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[土壤-作物系统中硒的分布特征及富硒土壤阈值]

[Distribution Characteristics of Selenium in a Soil-Crop System and the Threshold of Selenium-Rich Soils].

作者信息

Wang Rui, Deng Hai, Jia Zhong-Min, Yan Ming-Shu, Zhou Jiao, He Zhong-Xiang, Liang Shao-Biao, Dong Jin-Xiu, Su Li-Ming

机构信息

Southeast Sichuan Geological Group, Chongqing Bureau of Geology and Minerals Exploration, Chongqing 400038, China.

Chongqing Key Laboratory of Land Quality Geological Survey, Chongqing 400038, China.

出版信息

Huan Jing Ke Xue. 2020 Dec 8;41(12):5571-5578. doi: 10.13227/j.hjkx.202006113.

Abstract

In order to determine the distribution characteristics of Se in soil-crop systems, we carried out a study on the Se-rich soil threshold by collecting 8789 surface soils and 155 deep soils in the Qianjiang District of Chongqing City, China, and 141 corn seeds and 159 rice seeds (simultaneously collecting 141 and 159 corresponding root soil samples, respectively). We then analyzed the Se content, organic matter, S, Mn, TFeO, AlO, and KO in soils and crops, and soil pH. We also analyzed the surface layer using geostatistical methods and the distribution characteristics of Se in deep soils using multiple regression analysis to study the factors influencing the bioavailability of Se. Based on the contents of each component of root soil and the Se contents of crops, the Se rich threshold was examined. The results showed that the high-Se soils in the study area account for 32.72% of the total area; the distribution of Se contents in the surface and deep soils is mainly controlled by the parent material, the source of soil Se is stable, and the surface enrichment is obvious. The Se-rich rates of corn and rice were 75.35% and 46.81%, respectively, and soil organic matter and S content will limit the bioavailability of Se. If the planted crop is corn, it is recommended to use 0.3 mg·kg as the Se-rich soil threshold; if the planted crop is rice, when the soil pH is ≤ 7.5, it is recommended to use 0.3 mg·kg as the Se-rich soil threshold, while at a soil pH>7.5, it is recommended to use 0.4 mg·kg as the threshold. Similarly, if other large crops are planted in the study area, this method can also be used to carry out a study on the proposed Se-rich soil threshold.

摘要

为了确定土壤 - 作物系统中硒的分布特征,我们通过在中国重庆市黔江区采集8789份表层土壤和155份深层土壤以及141份玉米种子和159份水稻种子(同时分别采集141份和159份相应的根际土壤样品),开展了富硒土壤阈值研究。然后我们分析了土壤和作物中硒含量、有机质、硫、锰、全铁氧化物、氧化铝和氧化钾以及土壤pH值。我们还用地统计学方法分析表层,并用多元回归分析研究深层土壤中硒的分布特征,以探讨影响硒生物有效性的因素。基于根际土壤各组分含量和作物硒含量,考察了富硒阈值。结果表明,研究区高硒土壤占总面积的32.72%;表层和深层土壤中硒含量分布主要受成土母质控制,土壤硒源稳定,表层富集明显。玉米和水稻的富硒率分别为75.35%和46.81%,土壤有机质和硫含量会限制硒的生物有效性。若种植作物为玉米,建议以0.3 mg·kg作为富硒土壤阈值;若种植作物为水稻,当土壤pH值≤7.5时,建议以0.3 mg·kg作为富硒土壤阈值,而当土壤pH值>7.5时,建议以0.4 mg·kg作为阈值。同样,若在研究区种植其他大宗作物,也可采用此方法开展富硒土壤阈值研究。

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