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中国农学通报 ›› 2017, Vol. 33 ›› Issue (36): 111-118.doi: 10.11924/j.issn.1000-6850.casb17020044

• 资源 环境 生态 土壤 气象 • 上一篇    下一篇

黄土丘陵区煤矿开采对土壤理化性质的影响

王炎强,毕如田,张吴平,荆耀栋,温媛媛   

  1. 山西农业大学 资源环境学院山西 太谷,山西农业大学 资源环境学院山西 太谷,山西农业大学 资源环境学院山西 太谷,山西农业大学 资源环境学院山西 太谷,山西农业大学 资源环境学院山西 太谷
  • 收稿日期:2017-02-14 修回日期:2017-03-24 接受日期:2017-04-06 出版日期:2017-12-29 发布日期:2017-12-29
  • 通讯作者: 毕如田
  • 基金资助:
    国土资源部公益性行业项目“北方村庄压煤山丘区土地综合整治技术研究”(201411007)。

Impact of mining on soil physicochemical properties in Loess Plateau——A case study on Changhe River basin in Jincheng city

  • Received:2017-02-14 Revised:2017-03-24 Accepted:2017-04-06 Online:2017-12-29 Published:2017-12-29

摘要: 【目的】为揭示黄土丘陵区煤矿开采对土壤理化性质的影响,并为扰动区的恢复治理工作提供一定的理论依据。【方法】运用地统计学理论和方法,测定并计算长河流域内0-20cm /20-40cm/ 40-60cm深度土壤的容重、孔隙度、机械组成、有机质等指标,对煤矿开采对土壤理化性质扰动的统计变化规律、空间结构、空间分布及其成因进行了分析。【结果】研究结果表明:扰动区与未扰动区对比,(1)从平均值变化结果来看,土壤容重、砂粒、有机质含量增大,孔隙度、粉粒、粘粒含量减小,其中容重在0-20cm和砂粒在0-60cm处显著增大(p<0.05),孔隙度在0-20cm、有机质在0-40cm和粉粒在0-60cm处显著减小(p<0.05),其它各层没有显著变化。(2)煤矿开采导致孔隙度、容重和有机质的空间依赖度减弱,其中有机质由强空间依赖变为中等空间依赖,煤矿开采使砂粒、粉粒和粘粒的空间依赖性得到增强,其中砂粒由中等空间依赖变为强空间依赖。(3)研究区土壤理化性质在三个土层空间分布上都具有一定的相似性,长河两侧土壤理化性质含量高低分布较为明显。煤炭开采对土壤的破坏分为显性破坏和隐性破坏,并且两者之间存在一定的因果关系,地表产生的沉陷和裂缝会致使土壤板结,改变地表形态,促进土壤空气与大气空气交换,从而使扰动区内土壤理化性质发生变化。【结论】研究发现扰动区和未扰动区的土壤理化性质有明显差异,为小流域采煤扰动后土壤理化性质变化及其成因提供一定的系统诊断依据。

关键词: 茶树扦插, 茶树扦插, 苗圃地, 夏季覆地膜, 消毒

Abstract: Based on the method of Geo-statistics, this study analyses the change regulation, special structure, distribution and cause of impact of mining on soil physicochemical properties through determining and calculating the indexes of soil bulk density, porosity, mechanical composition and organic matter in order to provide theoretical basis to restoration management of disturbed zone. By contrasting the disturbed zone and undisturbed zone, the results show that:①The average change shows that the soil bulk density, gravel and organic matter increase, among which bulk density increases significantly at 0-20cm and gravel increases at 0-60cm(p<0.05); while the porosity, silt and clay reduces, among which porosity decreases significantly at 0-20cm, organic matter decreases at 0-40cm and silt reduces at 0-60cm(p<0.05) and other layers have no significant change.② The spatial dependency degree of porosity, bulk density and organic matter decrease due to mining, among which organic matter varies from strong dependency to moderate dependency; while the spatial dependency degree of sand, silt and clay increase due to mining, among which sand varies from moderate dependency to strong dependency.③The distribution of soil physicochemical properties has a certain similarity in three soil layers, among which the two sides of Changhe is obvious. The damage of soil by mining can be divided into dominant and implicit damage and there is a causal relationship between the two. The subsidence and cracks in surface may cause soil compaction and deformation,which promote the exchange between soil air and atmosphere and thus change the physicochemi- cal properties of soil.The results showed that the physical and chemical properties of soil in the disturbed and undisturbed areas were significantly different, which could provide a systematic diagnostic basis for the changes of soil physical and chemical properties and their causes.