Geochemical characteristics and geological genesis of soil selenium anomaly zone in the Hetao Plain, Inner Mongolia, and crop biological effects-based assessment of selenium-rich cultivated land development potential

IF 5.1 3区 地球科学 Q1 GEOSCIENCES, MULTIDISCIPLINARY
China Geology Pub Date : 2026-04-01 Epub Date: 2026-05-22 DOI:10.31035/cg2024037
Yong-chun Li , Guo-dong Chen , Yu-chun-zi Du , Jiu-fen Liu , Xue-zhen Li , Hong-bing Hou
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Abstract

Exploring the geological genesis of selenium (Se) in Se-rich soil of the Hetao Plain, a major grain production base of corn, wheat, potato, sunflower and zucchini in northern China, is vital for the rational development of Se-rich land resources and the environmental geochemical assessment. In this study, element geochemical characterization, geospatial analysis and mathematical statistics were employed to investigate the factors influencing the spatial distribution of soil Se in the Hetao Plain, focusing on the differences in soil chemical weathering intensity, rare earth elements distribution pattern and soil sedimentary sequence characteristics between the study area and typical surrounding parent materials. The results indicated that the soil Se content in the study area ranged from 0.07 mg/kg to 0.72 mg/kg, with an average value of 0.24 mg/kg, which was higher than the regional background values. Moreover, this suggested that local Se enrichment occurred in the soil of study area, and that the Se distribution was restricted by factors including soil clay minerals, constant elements and soil organic matter (SOM) contents. The characteristics of soil parent material in the study area differed significantly from those of the piedmont diluvial parent material, whereas were similar to those of the Yellow River floodplain and lacustrine parent materials, revealing that the soil parent material in the study area mainly came from the water system transportation. Through combining the characteristics of soil sedimentary sequences in the study area with the location of the Yellow River ancient channel, it is suggested that the origin of high Se soil in the central and northern belt zone of the study area is associated with the Yellow River ancient channel, where the enrichment pattern is “channel sedimentary type”. In addition, the development and utilization potential of Se-rich cultivated land was explored based on the biological effects of Se. It was concluded that the Se content of crops (corn, sunflower and zucchini) in the study area was higher than that of similar crops in China, that crop species and soil Se content were the dominant influencing factors of crop Se content in the study area, and that the crops growing in Se-rich areas had higher Se enrichment rate than those growing in non-Se-rich areas. This exhibited a high development and utilization potential of the investigated cultivated land for Se-rich crop production.
内蒙古河套平原土壤硒异常带地球化学特征、地质成因及基于作物生物效应的富硒耕地开发潜力评价
河套平原是中国北方玉米、小麦、马铃薯、向日葵和西葫芦的主要粮食生产基地,研究该地区富硒土壤中硒的地质成因,对合理开发富硒土地资源和进行环境地球化学评价具有重要意义。本文采用元素地球化学表征、地理空间分析和数理统计等方法,研究了河套平原土壤硒元素空间分布的影响因素,重点研究了研究区土壤化学风化强度、稀土元素分布格局和土壤沉积序列特征与周围典型母质的差异。结果表明:研究区土壤硒含量范围为0.07 ~ 0.72 mg/kg,平均值为0.24 mg/kg,高于区域背景值;研究区土壤存在局地富集硒的现象,硒的分布受土壤黏土矿物、常量元素和土壤有机质含量等因素的制约。研究区土壤母质特征与山前洪积土母质特征有显著差异,而与黄河河漫滩和湖泊母质特征相似,表明研究区土壤母质主要来自水系搬运。结合研究区土壤沉积序列特征与黄河古河道位置,认为研究区中北部带高硒土的成因与黄河古河道有关,富集模式为“河道沉积型”。此外,基于硒的生物效应,探讨了富硒耕地的开发利用潜力。结果表明,研究区作物(玉米、向日葵和西葫芦)硒含量高于全国同类作物,作物种类和土壤硒含量是影响研究区作物硒含量的主要因素,富硒区作物硒富集率高于非富硒区作物。研究区具有较高的富硒作物开发利用潜力。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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来源期刊
China Geology
China Geology GEOLOGY-
CiteScore
7.80
自引率
11.10%
发文量
275
审稿时长
16 weeks
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