煤炭工程 ›› 2018, Vol. 50 ›› Issue (11): 141-146.doi: 10.11799/ce201811034

• 研究探讨 • 上一篇    下一篇

煤矸石充填复垦修复区土壤有机碳空间分布研究

吴思聪,陈孝杨,邢雅珍,宋称心,吴光龙,孟凡星   

  1. 安徽理工大学
  • 收稿日期:2018-05-23 修回日期:2018-08-02 出版日期:2018-11-20 发布日期:2018-12-25
  • 通讯作者: 吴思聪 E-mail:576745020@qq.com

Spatial Distribution of Soil Organic Carbon in Reclaimed Soil Filled with Coal Gangue- A Case Study of Xinzhuangzi Coal Mine in Huainan City, Anhui

  • Received:2018-05-23 Revised:2018-08-02 Online:2018-11-20 Published:2018-12-25

摘要: 土壤有机碳(SOC)作为表征土壤质量与生态特性的关键指标,其恢复与分布状况的研究对评估重构土壤质量变化、指导重构土壤改良具有重要意义。本文以淮南市新庄孜矿煤矸石充填复垦修复区SOC为研究对象,按照不同覆土厚度与植被类型将研究区分为10种采样区,分层采集重构土壤剖面不同深度土壤样品(0~20、20~40cm),测定其容重(BD)、含水量(WC)、pH,以及有机碳(SOC),以研究不同覆土厚度、不同植被类型对SOC空间分布特征的影响,及其与土壤理化性质的相关性。结果表明:不同植被类型下的SOC含量整体上差异显著,表层土壤(0~20cm)的SOC含量由大到小依次为草地>板栗林地>黄豆地>玉米地>水杉林地|20~40cm土层中SOC含量,草地>板栗林地>玉米地>水杉林地>黄豆地;不同覆土厚度下SOC含量在20~40cm土层中差异极显著,并随上覆土层厚度的增加而增大,最高值为覆土81 ~ 100cm的采样区(4.06 ~ 5.87g/kg),随着采样深度的增加,SOC含量逐渐减少,且随上覆土层厚度的加深,整体上的降低速率加快|上覆植被类型对研究区SOC含量的影响大于覆土厚度对其的影响|在研究区现有植被类型和覆土厚度的交互作用下对SOC的含量没有显著性的差异|SOC与pH值呈显著正相关关系,与BD呈极显著地负相关系,与WC呈正相关关系(P>0.05)。

关键词: 土壤有机碳, 复垦土壤, 空间分布, 植被类型, 覆土厚度

Abstract: Abstract :Soil organic carbon (SOC) is a key indicator for characterization of soil quality and ecological characteristics. The study of restoration and distribution of SOC is of great significance for assessing the changes of soil quality and guiding the reconstruction of soil. The selection of gangue-filled reclamation and restoration area in Xinzhuangzi Mine, Huainan City as the research object. the study was divided into 10 sampling plots according to different topsoil cover thickness and vegetation type. The soil samples at 0-20 cm and 20-40 cm soil from different depths of reclaimed soil profile were collected to determine their bulk density(BD), water content (WC),pH value ,and soil organic carbon (SOC). Thus, the authors studied the effect of topsoil thickness and vegetation type on SOCsoil organic carbon (SOC) spatial distribution, and the correlation between SOC and soil physical and chemical properties .The results showed that: (1) The SOC content in different vegetation types was significantly different.In the 20-40 cm topsoil ,the order of SOC content from big to small is that grassland> chestnut woodland> soybean field> corn field> metasequoia forest land. In the 20-40 cm soil, the order of SOC content is from small to large grassland> chestnut woodland> corn field> metasequoia woodland> soybean field . (2) In the 20-40 cm soil layer, the SOC content varies significantly with different soil thickness, and increases with the thickness of the overlying soil layer. The highest value is the sampling area with cover soil of 81-100 cm (4.06 ~ 5.87 g/kg). As the sampling depth increases, the SOC content gradually decreases, and as the thickness of the overlying soil layer deepens, the overall rate of decline is faster. (3) The effect of overlying vegetation type on the SOC content in the study area was greater than that of the soil thickness; there was no significant difference in the content of SOC under the interaction of the existing vegetation type and soil cover thickness in the study area. (4) There has a significant positive correlation between SOC and pH, a significant negative correlation with BD, and a positive correlation with WC (P>0.05).

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