水利水电科技进展
水利水電科技進展
수이수전과기진전
ADVANCES IN SCIENCE AND TECHNOLOGY OF WATER RESOURCES
2013年
4期
10-13
,共4页
曾明明%陈建生%王婷%何海清%何文政
曾明明%陳建生%王婷%何海清%何文政
증명명%진건생%왕정%하해청%하문정
堤坝渗漏%瞬态温度场%传热%渗透流速
隄壩滲漏%瞬態溫度場%傳熱%滲透流速
제패삼루%순태온도장%전열%삼투류속
dam seepage%transient temperature field%heat transmission%seepage velocity
为研究堤坝渗漏初期渗漏通道周围的温度场分布,结合集中渗漏通道自身特点假定渗漏通道为圆柱状,考虑到渗漏通道周围岩土体介质同时存在热对流与热传导两种热量交换形式,建立渗漏流体流动的瞬态温度场模型。根据确定的边界条件和初始条件,用分离变量推导出渗漏通道中的温度分布公式。将该模型应用于北江大堤石角段管涌地区,将实测的温度数据代入模型,反演出渗漏流速。计算结果表明:采用温度场模型反演得到的渗漏流速与同位素示踪法得到的渗透流速结果相近,验证了所建立的模型是可行的。
為研究隄壩滲漏初期滲漏通道週圍的溫度場分佈,結閤集中滲漏通道自身特點假定滲漏通道為圓柱狀,攷慮到滲漏通道週圍巖土體介質同時存在熱對流與熱傳導兩種熱量交換形式,建立滲漏流體流動的瞬態溫度場模型。根據確定的邊界條件和初始條件,用分離變量推導齣滲漏通道中的溫度分佈公式。將該模型應用于北江大隄石角段管湧地區,將實測的溫度數據代入模型,反縯齣滲漏流速。計算結果錶明:採用溫度場模型反縯得到的滲漏流速與同位素示蹤法得到的滲透流速結果相近,驗證瞭所建立的模型是可行的。
위연구제패삼루초기삼루통도주위적온도장분포,결합집중삼루통도자신특점가정삼루통도위원주상,고필도삼루통도주위암토체개질동시존재열대류여열전도량충열량교환형식,건립삼루류체류동적순태온도장모형。근거학정적변계조건화초시조건,용분리변량추도출삼루통도중적온도분포공식。장해모형응용우북강대제석각단관용지구,장실측적온도수거대입모형,반연출삼루류속。계산결과표명:채용온도장모형반연득도적삼루류속여동위소시종법득도적삼투류속결과상근,험증료소건립적모형시가행적。
In order to study the distribution of temperature fields around the leakage passage in the early period of dam seepage, the concentrated leakage passage can be regarded as a circular column based on its own characteristics. Based on two heat exchange patterns, heat conduction and heat convection in rock and soil media around the leakage passage, a transient temperature field model for dam seepage is established. According to the determined boundary and initial conditions, an equation for the temperature distribution in the leakage passage is derived by the separation of variables. The model is applied to the piping area of Shijiao reach of Beijiang Levee. The measured temperature data are substituted into the model, and the seepage velocity is obtained. The calculated results show that the seepage velocity obtained from the temperature field model is close to that gained from the isotope tracer method, and the feasibility of the proposed model is validated.