This paper combines porosity change and compression coefficient with the help of compression proposed by Zimmerman. It proves theoretically the porosity change of rock in the process of elastic deformation.

 
  • 借助于Zimmerman提出的壓縮系數及其相關(guān)關(guān)系,將孔隙度變化與壓縮系數結合起來(lái),從理論上證明了巖石在彈性變形過(guò)程中孔隙度的變化情況。
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