CAJ | 학술논문

为了研究土壤常量元素来源及分布特征，分析了华东多目标地球化学调查区表层土壤和深层土壤常量元素质量分数的关系，以及不同成土母质发育的土壤常量元素质量分数之间的相互关系。结果显示：在该地区表层土壤和深层土壤中，常量元素存在显著相关性，质量分数比值为0．75～1．04，说明该区域表层土壤常量元素与深层土壤属于同一物质来源，主要来源于成土母质；常量元素在不同地质单元区土壤质量分数的高低及变异系数的大小除了成土母质原因，元素自身地球化学性质也是其主要影响因素；元素之间相关性及因子分析很好地区分出了在该地区成土过程中元素共生组合特征，即 CaO MgO Na2 O、Al2 O3 TFe2 O3 K2 O、SiO23个组合。通过分析可以得出在该地区表层土壤常量元素对成土母质有良好继承性，因此能够利用表层土壤元素组合特征和质量分数高低在一定程度上辨别该地区土壤的成土母质岩性、来源和土壤机械组成。
위료연구토양상량원소래원급분포특정，분석료화동다목표지구화학조사구표층토양화심층토양상량원소질량분수적관계，이급불동성토모질발육적토양상량원소질량분수지간적상호관계。결과현시：재해지구표층토양화심층토양중，상량원소존재현저상관성，질량분수비치위0．75～1．04，설명해구역표층토양상량원소여심층토양속우동일물질래원，주요래원우성토모질；상량원소재불동지질단원구토양질량분수적고저급변이계수적대소제료성토모질원인，원소자신지구화학성질야시기주요영향인소；원소지간상관성급인자분석흔호지구분출료재해지구성토과정중원소공생조합특정，즉 CaO MgO Na2 O、Al2 O3 TFe2 O3 K2 O、SiO23개조합。통과분석가이득출재해지구표층토양상량원소대성토모질유량호계승성，인차능구이용표층토양원소조합특정화질량분수고저재일정정도상변별해지구토양적성토모질암성、래원화토양궤계조성。
In order to explore the sources and distribution of macro-elements in soils,relationships between surface soils and deep soils,relationships between ratios and elements among different parent materials were studied in multi-purpose geochemical survey area of East China.The results showed that the macro-elements in surface soils and deep soils were significantly correlated,and ratios in mass ranged from 0.75 to 1.04 in the study area,The analysis results presented that macro-elements in surface soils mainly originated from parent material, and the distribution of geochemical elements is primarily influenced by both parent material and the geochemical characteristics of macro-element.Correlation analysis and factor analysis were applied to distinguish the paragenesis and assemblage rules in soil-forming process,which were CaO MgO Na2 O,Al2 O3 TFe2 O3 K2 O and SiO2 .The anlysis showed macro-elements had good Inheritance from parent materials,and elements paragenesis and assemblage rules and ratios in soils can be used to distinguish the lithology,sources and soil particle composition.