首页|岷江上游干旱河谷区汶川段风化壳剖面元素地球化学特征

岷江上游干旱河谷区汶川段风化壳剖面元素地球化学特征

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选择岷江上游干旱河谷区汶川段不同基岩类型的岩石—土壤垂向剖面,开展地球化学测试分析工作,据此研究不同类型风化壳剖面元素垂向分布特征,探究基岩对土壤化学元素含量的影响,并从地质角度出发为该区域农业生产种植和生态环境修复提供建议.风化壳剖面自上而下可划分为腐殖层(A)、淀积层(B)、母质层(C)和基岩层(R),腐殖层中Al、Ca、K、Mg、Fe、Se、Zn、Cu、Cd、Pb均值高于其在全国土壤中的平均值,Si、Na、Mn、Cr、As、Cd、Hg均值低于全国土壤中的平均值.不同基岩风化壳剖面中,除去在基岩中含量较高的元素在所对应的土壤层中含量较高外,相同元素在其余土壤层中含量大致相同.风化剖面由基岩层至腐殖层,化学风化强度逐渐增强,土壤的风化程度普遍高于基岩风化程度.元素含量除继承母岩特征外,还发生了分异,Al、K、Se在腐殖层富集,Na、Fe、Si、Pb、Cu、Zn、Mn、As、Cd、Cr、Hg在淀积层富集,Mg、Ca在母质层富集.
Element geochemical characteristics of weathering crust profiles of the Wenchuan section in the upper arid valley of the Minjiang River
This study conducted geochemical tests and analyses for vertical rock-soil profiles with different bedrock types in the Wen-chuan section in the upper arid valley of the Minjiang River.Based on the above,this study explored the vertical distributions of ele-ments in these weathering crust profiles to investigate the influence of bedrocks on the contents of chemical elements in soils.From a geological perspective,this study provided proposals for planting in agricultural production and eco-environmental restoration for the study area.The results of this study are as follows:(1)From top to bottom,weathering crust profiles can be divided into four layers:the humus layer(A),the illuvial layer(B),the soil parent material layer(C),and the bedrock layer(R).The humus layers exhib-it higher average values of Al,Ca,K,Mg,Fe,Se,Zn,Cu,Cd,and Pb and lower average values of Si,Na,Mn,Cr,As,Cd,and Hg,compared to corresponding national average values in soils;(2)In weathering crust profiles with different bedrock types,except for elements with higher contents in both bedrocks and corresponding soil layers,the same elements manifest similar contents in other soil layers;(3)The chemical weathering intensity increased from the bedrock to the humus layers,with soil weathering degrees gener-ally higher than bedrock weathering degrees;(4)In addition to characteristics inherited from soil parent materials,elements in weathe-ring crust profiles show content differentiation,characterized by enriched Al,K,and Se in humus layers,enriched Na,Fe,Si,Pb,Cu,Zn,Mn,As,Cd,Cr,and Hg in illuvial layers,and enriched Mg and Ca in soil parent material layers.

arid valleyrock-soilelemental characteristicplanting proposal

周雪妮、曹亚廷、计扬

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中国地质调查局 军民融合地质调查中心,四川 成都 610036

成都理工大学 地质灾害防治与地质环境保护国家重点实验室,四川 成都 610059

干旱河谷 岩石—土壤 元素特征 种植建议

中国地调局军民融合地质调查中心项目

DD20220955

2024

物探与化探
中国国土资源航空物探遥感中心

物探与化探

CSTPCD
影响因子:0.828
ISSN:1000-8918
年,卷(期):2024.48(3)
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