報(bào)告題目：Pore-Scale Experimental Studies of Two-Phase Flow, Mass and Heat Transport in Porous Media
報(bào) 告 人：Majid Hassanizadeh教授
報(bào)告時(shí)間：11月5日 10:30—12:00
報(bào)告地點(diǎn)：全國(guó)重點(diǎn)實(shí)驗(yàn)室A403
報(bào)告人簡(jiǎn)介：
Majid Hassanizadeh教授是歐洲科學(xué)院院士，國(guó)際多孔介質(zhì)學(xué)會(huì)（Interpore）執(zhí)行主席，荷蘭烏特列支大學(xué)地球科學(xué)系教授，德國(guó)斯圖加特大學(xué)高級(jí)教授，重慶大學(xué)客座教授，多次入選全球ESI高被引學(xué)者。他2021年當(dāng)選歐洲科學(xué)院院士，2019年獲得水文學(xué)終身成就霍頓獎(jiǎng)?wù)拢?012年當(dāng)選亨利達(dá)西杰出講師(Henry Darcy Distinguished Lecturer)。曾擔(dān)任滲流力學(xué)頂級(jí)期刊《Advances in Water Resources》主編、《Water Resources Research》副主編。主要從事地下能源與環(huán)境領(lǐng)域的滲流力學(xué)研究，包括兩相滲流的理論、數(shù)值和實(shí)驗(yàn)研究，孔尺度數(shù)值模擬、微流控實(shí)驗(yàn)研究、工業(yè)多孔介質(zhì)材料的滲流，土壤與地下水修復(fù)等。發(fā)表300多篇學(xué)術(shù)論文和著作，h因子為69，總被引超過(guò)20000次。
報(bào)告內(nèi)容摘要：
In recent decades, there have been major advances in experimental techniques for pore-scale studies of fluids flow and mass and heat transport in porous media. An effective and highly popular method is the use of micromodels, which allow direct observation of flow and transport on the pore scale, and thus help to increase our insight of flow and transport phenomena on both micro and macro-scales.
A micromodel is an artificial representation of a porous medium, made of a transparent material. In our studies, we have used Poly-Di-Methyl-Siloxane (PDMS), which is a viscoelastic, silicon-based organic polymer. It is optically transparent, inert, non-toxic, and non-flammable. We have studied capillary phenomena, colloid transport, and heat transfer during two-phase flow. We have shown that capillarity phenomena are controlled by fluid-fluid interfaces at the micro-scale. Phenomena such as Haines jump, snap off, and local drainage during imbibition can be clearly seen. We have used our results to produce macroscale data and test our Darcy scale models.
In colloid transport experiments, we directly observe colloids movement, their retention at solid-fluids and fluid-fluid interfaces, and their remobilization with the moving interface and contact lines. We have also performed kinetic heat transport experiments where the two fluids have distinctly different temperatures at the pore scale. Under such conditions, fluid-fluid interfaces play a major in heat transport processes. Our results are relevant for understanding processes in oil and gas reservoirs, soil and groundwater remediation. CO2 sequestration in geological formations, energy storage operations, and deep geothermal systems.
主辦單位：油氣藏地質(zhì)及開(kāi)發(fā)工程全國(guó)重點(diǎn)實(shí)驗(yàn)室
石油與天然氣工程學(xué)院
SPE成都分會(huì)、SPWLA西南分會(huì)
科學(xué)技術(shù)發(fā)展研究院
