岩土力学
巖土力學
암토역학
ROCK AND SOIL MECHANICS
2014年
9期
2623-2633,2641
,共12页
匡冬琴%李琦%王永胜%王秀杰%林青%魏晓琛%宋然然
劻鼕琴%李琦%王永勝%王秀傑%林青%魏曉琛%宋然然
광동금%리기%왕영성%왕수걸%림청%위효침%송연연
CO2地质封存%深部咸水层%运移分布%数值模拟%神华CCS
CO2地質封存%深部鹹水層%運移分佈%數值模擬%神華CCS
CO2지질봉존%심부함수층%운이분포%수치모의%신화CCS
CO2 geological storage%deep saline aquifer%migration and distribution%numerical simulation%Shenhua CCS
CO2咸水层封存被广泛认为是一种具有大规模温室气体减排潜力的地学前缘技术。选取中国第一个全流程 CCS 项目为研究背景,结合工程实际情况,选取鄂尔多斯盆地为具体研究对象,提取相关参数,建立相应的地质模型,通过数值模拟研究咸水层多层统注时CO2在咸水中的主要封存机制、CO2在地层中的运移分布特征及其与注入能力的关系,并观测由于CO2注入引起的地层压力、CO2摩尔分数、酸碱度等的变化情况,为方案的进一步优化奠定基础。研究表明,CO2注入咸水层后,大部分进入储层上部,且注入能力越大时,注入的层位越多,注入量越大;CO2在咸水层中的存在形式有自由态、束缚态和溶解态。所有探索性研究的目的是给示范性项目的未来提供一个良好的基础优化方案。
CO2鹹水層封存被廣汎認為是一種具有大規模溫室氣體減排潛力的地學前緣技術。選取中國第一箇全流程 CCS 項目為研究揹景,結閤工程實際情況,選取鄂爾多斯盆地為具體研究對象,提取相關參數,建立相應的地質模型,通過數值模擬研究鹹水層多層統註時CO2在鹹水中的主要封存機製、CO2在地層中的運移分佈特徵及其與註入能力的關繫,併觀測由于CO2註入引起的地層壓力、CO2摩爾分數、痠堿度等的變化情況,為方案的進一步優化奠定基礎。研究錶明,CO2註入鹹水層後,大部分進入儲層上部,且註入能力越大時,註入的層位越多,註入量越大;CO2在鹹水層中的存在形式有自由態、束縳態和溶解態。所有探索性研究的目的是給示範性項目的未來提供一箇良好的基礎優化方案。
CO2함수층봉존피엄범인위시일충구유대규모온실기체감배잠력적지학전연기술。선취중국제일개전류정 CCS 항목위연구배경,결합공정실제정황,선취악이다사분지위구체연구대상,제취상관삼수,건립상응적지질모형,통과수치모의연구함수층다층통주시CO2재함수중적주요봉존궤제、CO2재지층중적운이분포특정급기여주입능력적관계,병관측유우CO2주입인기적지층압력、CO2마이분수、산감도등적변화정황,위방안적진일보우화전정기출。연구표명,CO2주입함수층후,대부분진입저층상부,차주입능력월대시,주입적층위월다,주입량월대;CO2재함수층중적존재형식유자유태、속박태화용해태。소유탐색성연구적목적시급시범성항목적미래제공일개량호적기출우화방안。
Geological storage of carbon dioxide (CO2) into deep saline aquifers is a leading-edge technology of greenhouse gas emissions reduction. The paper investigates China's first full-chain carbon capture and storage (CCS) project, i.e. Shenhua CCS demonstration project. Combining actual operation condition, the site of demonstration project in Ordos Basin is selected for the study. The relevant parameters are extracted to establish the geological model that is used to simulate multilayer injection of CO2 into deep saline aquifers. In order to analyze migration and distribution of CO2 while and after injection, the relationship between injection capacity and storage mechanisms of CO2 is investigated in detail. Additionally, it is also investigated on changes of formation pressure, CO2 phase, CO2 mole fraction and pH value. The numerical simulation shows that when CO2 is injected into deep saline aquifers, it is almost sequestered into the top of the reservoir. When the injection capacity is stronger, CO2 is injected into more layer formations, and the injection volume of CO2 is relatively bigger. The injected CO2 bears a very complicated phase state in deep saline aquifers. It is mixed with a free gas, trapped and dissolved phases. Simultaneously, when an injection rate is different, main phase types of injected CO2 into deep saline aquifers are different and they change with time. The change pattern of pH values is also different because of strength of seepage effect caused by different injection rates. All exploratory studies are aiming at building a good foundation to optimize future schemes of the demonstration project.