岩土力学
巖土力學
암토역학
ROCK AND SOIL MECHANICS
2013年
7期
1913-1922
,共10页
肖维民%夏才初%王伟%卞跃威
肖維民%夏纔初%王偉%卞躍威
초유민%하재초%왕위%변약위
岩石力学%粗糙节理%闭合变形%隙宽%曲折因子%接触面积
巖石力學%粗糙節理%閉閤變形%隙寬%麯摺因子%接觸麵積
암석역학%조조절리%폐합변형%극관%곡절인자%접촉면적
rock mechanics%rough joint%closure deformation%aperture%tortuosity coefficient%contact area
节理中接触面积的存在使得渗流曲折效应更加明显,将对渗流产生显著影响。为了研究节理接触面积对节理渗流的影响,建立节理渗流概念模型,推导得到了节理渗流的接触面积影响系数;然后在节理渗流计算公式中引入该影响系数,得到了考虑接触面积影响的渗流计算公式。同时,由于接触面积的存在使得渗流曲折因子的计算更为复杂,在获得节理隙宽分布的基础上提出了计算节理渗流曲折因子的五点比较法。然后以人工大理岩节理试件为研究对象,在获得其三维表面形貌的基础上,一方面对其进行不同接触状态下5级法向应力作用下的渗流试验;另一方面,在根据节理试件的三维表面形貌数据计算节理的渗流平均曲折因子和接触面积比的基础上,分别采用考虑接触面积影响的渗流计算公式和Zimmerman 计算公式对节理试件在不同法向应力作用下的渗流体积流量进行计算,并将计算结果与实测值进行比较。结果表明:考虑接触面积影响的渗流计算公式计算结果与实测值吻合较好,从而验证了考虑接触面积影响的渗流计算公式的正确性,而 Zimmerman计算公式高估了节理的渗流流量。
節理中接觸麵積的存在使得滲流麯摺效應更加明顯,將對滲流產生顯著影響。為瞭研究節理接觸麵積對節理滲流的影響,建立節理滲流概唸模型,推導得到瞭節理滲流的接觸麵積影響繫數;然後在節理滲流計算公式中引入該影響繫數,得到瞭攷慮接觸麵積影響的滲流計算公式。同時,由于接觸麵積的存在使得滲流麯摺因子的計算更為複雜,在穫得節理隙寬分佈的基礎上提齣瞭計算節理滲流麯摺因子的五點比較法。然後以人工大理巖節理試件為研究對象,在穫得其三維錶麵形貌的基礎上,一方麵對其進行不同接觸狀態下5級法嚮應力作用下的滲流試驗;另一方麵,在根據節理試件的三維錶麵形貌數據計算節理的滲流平均麯摺因子和接觸麵積比的基礎上,分彆採用攷慮接觸麵積影響的滲流計算公式和Zimmerman 計算公式對節理試件在不同法嚮應力作用下的滲流體積流量進行計算,併將計算結果與實測值進行比較。結果錶明:攷慮接觸麵積影響的滲流計算公式計算結果與實測值吻閤較好,從而驗證瞭攷慮接觸麵積影響的滲流計算公式的正確性,而 Zimmerman計算公式高估瞭節理的滲流流量。
절리중접촉면적적존재사득삼류곡절효응경가명현,장대삼유산생현저영향。위료연구절리접촉면적대절리삼류적영향,건립절리삼류개념모형,추도득도료절리삼류적접촉면적영향계수;연후재절리삼류계산공식중인입해영향계수,득도료고필접촉면적영향적삼류계산공식。동시,유우접촉면적적존재사득삼류곡절인자적계산경위복잡,재획득절리극관분포적기출상제출료계산절리삼류곡절인자적오점비교법。연후이인공대리암절리시건위연구대상,재획득기삼유표면형모적기출상,일방면대기진행불동접촉상태하5급법향응력작용하적삼류시험;령일방면,재근거절리시건적삼유표면형모수거계산절리적삼류평균곡절인자화접촉면적비적기출상,분별채용고필접촉면적영향적삼류계산공식화Zimmerman 계산공식대절리시건재불동법향응력작용하적삼류체적류량진행계산,병장계산결과여실측치진행비교。결과표명:고필접촉면적영향적삼류계산공식계산결과여실측치문합교호,종이험증료고필접촉면적영향적삼류계산공식적정학성,이 Zimmerman계산공식고고료절리적삼류류량。
The contact area will make flow tortuosity more obvious and influence the flow rate significantly. In order to investigate the effect of contact area on fluid flow through joint, a conceptual flow model is established to obtain the contact influential coefficient. And the influential coefficient is introduced into the equation for flow rate calculation considering the effect of tortuosity; a new equation considering the effect of contact area is derived. As the contact area makes the calculation of tortuosity coefficient more complicated, an algorithm for calculating the average tortuosity coefficient is proposed based on the joint aperture distribution. An artificial marble joint is taken as an object and the surface topography data are scanned. In one hand, flow tests are carried out on the joint specimen under five levels of normal stresses. In the other hand, on the basis of the average tortuosity coefficients and contact area ratios of joint specimen under five levels of normal stresses calculated according to the joint surface topography data, the volumetric flow rates through joint specimen are predicted by the new equation considering contact area presented in this paper and Zimmerman's equation, respectively. Then the predictions of the two equations are compared with experimental observations. It is shown from the comparison results that the predictions of the new equation agree well with experimental observations, while Zimmerman's equation overestimates the flow rate through the joint, thus validating the veracity of the new equation.