LEADER 02163nam0 2200397 i 450 001 SUN0124689 005 20191023021348.224 010 $d0.00 017 70$2N$a978-3-319-99689-9 100 $a20191023d2018 |0engc50 ba 101 $aeng 102 $aCH 105 $a|||| ||||| 200 1 $a*From particle systems to partial differential equations$ePSPDE V, Braga, Portugal, November 2016$fPatricia Gonçalves, Ana Jacinta Soares editors 205 $aCham : Springer, 2017 210 $avii$d167 p.$cill. ; 24 cm 215 $aPubblicazione in formato elettronico 410 1$1001SUN0102574$12001 $a*Springer proceedings in mathematics & statistics$v258$1210 $aBerlin$cSpringer$d2012-. 606 $a60K35$xInteracting random processes; statistical mechanics type models; percolation theory [MSC 2020]$2MF$3SUNC019993 606 $a35Qxx$xPartial differential equations of mathematical physics and other areas of application [MSC 2020]$2MF$3SUNC022881 606 $a82C40$xKinetic theory of gases in time-dependent statistical mechanics [MSC 2020]$2MF$3SUNC023377 606 $a60G60$xRandom fields [MSC 2020]$2MF$3SUNC023477 606 $a35L67$xShocks and singularities for hyperbolic equations [MSC 2020]$2MF$3SUNC023749 606 $a35R60$xPDEs with randomness, stochastic partial differential equations [MSC 2020]$2MF$3SUNC025169 606 $a60F17$xFunctional limit theorems; invariance principles [MSC 2020]$2MF$3SUNC033628 620 $aCH$dCham$3SUNL001889 702 1$aGonçalves$b, Patricia$3SUNV081224 702 1$aSoares$b, Ana Jacinta$3SUNV087557 712 12$aInternational Conference on Particle Systems and Partial Differential Equation$d5.$f2016$eBraga, Portugal$3SUNV096130 712 $aSpringer$3SUNV000178$4650 801 $aIT$bSOL$c20210503$gRICA 856 4 $uhttp://doi.org/10.1007/978-3-319-99689-9 912 $aSUN0124689 950 $aUFFICIO DI BIBLIOTECA DEL DIPARTIMENTO DI MATEMATICA E FISICA$d08CONS e-book 1144 $e08eMF1144 20191023 996 $aFrom particle systems to partial differential equations$91409990 997 $aUNICAMPANIA LEADER 00948nam 2200337Ia 450 001 996391916403316 005 20221108062614.0 035 $a(CKB)1000000000676325 035 $a(EEBO)2240938000 035 $a(OCoLC)12409790 035 $a(EXLCZ)991000000000676325 100 $a19850821d1691 uy | 101 0 $aeng 135 $aurbn||||a|bb| 200 04$aThe Congress at The Hague$b[electronic resource] 210 $aLondon $cPrinted for Ric. Baldwin ...$d1691 215 $a[6], 71, [1] p 300 $aAdvertisement: p. [1] at end. 300 $aDedication signed: C.W. 300 $aReproduction of original in Huntington Library. 330 $aeebo-0113 607 $aNetherlands$xHistory$y1648-1714 701 $aC. W$01006714 801 0$bEAA 801 1$bEAA 801 2$bm/c 801 2$bWaOLN 906 $aBOOK 912 $a996391916403316 996 $aThe Congress at The Hague$92364062 997 $aUNISA LEADER 04003oam 2200589zu 450 001 996217177003316 005 20210807004712.0 010 $a1-118-66739-5 035 $a(CKB)3450000000004138 035 $a(SSID)ssj0000904874 035 $a(PQKBManifestationID)11494234 035 $a(PQKBTitleCode)TC0000904874 035 $a(PQKBWorkID)10924121 035 $a(PQKB)10374937 035 $a(NjHacI)993450000000004138 035 $a(PPN)189492805 035 $a(EXLCZ)993450000000004138 100 $a20160829d1991 uy 101 0 $aeng 135 $aur||||||||||| 181 $ctxt 182 $cc 183 $acr 200 10$aPhysical and Hydrologic Flow Properties of Fractures Las Vegas, Nevada~%#~151;zion Canyon, Utah~%#~151;grand Canyon, Arizona~%#~151;yucca Mountain, Nevada, Field Trip T385 210 31$a[Place of publication not identified]$cAmerican Geophysical Union$d1991 215 $a1 online resource (ix, 36 pages) $cillustrations 225 1 $aField trip guidebook (International Geological Congress (28th : 1989 : Washington, D.C.)) ;$vT385 300 $aBibliographic Level Mode of Issuance: Monograph 311 $a0-87590-650-8 320 $aIncludes bibliographical references. 330 $aPublished by the American Geophysical Union as part of the Field Trip Guidebooks Series, Volume 385.Fractures are one of the most abundant structures in geology and are found in almost all rocks and soils at or near the Earth's surface. They are found over a wide range of length scales, from micro-fractures within mineral grams (micro-meters) to oceanic-intraplate fractures as much as 5000 km in length. The important role of fractures in fluid transport in the crust has long been recognized by geologists who have studied dikes (fracture conduits for flow of igneous rocks) and mineral veins fracture conduits for precipitation from aqueous Fluids. In studying these paleo-flow systems, little attention has been given to quantification of the flow properties of the system. Until two decades ago, hydrologists (Long, 1983) and petroleum-reservoir engineers (Nelson, 1985) studying fluid flow in rock had recognized the role of fractures only qualitatively. Quantitatively, the mathematics of fracture flow had been considered intractable while the mathematics of porous-media flow through the rock matrix had been developed and refined for almost one hundred ears. Direct observation of the flow properties of rock at field scales demonstrated the inadequacy of the porous media models beyond the scale of laboratory samples. The hydraulic conductivity of fractured bulk rock has been measured to be as much as 8 orders of magnitude greater than matrix hydraulic conductivity measured in laboratory samples of the same intact rock. Clearly, fractures are primary conduits for fluid flow in rock at time scales of economic and practical interest. Quantitative understanding of the physics of flow in individual fractures and fracture networks has become an important research topic with direct applications to contemporary and paleo flow systems. 410 0$aField trip guidebook (International Geological Congress (28th : 1989 : Washington, D.C.)) ;$vT385. 606 $aGroundwater flow 606 $aGroundwater flow$zArizona 606 $aGroundwater flow$zNevada 606 $aGroundwater flow$zUtah 606 $aFaults (Geology) 606 $aJoints (Geology) 615 0$aGroundwater flow. 615 0$aGroundwater flow 615 0$aGroundwater flow 615 0$aGroundwater flow 615 0$aFaults (Geology) 615 0$aJoints (Geology) 676 $a551.49 700 $aBarton$0880609 702 $aHsieh$b P. A. 801 0$bPQKB 906 $aBOOK 912 $a996217177003316 996 $aPhysical and Hydrologic Flow Properties of Fractures Las Vegas, Nevada~%#~151;zion Canyon, Utah~%#~151;grand Canyon, Arizona~%#~151;yucca Mountain, Nevada, Field Trip T385$91966682 997 $aUNISA