Ⅰ. 지하수의 이동
1. 공극률과 투수도
공극률은 공극이라 불리는 열린 공간을 갖는 토양 혹은 기반암의 전체에 대한 공극 체적의 비이다. 즉 주어진 체적의 퇴적물 혹은 암석이 포함할 수 있는 물의 양을 결정하는 것이 공극률이다. 퇴적물의 공극률은 구성입자배열의 치밀도와 입자들의 크기 및
II. How is CBM formed
Coalbed methane (CH4) forms in one of two ways. During the earliest stage of coalification (the process that turns plant detritus into coal), biogenic methane is generated as a by-product of bacterial respiration. Aerobic bacteria (those that use oxygen in respiration) first metabolize any free oxygen left in the plant remains and the surrounding sediments. In fresh water
1. 지원서-이력서
Eun Yong Kim
가. RESEARCH INTERESTS
• Joint and fault spacing and mechanisms for jointing and faulting
• Fracture characterization in aquifers and hydrocarbon reservoirs
• Poroelasticity and abnormal fluid pressure in sedimentary basins
• Crustal stress and deformation fields and their relationships to jointing, faulting, fluid migration