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    徐州市铜山区土壤硒含量分布、来源及其开发利用建议

    Geological distribution, provenance, and utilization strategies of soil selenium in Tongshan District, Xuzhou City, China

    • 摘要:
      研究目的 徐州市铜山区柳新镇、茅村镇因土壤硒含量较高而备受关注,为此深入查明了富硒地块的分布,探究了土壤硒的来源。
      研究方法 在研究区采集表层土壤3067件、土壤垂向剖面3个、大气干沉降样品4个、灌溉水及底泥样品8组、煤矸石样品4件、粉煤灰样品1件。
      研究结果 研究区表层土壤硒含量范围为0.08~15.80 mg/kg,均值为0.57 mg/kg,变异系数为1.14,呈现高度空间变异性。硒元素在土壤表层、大气干沉降、底泥中明显富集,是受到煤炭产业相关的人类活动影响,包括燃煤过程中硒的挥发和飞灰搬运、堆积粉煤灰和煤矸石中硒的淋滤和迁移、采矿洗选废水排放、采煤塌陷区复垦活动等。点状硒含量高值区往往由露天煤矸石堆积、燃煤大气排放造成,面状硒含量高值区的形成主要受到水流搬运的影响,如留武村—大庄村—茅村村—檀山村一带,高硒粉煤灰在径流的作用下沿河流沟渠输送硒元素,通过灌溉进入农田土壤并积累。富硒耕地资源综合评价结果显示,研究区共有富硒耕地面积8145.61 hm2,其中优质富硒耕地资源面积占全区耕地总面积的79.39%,预估区域表层土壤硒资源总量为13.34 t,具有较好的开发利用前景。
      结论 本研究为区域富硒土壤的应用开发提供了基础数据支撑,应进一步关注农产品硒含量和居民摄入量,通过优化布局、科技赋能、政策支持、品牌建设、融资拓展和资源管理等措施推动产业升级。

       

      Abstract:
      This paper is the result of agricultural geological survey engineering.
      Objective Liuxin Town and Maocun Town in Tongshan District, Xuzhou City, have drawn attention due to the elevated levels of soil selenium (Se). We elucidate the distribution of Se-enriched zones and identify the underlying sources.
      Methods A comprehensive sampling was conducted, including 3067 surface soil samples, 3 vertical soil profiles, 4 atmospheric dry deposition samples, 8 sets of irrigation water and sediment samples, 4 coal gangue samples, and 1 fly ash sample.
      Results The surface soil Se concentrations ranged from 0.08 to 15.80 mg/kg, with an average of 0.57 mg/kg and a coefficient of variation (CV) of 1.14, indicating strong spatial heterogeneity. Significant Se enrichment was observed in the soil surface layer, atmospheric dry deposition, and river sediments, primarily driven by coal-related anthropogenic activities. These included Se volatilization and fly ash dispersal during coal combustion, Se leaching and migration from accumulated fly ash and coal gangue, discharge of mining and washing wastewater, and land reclamation in coal mining subsidence areas, etc. Point-source Se hotspots were linked to open-pit coal gangue stockpiles and coal-fired atmospheric emissions, whereas non-point-source was mainly attributed to hydrological transport. For instance, in the areas of Liuwu-Dazhuang-Maocun-Tanshan village corridor, high-Se fly ash was transported via runoff through river networks, subsequently entering farmland soils via irrigation. A comprehensive evaluation of Se-enriched cultivated land resources revealed that there were 8145.61 hectares of Se-enriched area, of which premium Se-enriched land accounted for 79.39% of the total area, and the estimated total selenium resource in the topsoil was 13.34 tons, indicating significant potential for agricultural development and utilization.
      Conclusions The present study provided foundational data to support the exploitation and utilization of Se-enriched soils in the study area. Future efforts should focus on monitoring selenium levels in agricultural products and human dietary intake, while promoting selenium industrial upgrading through optimized land-use planning, technological innovation, policy incentives, brand establishment, financial support, and resource management.

       

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