南京大学学报(自然科学版)
南京大學學報(自然科學版)
남경대학학보(자연과학판)
Journal of Nanjing University (Natural Sciences)
2015年
6期
1268-1278
,共11页
贺小桐%叶淑君%于军%吴吉春%龚绪龙
賀小桐%葉淑君%于軍%吳吉春%龔緒龍
하소동%협숙군%우군%오길춘%공서룡
速度场%地下水%地面沉降%数值模拟
速度場%地下水%地麵沉降%數值模擬
속도장%지하수%지면침강%수치모의
solid particle velocity%groundwater%land subsidence%numerical simulation
根据 Helm提出的基于固体颗粒速度场的含水层运动理论进行抽水型三维地面沉降建模。通过5个算例对该模型进行了验证并展示了其在不同水文地质条件不同抽水井布置条件下的理论运用。研究表明:基于固体颗粒速度场的三维地面沉降模型可以客观反映抽水引起的含水层的三维运动。基于固体颗粒速度场的三维地面沉降模型,直接将抽水引起的含水层系统中土体的三维运动与地下水水位变化相关联,不涉及复杂的土体本构关系,相较传统的流—固耦合模型或者解耦模型所需确定的参数较少,且无需求解大型的三维位移方程,从而实现以简单的模型快速有效地模拟三维地面沉降的目的。
根據 Helm提齣的基于固體顆粒速度場的含水層運動理論進行抽水型三維地麵沉降建模。通過5箇算例對該模型進行瞭驗證併展示瞭其在不同水文地質條件不同抽水井佈置條件下的理論運用。研究錶明:基于固體顆粒速度場的三維地麵沉降模型可以客觀反映抽水引起的含水層的三維運動。基于固體顆粒速度場的三維地麵沉降模型,直接將抽水引起的含水層繫統中土體的三維運動與地下水水位變化相關聯,不涉及複雜的土體本構關繫,相較傳統的流—固耦閤模型或者解耦模型所需確定的參數較少,且無需求解大型的三維位移方程,從而實現以簡單的模型快速有效地模擬三維地麵沉降的目的。
근거 Helm제출적기우고체과립속도장적함수층운동이론진행추수형삼유지면침강건모。통과5개산례대해모형진행료험증병전시료기재불동수문지질조건불동추수정포치조건하적이론운용。연구표명:기우고체과립속도장적삼유지면침강모형가이객관반영추수인기적함수층적삼유운동。기우고체과립속도장적삼유지면침강모형,직접장추수인기적함수층계통중토체적삼유운동여지하수수위변화상관련,불섭급복잡적토체본구관계,상교전통적류—고우합모형혹자해우모형소수학정적삼수교소,차무수구해대형적삼유위이방정,종이실현이간단적모형쾌속유효지모의삼유지면침강적목적。
Three-dimensional(3-D)land subsidence caused by groundwater extraction was simulated by using aquifer movement theory based on solid particle velocity,which was developed by Donald Helm.Two numerical experiments were conducted to verify the 3-D land subsidence models based on solid particle velocity.Three experiment demonstrated the application of models under different hydrogeological conditions and in different spatially arrangement of pumping wells.The result showed the three-dimensional motion caused by ground water pumpage. This model,based on solid particle velocity field,does not involved complex soil constitutive models.There are less parameters to be determined compared to traditional fluid-solid coupled or decoupled model,There are no large-scale three-dimensional displacement equations in this new 3-D land subsidence model,so that three-dimensional simulation of land subsidence can be achieved more efficiently by this kind of simplified model.