Zobrazeno 1 - 10
of 17
pro vyhledávání: '"J. Schmalholz"'
Publikováno v:
Vadose Zone Journal. 3:1106-1115
In a study to investigate water content distributions inside a lysimeter in a noninvasive manner, we used ground penetrating radar (GPR) tomography. Our main objective was to evaluate the temporal changes and spatial distributions of the volumetric w
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::10f8d9a4f2de279426a2b7bd040a9eb3
https://doi.org/10.2113/3.4.1106
https://doi.org/10.2113/3.4.1106
Publikováno v:
Near Surface Geophysics. 1:173-181
Urban soils are subject to strong variations in environmental conditions, such as water flow, solute transport and heat budget. The INTERURBAN research project has been set up to investigate the dynamics of water and solutes at urban locations with p
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::fe3741f09f151ecca4d0e6f7dd435c59
https://doi.org/10.3997/1873-0604.2003008
https://doi.org/10.3997/1873-0604.2003008
Publikováno v:
Near Surface 2007 - 13th EAGE European Meeting of Environmental and Engineering Geophysics.
Four different moisture states inside an undisturbed soil monolith, in our case a lysimeter, (cylindrical vessel of 1.2 m diameter and 1.5 m height) are imaged with georadar tomography. Two of the moisture states correspond to different steady state
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::1073567cb0f7f05c715aa0ecf12f9f7f
https://doi.org/10.3997/2214-4609.20146575
https://doi.org/10.3997/2214-4609.20146575
Publikováno v:
Near Surface 2005 - 11th European Meeting of Environmental and Engineering Geophysics.
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::179d5714b30c3d876f51b1e82a5b975b
https://doi.org/10.3997/2214-4609-pdb.13.b049
https://doi.org/10.3997/2214-4609-pdb.13.b049
Publikováno v:
Near Surface 2005 - 11th European Meeting of Environmental and Engineering Geophysics.
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::471b19eb330dae4e031e43d298e42738
https://doi.org/10.3997/2214-4609-pdb.13.p044
https://doi.org/10.3997/2214-4609-pdb.13.p044
Publikováno v:
Near Surface 2004 - 10th EAGE European Meeting of Environmental and Engineering Geophysics.
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::98f12b7c5d3b263ec1bc7c6e7239b172
https://doi.org/10.3997/2214-4609-pdb.10.a026
https://doi.org/10.3997/2214-4609-pdb.10.a026
Publikováno v:
Near Surface 2004 - 10th EAGE European Meeting of Environmental and Engineering Geophysics.
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::f1fe3d5516b401b0c72b753414716963
https://doi.org/10.3997/2214-4609-pdb.10.b001
https://doi.org/10.3997/2214-4609-pdb.10.b001
Publikováno v:
9th EAGE/EEGS Meeting.
Urban soils are subject to strong variations of environmental conditions, like water flow, solute transport or heat budget. The research project INTERURBAN has been formed to study the dynamics of water and materials at urban locations with special c
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::22bb39a61fba14d3cdad2b8e729a5dd8
https://doi.org/10.3997/2214-4609.201414548
https://doi.org/10.3997/2214-4609.201414548
Publikováno v:
Field Screening Europe 2001 ISBN: 9789401039246
Mapping of subsurface contamination is one of the most important aims of environ–mental geophysics. For this purpose great efforts have been and will be carried out in the development of non-destructive geophysical mapping and monitoring techniques
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::053e08b5570ebbef72f61026a91a34de
https://doi.org/10.1007/978-94-010-0564-7_58
https://doi.org/10.1007/978-94-010-0564-7_58
Publikováno v:
Field Screening Europe 2001 ISBN: 9789401039246
The domestic waste site Karlsruhe-West was equipped in 1993 with a surface sealing system. This system mainly consists of a mineral clay liner (thickness 0.60 m) with an underlying capillary barrier and an upper gravel layer (thickness 0.15 m). To su
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::dba41aa07794cd741e95c5542c15f09f
https://doi.org/10.1007/978-94-010-0564-7_42
https://doi.org/10.1007/978-94-010-0564-7_42