究站,广西平果 531406

自然资源部南方石山地区矿山地质环境修复工程技术创新中心,广西南宁 530028

中国地质大学(北京)地球科学与资源学院,北京 100083

中国地质调查局天津地质调查中心,天津 300170

广西壮族自治区第四地质队,广西 南宁 530031

广西壮族自治区自然资源生态修复中心,广西 南宁 530028

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土壤锌(Zn) 年净输入通量密度 岩溶区 广西横州

2024

中国环境科学
中国环境科学学会

中国环境科学

CSTPCDCHSSCD北大核心
影响因子:2.174
ISSN:1000-6923
年,卷(期):2024.44(12)