[an error occurred while processing this directive] 世界地质 2020, 39(2) 471-478 DOI:   10.3969/j.issn.1004-5589.2020.02.023  ISSN: 1004-5589 CN: 22-1111/P

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本文关键词相关文章
松嫩平原
XRD
苏打盐渍土
黏粒矿物
本文作者相关文章
冯君
郑庆福
隋振民
王宇
赵兰坡
PubMed
Article by Feng J
Article by Zheng Q
Article by Sui Z
Article by Wang Y
Article by Zhao L
松嫩平原苏打盐渍土表层土壤黏粒矿物的组成分析
冯君1, 郑庆福2, 隋振民1, 王宇1, 赵兰坡1
1. 吉林农业大学资源与环境学院, 长春 130118;
2. 内蒙古民族大学仪器设备与实验室管理中心, 内蒙古通辽 028000
摘要: 以松嫩平原内的前郭和大安两地苏打盐渍土表层土壤为供试土壤,采用Rigaku RIX 2000型荧光光谱仪和XRD-7000衍射仪,对土壤黏粒矿物组成进行了分析。结果表明:表层土壤黏粒(<2 μm)化学组成均以SiO2、Al2O3和Fe2O3为主,其SiO2/Al2O3>4,土壤风化脱硅作用较弱;土壤黏粒以2:1型层状铝硅酸盐矿物为主,含有蒙脱石、伊利石-蒙脱石混层矿物、伊利石、伊利石-白云母混层矿物、蛭石、1:1型层状铝硅酸盐高岭石以及少量2:1:1型绿泥石和石英及1.42 nm间层矿物。苏打盐渍土处于风化脱K作用阶段,土壤中混层及间层矿物较多,以蛭石-绿泥石、蒙脱石-绿泥石过渡矿物为主,为二八面体白云母和二八面体蒙脱石混层矿物。水田利用可使土壤黏粒中绿泥石增加,改善苏打盐渍土不良的结构。
关键词 松嫩平原   XRD   苏打盐渍土   黏粒矿物  
Composition analysis of clay minerals from soda saline surface soil in Songhuajiang-Nenjiang plain
FENG Jun1, ZHENG Qing-fu2, SUI Zhen-min1, WANG Yu1, ZHAO Lan-po1
1. College of Resources and Environment Science, Jilin Agricultural University, Changchun 130118, China;
2. Equipment and Laboratory Management Center, Inner Mongolia University for the Nationalities, Tongliao 028000, Inner Mongolia, China
Abstract: Taking the soda saline surface soil of Qianguo and Da'an of the Songhuajiang-Nenjiang plain as sample soil,the compositions of the clay mineral of soil were analyzed by using XRF and XRD test methods.The results show that the chemical compositions of clay smaller than 2 μm are SiO2,Al2O3 and Fe2O3,and the ratio of SiO2/Al2O3 is greater than 4,revealing that weathering desilication is weak. The surface soda saline soil clay mineral compositions are mainly 2:1 type of layered aluminosilicate minerals consisting of montmorillonite,mixed layer of illite and montmorillonite,illite,mixed layer of illite and muscovite,vermiculite, some 1:1 type layered aluminosilicate kaolinite,and minor 2:1:1 type chlorite,quartz and 1.42 nm interlayer minerals.Soda saline soil is in the stage of weathering and potassium removing. There are many mixed layer and interlayer minerals in the soil,mainly transition minerals e. g., vermiculite-chlorite and montmorillonite-chlorite,and the mixed layer minerals of octahedral muscovite and octahedral montmorillonite. Paddy field utilization can increase chlorite in soil clay and improve the structure of soda saline soil.
Keywords: Songhuajiang-Nenjiang plain   X-ray diffraction   soda saline soil   clay mineral  
收稿日期 2019-10-24 修回日期 2019-12-28 网络版发布日期  
DOI: 10.3969/j.issn.1004-5589.2020.02.023
基金项目:

国家重点研发项目(2016YFC0501201)与吉林省科技发展项目(990532)联合资助。

通讯作者: 赵兰坡(1955-),教授,主要从事黑土培肥及盐渍土改良方面的研究。E-mail:zhaolanpo12@163.com
作者简介:
作者Email: zhaolanpo12@163.com

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