中国地质学会岩矿测试技术专业委员会、国家地质实验测试中心主办

江西赣县清溪地区土壤硒地球化学特征和水稻根系土硒生物有效性影响因素

刘冰权, 沙珉, 谢长瑜, 周强强, 魏星星, 周梵. 江西赣县清溪地区土壤硒地球化学特征和水稻根系土硒生物有效性影响因素[J]. 岩矿测试, 2021, 40(5): 740-750. doi: 10.15898/j.cnki.11-2131/td.202107230082
引用本文: 刘冰权, 沙珉, 谢长瑜, 周强强, 魏星星, 周梵. 江西赣县清溪地区土壤硒地球化学特征和水稻根系土硒生物有效性影响因素[J]. 岩矿测试, 2021, 40(5): 740-750. doi: 10.15898/j.cnki.11-2131/td.202107230082
LIU Bing-quan, SHA Min, XIE Chang-yu, ZHOU Qiang-qiang, WEI Xing-xing, ZHOU Fan. Geochemical Characteristics of Soil Selenium and Influencing Factors of Selenium Bioavailability in Rice Root Soils in Qingxi Area, Ganxian County, Jiangxi Province[J]. Rock and Mineral Analysis, 2021, 40(5): 740-750. doi: 10.15898/j.cnki.11-2131/td.202107230082
Citation: LIU Bing-quan, SHA Min, XIE Chang-yu, ZHOU Qiang-qiang, WEI Xing-xing, ZHOU Fan. Geochemical Characteristics of Soil Selenium and Influencing Factors of Selenium Bioavailability in Rice Root Soils in Qingxi Area, Ganxian County, Jiangxi Province[J]. Rock and Mineral Analysis, 2021, 40(5): 740-750. doi: 10.15898/j.cnki.11-2131/td.202107230082

江西赣县清溪地区土壤硒地球化学特征和水稻根系土硒生物有效性影响因素

  • 基金项目:
    中国地质调查局地质调查项目"海峡西岸经济区土地质量地球化学调查"(DD20160321);中国地质调查局地质调查项目"江西赣州地区土地资源地质环境调查"(J[2014]02-021-024)
详细信息
    作者简介: 刘冰权, 硕士, 高级工程师, 从事生态地球化学及环境地球化学研究。E-mail: 251497867@qq.com
  • 中图分类号: S151.93;O613.52;O657.63;O657.31

Geochemical Characteristics of Soil Selenium and Influencing Factors of Selenium Bioavailability in Rice Root Soils in Qingxi Area, Ganxian County, Jiangxi Province

  • 江西赣南地区是典型的硒缺乏地理分布区,但近年来研究成果表明该地区稻谷富硒率高,土壤与稻谷富硒存在不一致的原因尚不明确,探讨土壤和稻谷硒含量特征和土壤硒的生物有效性,对赣南地区富硒土地资源利用和富硒农产品开发具有重要意义。本文以赣县清溪地区为研究对象,采用电感耦合等离子体质谱/发射光谱(ICP-MS/OES)等方法测定了研究区1734件表层土壤、57组稻谷及配套根系土硒等元素含量及硒形态地球化学指标;系统分析了区内土壤硒含量和分布特征、稻谷硒含量特征,探讨了根系土硒生物有效性的影响因素。结果表明:研究区表层土壤以足硒、富硒区为主,土壤硒含量与成土母岩关系密切,不同成土母岩区土壤硒含量规律为:古生代变质岩>中生代花岗岩>新元古代变质岩>中生代陆源碎屑岩>新生代第四系。根系土硒含量均未达到富硒土壤标准,稻谷富硒率为64.91%,稻谷对土壤硒的富集能力强(富集系数20.05%),当根系土硒含量≥0.25mg/kg时,水稻富硒率高达70.83%,能够稳定产出优质富硒水稻。硒的赋存形态是影响土壤硒生物有效性的主要因素,土壤总硒含量较低时,水溶态、离子可交换态、碳酸盐结合态硒的占比高,从而提升了硒的生物有效性;有机质含量低,对硒吸附能力弱,也是硒生物有效性高的重要原因。本研究认为,赣县清溪地区富硒、足硒土壤开发利用时,综合考虑土壤硒含量、土壤理化指标、硒形态对土壤硒生物有效性的影响,有利于科学指导天然富硒土地划定和富硒水稻产业开发。

  • 加载中
  • 图 1  研究区地质和水稻采样点位置示意图

    Figure 1. 

