吉林大学学报(地球科学版)
吉林大學學報(地毬科學版)
길림대학학보(지구과학판)
JOURNAL OF JILIN UNIVERSITY(EARTH SCIENCE EDITION)
2014年
5期
1633-1646
,共14页
雷宏武%金光荣%李佳琦%石岩%冯波
雷宏武%金光榮%李佳琦%石巖%馮波
뢰굉무%금광영%리가기%석암%풍파
增强地热系统%热%水动力耦合%数值模拟%松辽盆地
增彊地熱繫統%熱%水動力耦閤%數值模擬%鬆遼盆地
증강지열계통%열%수동력우합%수치모의%송료분지
enhanced geothermal system%coupled thermal-hydrodynamic processes%numerical simulation%Songliao basin
增强型地热系统地热能开发涉及到热和水动力的耦合,对应的温度和压力场时空变化特征是评价地热开发效果的关键问题。基于松辽盆地徐家围子深部地质条件,采用 TOUGH2进行了地热能开发过程中裂隙孔隙介质系统中温度和压力变化的数值模拟,分析了不同埋深水平情况下地热能开发的差别,研究了孔隙基质和裂隙介质的渗透率和孔隙度、岩石导热系数、井径、注入压力、注入温度及裂隙周围基质因素对地热能开发的影响。结果表明:采用定压力开发时生产井抽出控制整个区域的压力分布,压力梯度在注入井区域较大,并随着开发的进行,注入井的注入对压力的影响逐渐增大;温度由注入井到生产井逐渐增大,并随着开发的进行温度降低范围逐渐向生产井扩大;质量和热提取速率随时间逐渐减小。不同埋深位置的模拟结果显示,埋深大的温度相对较高,水的流动性较强,质量和热提取速率较高,压力和温度变化幅度均较大。裂隙系统的渗透率、注入井/生产井压力和注入温度、井径对深部地热开采过程中的压力和温度影响较大,从而影响热的提取效率;而孔隙基质的渗透率和孔隙度、裂隙介质的裂隙度和岩石的热传导系数的影响并不明显。
增彊型地熱繫統地熱能開髮涉及到熱和水動力的耦閤,對應的溫度和壓力場時空變化特徵是評價地熱開髮效果的關鍵問題。基于鬆遼盆地徐傢圍子深部地質條件,採用 TOUGH2進行瞭地熱能開髮過程中裂隙孔隙介質繫統中溫度和壓力變化的數值模擬,分析瞭不同埋深水平情況下地熱能開髮的差彆,研究瞭孔隙基質和裂隙介質的滲透率和孔隙度、巖石導熱繫數、井徑、註入壓力、註入溫度及裂隙週圍基質因素對地熱能開髮的影響。結果錶明:採用定壓力開髮時生產井抽齣控製整箇區域的壓力分佈,壓力梯度在註入井區域較大,併隨著開髮的進行,註入井的註入對壓力的影響逐漸增大;溫度由註入井到生產井逐漸增大,併隨著開髮的進行溫度降低範圍逐漸嚮生產井擴大;質量和熱提取速率隨時間逐漸減小。不同埋深位置的模擬結果顯示,埋深大的溫度相對較高,水的流動性較彊,質量和熱提取速率較高,壓力和溫度變化幅度均較大。裂隙繫統的滲透率、註入井/生產井壓力和註入溫度、井徑對深部地熱開採過程中的壓力和溫度影響較大,從而影響熱的提取效率;而孔隙基質的滲透率和孔隙度、裂隙介質的裂隙度和巖石的熱傳導繫數的影響併不明顯。
증강형지열계통지열능개발섭급도열화수동력적우합,대응적온도화압력장시공변화특정시평개지열개발효과적관건문제。기우송료분지서가위자심부지질조건,채용 TOUGH2진행료지열능개발과정중렬극공극개질계통중온도화압력변화적수치모의,분석료불동매심수평정황하지열능개발적차별,연구료공극기질화렬극개질적삼투솔화공극도、암석도열계수、정경、주입압력、주입온도급렬극주위기질인소대지열능개발적영향。결과표명:채용정압력개발시생산정추출공제정개구역적압력분포,압력제도재주입정구역교대,병수착개발적진행,주입정적주입대압력적영향축점증대;온도유주입정도생산정축점증대,병수착개발적진행온도강저범위축점향생산정확대;질량화열제취속솔수시간축점감소。불동매심위치적모의결과현시,매심대적온도상대교고,수적류동성교강,질량화열제취속솔교고,압력화온도변화폭도균교대。렬극계통적삼투솔、주입정/생산정압력화주입온도、정경대심부지열개채과정중적압력화온도영향교대,종이영향열적제취효솔;이공극기질적삼투솔화공극도、렬극개질적렬극도화암석적열전도계수적영향병불명현。
The geothermal energy exploitation in enhanced geothermal system involves the coupled processes of temperature and pressure,the spatial and temporal variation of which is the key issue. Based on the deep geological condition of Xujiaweizi in Songliao basin,using the TOUGH2 software,we simulate the variation of temperature and pressure in fracture-matrix media system, analyze the difference of geothermal development in different depth levels,and study the effects of important factors including the permeability and porosity of porous and fractured media,rock thermal conductivity,well radius,injection pressure and temperature,and surrounding matrix.The results show the pressure distribution is dominated by production well with large pressure gradient at the injection well and the impact of injection well increases with time.Temperature increases from injection well to production well and the area of decrease of temperature increases as the development of geothermal.Mass and heat extraction rate reduce and stabilize with time.The simulation results of different depth levels indicate the great mass and heat extraction rate and large change of pressure and temperature exist in the big depth level because of large water mobility. The effects of factors including fractured media permeability,injection/production well pressure and temperature,and well radius on pressure and temperature of the system are great,and ultimately it affects heat extraction efficiency.While the effects of another factors are not obvious.