石油与天然气地质 ›› 1984, Vol. 5 ›› Issue (1): 37-45.doi: 10.11743/ogg19840105

• 论文 • 上一篇    下一篇

碳酸盐土与可燃有机矿藏

殷乾根1, 陈荣书2   

  1. 1. 武汉市沼气建设领导小组办公室;
    2. 武汉地质学院
  • 收稿日期:1983-01-24 出版日期:1984-03-25 发布日期:2012-01-16

CARBONATE-SOIL RELATED TO COMBUSTIBLE ORGANIC DEPOSITS

Yin Qiangen1, Chen Rongshu2   

  1. 1. Section of Marsh Gas Utilization, Wuhan City;
    2. Wuhan College of Geology
  • Received:1983-01-24 Online:1984-03-25 Published:2012-01-16

摘要:

可燃有机矿藏附近,往往覆盖着不同类型的碳酸盐土。研究和揭示其相关性,既可为农业土壤改良服务,又有可能预测地下可燃有机矿藏。

Abstract:

1)Combustible organic deposits often coexist with soda saline-alkalai soil,drab soil and sajong black soil.All these kind of carbonate-rich soils are called carbonate-soils in this paper.2)Large amount of CO2 is emitted during the formation of the combusti-ble organic deposits.As confirmed by regional mapping,the landscape of gas-bearing soils in Song-Nen Basin,as well as the concentration of soda there in soils are related in some extent to the gas of Daqing Oilfield.3)Having determind the background value of carbonates in soils of a se-dimentary basin and contoured its abnormal zones,can one roughly point out the organic carbon-rich areas beneath the soils.There are three carbonate-soil zones in China,which involved partially the nine big oil-bearing sedimentary basins and drab soil zones.Numerous combustible organic deposits could be found in these three large carbonate-soil zones.