    图 2  研究区根系土总硒与水溶态硒、活动态硒、稳定态硒、残渣态硒的散点图

    Figure 2. 

    表 1  研究区不同成土母质区土壤硒含量对比

    Table 1.  Comparison of Se contents in soils derived from different parent rocks in the study area

    成土母质 土壤硒含量范围
    (mg/kg)
    硒平均值
    (mg/kg)
    样品数
    (件)
    新生代第四系 0.07~0.90 0.26 346
    中生代陆源碎屑岩 0.08~0.84 0.28 262
    中生代花岗岩 0.09~1.58 0.35 930
    古生代变质岩 0.13~1.17 0.37 164
    新元古代变质岩 0.14~0.71 0.32 26
    下载: 导出CSV

    表 2  研究区稻谷与根系土硒含量特征及稻谷富集系数

    Table 2.  Characteristics of Se contents in rice and root soil and enrichment coefficient of rice in the study area

    硒含量 最大值 最小值 平均值 标准差 变异系数 重庆黔江区
    (王锐等, 2020[29])
    广西浔郁平原
    (陈锦平等, 2018[30])
    赣州青塘—梅窖地区
    (周墨等, 2018[25])
    根系土硒含量(mg/kg) 0.36 0.14 0.24 0.05 0.23 0.43 0.546 0.34
    稻米硒含量(mg/kg) 0.10 0.02 0.04 0.02 0.35 0.05 0.059 0.06
    硒生物富集系数(%) 63.42 8.58 20.05 9.73 0.49 13.00 10.80 16.00
    下载: 导出CSV

    表 3  研究区根系土硒含量分级及其对应稻谷的富硒率与重金属超标率

    Table 3.  Classification of Se contents in root soil, corresponding Se-enrichment rate and heavy metal excess rate of rice in the study area

    根系土硒含量水平
    (mg/kg)
    富硒水稻样本
    (件)
    超标水稻样本
    (件)
    水稻样本
    (件)
    富硒率
    (%)
    超标率
    (%)
    Se含量≥0.15 36 4 55 65.45 7.27
    Se含量≥0.20 30 3 45 66.67 6.66
    Se含量≥0.25 17 0 24 70.83 0
    下载: 导出CSV

    表 4  研究区根系土总硒与各形态硒含量、形态比例的相关系数(n=14)

    Table 4.  Correlation coefficients of total Se in root soil vs. its species content and proportion in the study area

    硒形态 各形态硒含量与土壤总硒的相关系数 硒形态 各形态硒比例与土壤总硒的相关系数
    水溶态 0.85** 水溶态 -0.54*
    离子可交换态 0.13 离子可交换态 -0.66**
    碳酸盐结合态 0.06 碳酸盐结合态 -0.74**
    腐植酸结合态 0.74** 腐植酸结合态 -0.09
    铁锰氧化态 0.70** 铁锰氧化态 -0.64**
    强有机结合态 0.84** 强有机结合态 -0.20
    残渣态 0.93** 残渣态 0.40
    活动态 0.52* 活动态 -0.75**
    稳定态 0.99** 稳定态 0.75**
    注:“**”代表在0.01水平下显著相关;“*”代表在0.05水平下显著相关。
    下载: 导出CSV
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出版历程
收稿日期:  2021-06-22
修回日期:  2021-07-31
录用日期:  2021-08-26
刊出日期:  2021-09-28

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