LEADER 04684nam 22011293a 450 001 9910367756603321 005 20250203235432.0 010 $a9783039210756 010 $a3039210750 024 8 $a10.3390/books978-3-03921-075-6 035 $a(CKB)4100000010106151 035 $a(oapen)https://directory.doabooks.org/handle/20.500.12854/40286 035 $a(ScCtBLL)636d6e1d-4722-43cb-bedd-5e6ee15c5f67 035 $a(OCoLC)1163826496 035 $a(oapen)doab40286 035 $a(EXLCZ)994100000010106151 100 $a20250203i20192019 uu 101 0 $aeng 135 $aurmn|---annan 181 $ctxt$2rdacontent 182 $cc$2rdamedia 183 $acr$2rdacarrier 200 00$aAdvances in Groundwater Flow and Solute Transport : $ePushing The Hidden Boundary /$fQuanrong Wang, Zhang Wen, Hongbin Zhan 210 $cMDPI - Multidisciplinary Digital Publishing Institute$d2019 210 1$aBasel, Switzerland :$cMDPI,$d2019. 215 $a1 electronic resource (196 p.) 311 08$a9783039210749 311 08$a3039210742 330 $aIn recent decades, the study of groundwater flow and solute transport has advanced into new territories that are beyond conventional theories, such as Darcy's law and Fick's law. The studied media have changed from permeable porous and fractured ones to much less permeable ones, such as clay and shale. The studied pore sizes have also changed from millimetres to micro-meters or even nano-meters. The objective of this Special Issue is to report recent advances in groundwater flow and solute transport that push the knowledge boundary into new territories which include, but are not limited to, flow and transport in sloping aquifer/hillslopes, coupled unsaturated and saturated flow, coupled aquifer-vertical/horizontal/slant well flow, interaction of aquifer with connected and disconnected rivers, non-Darcian flow, anomalous transport beyond the Fickian scheme, and flow and transport in extremely small pore spaces such as shale and tight sandstones. Contributions focusing on innovative experimental, numerical, and analytical methods for understanding unconventional problems, such as the above-listed ones, are encouraged, and contributions addressing flow and transport at interfaces of different media and crossing multiple temporal and spatial scales are of great value 606 $aEnvironmental science, engineering & technology$2bicssc 610 $aLevy stable distribution 610 $apermeameter test 610 $arough single fracture 610 $aseawater intrusion 610 $athe Beishan area 610 $agroundwater flow model 610 $aslenderness effect 610 $aSW-GW interaction 610 $asemi-analytical solution 610 $aassessment 610 $ahydraulic conductivity 610 $airrigation 610 $afirst-order analytical approach 610 $aUlan Buh Desert 610 $aIUM 610 $asolute longitudinal dispersion 610 $asoil formation 610 $aDSR 610 $abimsoils 610 $anuclear waste disposal 610 $aIUV 610 $ainfiltration 610 $aTOUGH2 610 $asustainable development 610 $agroundwater ERT 610 $anon-Darcian 610 $anon-Fickian 610 $aGFModel 610 $aerosion 610 $apermeability coefficient 610 $ahydrologic exchange 610 $aevaporation calculation 610 $aevolving-scale log-conductivity 610 $aradioactive contaminant 610 $afield measurements 610 $afractured aquifers 610 $adesert farmland 610 $aanalytical solution 610 $asilty clay 610 $auncertainty 610 $asteady-state vertical flux 610 $aflow modeling 610 $anon-Darcy flow 610 $apercolation 610 $aMonte Carlo 610 $asolute transport 610 $agroundwater flow 610 $asalinity map 610 $anumerical simulation 610 $astochastic Lagrangian framework 610 $aunsaturated flow 610 $afractional derivative 610 $awater resource utilization efficiency 610 $aheterogeneity 610 $aperturbation method 610 $aColumbia River 610 $awater flow 615 7$aEnvironmental science, engineering & technology 700 $aWang$b Quanrong$01787271 702 $aWen$b Zhang 702 $aZhan$b Hongbin 801 0$bScCtBLL 801 1$bScCtBLL 906 $aBOOK 912 $a9910367756603321 996 $aAdvances in Groundwater Flow and Solute Transport$94320137 997 $aUNINA