高原地震
高原地震
고원지진
EARTHQUAKE RESEARCH IN PLATEAU
2011年
4期
41-47
,共7页
李桂清%吴学瑜%刘兆友%彭淑丽%张凤萍%李华平
李桂清%吳學瑜%劉兆友%彭淑麗%張鳳萍%李華平
리계청%오학유%류조우%팽숙려%장봉평%리화평
豫01井水位%热水开采%水位动态
豫01井水位%熱水開採%水位動態
예01정수위%열수개채%수위동태
Water level of Yu 01 well%Hot water mining%Water level dynamic
河南省濮阳地区地下热水的开采对处于同水层的地震观测井—豫01井水位观测产生了严重的干扰影响。豫01井水位自1996年9月出现下降变化以来,其水位动态一直受到大家的关注。十几年来,地震界专家学者对有可能影响该井水位动态的诸多因素逐一进行了追踪研究。认为豫01井自1996年9月至今水位变化与中原油田抽水、注水、采油无关;其补给区降雨量对豫01井的水位变化影响不大。经多方调查了解,收集了濮阳地区深度超1 000 m深井热水开采资料。分析研究认为,深井热水开采是引起豫01井水位下降的直接原因。
河南省濮暘地區地下熱水的開採對處于同水層的地震觀測井—豫01井水位觀測產生瞭嚴重的榦擾影響。豫01井水位自1996年9月齣現下降變化以來,其水位動態一直受到大傢的關註。十幾年來,地震界專傢學者對有可能影響該井水位動態的諸多因素逐一進行瞭追蹤研究。認為豫01井自1996年9月至今水位變化與中原油田抽水、註水、採油無關;其補給區降雨量對豫01井的水位變化影響不大。經多方調查瞭解,收集瞭濮暘地區深度超1 000 m深井熱水開採資料。分析研究認為,深井熱水開採是引起豫01井水位下降的直接原因。
하남성복양지구지하열수적개채대처우동수층적지진관측정—예01정수위관측산생료엄중적간우영향。예01정수위자1996년9월출현하강변화이래,기수위동태일직수도대가적관주。십궤년래,지진계전가학자대유가능영향해정수위동태적제다인소축일진행료추종연구。인위예01정자1996년9월지금수위변화여중원유전추수、주수、채유무관;기보급구강우량대예01정적수위변화영향불대。경다방조사료해,수집료복양지구심도초1 000 m심정열수개채자료。분석연구인위,심정열수개채시인기예01정수위하강적직접원인。
The exploitation of underground hot water in deep well had a serious interference to the observation of water level in Yu 01 well in the same water layer. It has been paid close attention to changes in decline of water level in Yu 01 well since Sep. 1996. Over the past decade, industry experts and scholars have a follow-up study on influence factors of the water level dynamic in the well. Considering that, the decline of water level of Yu 01 well has no relation with pumping water, water injection , oil mining of Zhongyuan oil field and the rainfall on the recharge zone. The authors gathered data on deep wells in Puyang areas after multiple investigations, and the results show that the exploitation of underground hot water is the direct reason to cause the decline of water level in Yu 01 well.