پژوهشگاه بین المللی زلزله شناسی و مهندسی زلزله فصلنامه علوم و مهندسی زلزله 2476-6097 2 2 2015 06 22 Updated Lagrangian Description of Large Deformation Analysis of Unsaturated Soils under Dynamic and Static Loadings فرمول‌بند‌ی محیطها‌ی خاکی غیراشباع در تغییر شکلها‌ی بزرگ تحت بارگذار‌ی دینامیکی و استاتیکی 23 31 240267 FA مسعود میرمحمدصادقی مجتمع عالی آموزشی و پژوهشی صنعت آب و برق اصفهان بهروز گتمیری دانشکده فنی دانشگاه تهران Journal Article 2016 01 24 Extensive areas of the earth are covered by unsaturated soils. Besides, construction of fills, embankments and earth dams are related to compacted soils, which are a very widespread class of unsaturated soils, and there are many geotechnical problems with these soils. The unsaturated soil is assumed to be a three-phase porous media with a solid phase and two fluid phases, water and air. Therefore, considerable attempts have been made to explain or to predict shear strength and volume change behaviour of unsaturated soils in terms of effective stress. Bishop [1] modified classical expression of effective stress for saturated soils to the unsaturated soils in the following form: )()(waappp−χ+−σ=σ′in which σ′ is effective stress,ap and wp are pore air and pore water pressure respectively, )(wapp− is suction and χ is a parameter that mainly depends on degree of saturation. Many researchers showed that the use of a unique effective stress relation was not fully satisfactory to describe the various aspects of unsaturated soil behavior. The more realistic behavior of unsaturated soils could be explained using state variables and two independent tensorial variables )(wapp− and )(ap−σ i.e. the total stress and suction, respectively) and state surface of void ratio (e) and degree of saturation (rS) that provide the variation of them with applied total stress and suction. For a given soil, if the fabric does not change significantly, void ratio and degree of saturation are main factors controlling permeability. There are also some empirical relationships based on suction. Thus the permeability of water and air are functions of void ratio and degree of saturation. To obtain the governing equations for the mechanics of unsaturated porous media, the continuity relations of water and air and the dissolved air in water (Henry’s law) are used. The motion of water and air can be described by generalized Darcy’s law. The total mechanical equilibrium is derived by summing of linear momentum balance of three phases and neglecting relative acceleration of fluids. The basic approach in the incremental step-by-step solution is to assume that the solution for time t is known and that the solution for the time t+dt is required. In large deformation analysis, special attention must be given to the fact that the configuration of the body is changing continuously. In the updated - lagrangian (UL) formulation, all static and kinematic variables are referred to the configuration at time t, and the second Piola-Kirchhoff stress and lagrangian strain tensors can be employed effectively at time t+dt. For linearizing, we use the Jaumann stress increments instead of second Piola-kirchhohh stress increments. By using the appropriate stress-strain relation for unsaturated soils and the weighted residual methods, the integral equations are obtained. Utilizing the appropriate shape functions, the basic finite element equations are obtained. In the solution of the nonlinear response, the governing equation must be satisfied at the complete time by using a step-by-step incremental analysis and an iteration procedure like modified Newton-Rophson method is used. For a quantitative solution, the resultant equations are discretized in time by Newmark’s solution and the final finite element equations are obtained. Finally, by the UDAMN finite element code, which developed by authors, two problems, i.e. the settlement of unsaturated ground under loading and step construction of an unsaturated embankment, have been solved by this method. در این مقاله جنبه‌های نظری و محاسباتی تحلیل محیط‌های خاکی غیراشباع در تغییر شکل‌های بزرگ ارائه شده است. خاک غیراشباع به‌صورت محیطی سه فازه در نظر گرفته شده است. با توجه به این‌که در حال حاضر کاملاً اثبات شده که برخی از نظریه‌های مورد استفاده در مکانیک خاک کلاسیک در مکانیک خاک غیراشباع کاربرد ندارد، به-جای نظریه تنش مؤثر کلاسیک، که در خاک‌های اشباع کاربرد فراوانی دارد، از دو متغیر مستقل تنسوری تنش خالص و مکش به‌عنوان متغیرهای حالت و نیز سطوح حالت نسبت پوکی و درجه اشباع که تابع این دو متغیر حالت هستند، جهت تبیین رفتار این خاک‌ها استفاده شده است. جریان فازهای سیال بر اساس قانون دارسی بیان شده و نفوذپذیری نسبت به آب‌وهوا تابعی از نسبت پوکی و درجه اشباع در نظر گرفته شده‌اند. با این فرضیات تحلیل تغییر شکل‌های بزرگ با استفاده از توصیف لاگرانژین به‌هنگام انجام گرفته و معادلات دیفرانسیل و اجزاء محدود کوپله حاکم بر محیط غیراشباع تحت بارگذاری کلی دینامیکی حاصل شده است. سپس بر اساس نرم‌افزار UDAMN که اصلاح‌شده نرم‌افزار UDAM بوده و در این تحقیق تهیه شده، مثال‌هایی از کاربرد این تحلیل ارائه شده است. https://www.bese.ir/article_240267_24a11b1dbe2df6b32867bb15e4cd3aa0.pdf