about
From Global to Local and Vice Versa: On the Importance of the 'Globalization' Agenda in Continental Groundwater Research and Policy-Making.Stable water isotope patterns in a climate change hotspot: the isotope hydrology framework of Corsica (western Mediterranean).Stable carbon isotope fractionation data between H(2)CO(3)(*) and CO(2)(g) extended to 120 °C.14C and delta13C characteristics of organic matter and carbonate in saltmarsh sediments from south west Scotland.Field-based stable isotope analysis of carbon dioxide by mid-infrared laser spectroscopy for carbon capture and storage monitoring.Acid rain footprint three decades after peak deposition: Long-term recovery from pollutant sulphate in the Uhlirska catchment (Czech Republic).The 2014 water release into the arid Colorado River delta and associated water losses by evaporation.Pleistocene paleo-groundwater as a pristine fresh water resource in southern Germany--evidence from stable and radiogenic isotopes.Carbon isotope fractionation during reductive dechlorination of TCE in batch experiments with iron samples from reactive barriers.Carbon isotope fractionation during abiotic reductive dehalogenation of trichloroethene (TCE).Quantification of long-term wastewater fluxes at the surface water/groundwater-interface: an integrative model perspective using stable isotopes and acesulfame.Stable isotope mass balances versus concentration differences of dissolved inorganic carbon - implications for tracing carbon turnover in reservoirs.Turnover and release of P-, N-, Si-nutrients in the Mexicali Valley (Mexico): interactions between the lower Colorado River and adjacent ground- and surface water systems.Deposition, persistence and turnover of pollutants: First results from the EU project AquaTerra for selected river basins and aquifers.Subsequence dynamic time warping as a method for robust step segmentation using gyroscope signals of daily life activities.Controls of evaporative irrigation return flows in comparison to seawater intrusion in coastal karstic aquifers in northern Sri Lanka: Evidence from solutes and stable isotopes.Assessment of land subsidence mechanisms triggered by dolomitic marble dissolution from hydrogeochemistry and stable isotopes of spring watersStabile Isotope als Tracer zur Bestimmung der Abstandsgeschwindigkeit in Trinkwassergewinnungsbrunnen aus UferfiltratSpatial and temporal variations ofpCO2, dissolved inorganic carbon and stable isotopes along a temperate karstic watercourseHigh-resolution stable carbon isotope monitoring indicates variable flow dynamic patterns in a deep saline aquifer at the Ketzin pilot site (Germany)Stable carbon isotope analysis of dissolved inorganic carbon (DIC) and dissolved organic carbon (DOC) in natural waters - Results from a worldwide proficiency testWell-based, Geochemical Leakage Monitoring of an Aquifer Immediately Above a CO2 Storage Reservoir by Stable Carbon Isotopes at the Ketzin Pilot Site, GermanyOptimization of instrument setup and post-run corrections for oxygen and hydrogen stable isotope measurements of water by isotope ratio infrared spectroscopy (IRIS)Applications of stable water and carbon isotopes in watershed research: Weathering, carbon cycling, and water balancesPredicting δ13CDIC dynamics in CCS: A scheme based on a review of inorganic carbon chemistry under elevated pressures and temperaturesGeochemical and isotope characterization of geothermal spring waters in Sri Lanka: Evidence for steeper than expected geothermal gradientsInter-laboratory test for oxygen and hydrogen stable isotope analyses of geothermal fluids: Assessment of reservoir fluid compositionsDynamics of dissolved organic carbon in hillslope discharge: Modeling and challengesStable carbon and oxygen equilibrium isotope fractionation of supercritical and subcritical CO 2 with DIC and H 2 O in saline reservoir fluidsFast 200 Billionen Liter später …Zu wenig Wasser oder zu wenig Zuversicht?Vorhang auf – Online ist on stageA Summary on the Special Issue “Sustainability of Groundwater”Hydrogeologie unter einem D-A-CH …Was ist neu bei Grundwasser? – Staffelstab übernommenControls on carbon cycling in two contrasting temperate zone estuaries: The Tyne and Tweed, UKIndications for pedogenic formation of perylene in a terrestrial soil profile: Depth distribution and first results from stable carbon isotope ratiosCan conductivity and stable isotope tracers determine water sources during flooding? An example from the Elbe River in 2002Automated analyses of18O/16O ratios in dissolved oxygen from 12-mL water samplesWater mixing in a St. Lawrence river embayment to outline potential sources of pollution
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Q30382296-7745DECF-DAED-4DC7-91D1-6746381F9997Q30736256-ACC25804-C8F1-4EF9-8F5C-8D9B45EE443AQ30833900-52705925-71DA-4F4E-8553-37B8ACB163A4Q31063276-C1E0FE0B-FF21-472A-98ED-02C74CB0771EQ35398358-1051A082-0893-4873-800B-E5375B792874Q38687275-49602D53-E770-41E3-A59A-6E2A38DE4D0FQ38945453-B1B0949A-5383-4BEF-A988-68DC9295330EQ39153649-C365F1A1-23B4-4623-BA8D-832EB830B6C3Q43367528-463E82EB-E934-4CAF-93D6-98F05E0B2D8FQ43712975-267A210E-4AA3-4EC2-B77D-F1D2DC534E96Q45396501-3C49A730-23F7-44E9-A833-A3863063B9FEQ46406738-7DCE05E3-A56C-4BE7-8115-D5B915C65472Q46811851-6D2CFFF1-B4D1-4294-B1B1-170457AF0D5DQ51064233-EC9DFC68-A2E2-47AF-B9BD-A0AB91EE0D49Q51153296-7D9A5270-834A-44A9-B21E-8E1E26DD4555Q53087673-CDEDB6BF-438A-4178-85C8-4A7A22EB8C3AQ58195389-8328BFF3-2DAD-4A9D-ACA3-8D05EAAF3307Q58195390-5F6DA826-C36F-4B85-82A5-E11C33275128Q58195398-2B30CE12-7563-4CEE-A362-81F63F2098ACQ58195399-999441B8-3FF2-4844-A6C1-2B27966833A4Q58195402-4D301758-ABDC-408B-912E-9B0C67E3D6FBQ58195404-B4A8A03F-2081-4BC9-BF63-4EDB7C7B860EQ58195405-530AB115-2EB4-45F7-BCE9-6FAA18DF9340Q58195408-903B1DA6-EE9B-4C31-8B12-F819B2C13D3BQ58195410-6557ED5A-139F-4A57-A9DC-EF316C8B69CDQ58199860-C7D9F5CE-E852-4CC7-9A70-99BC49825405Q58479046-6C971BB1-60F6-4C33-94DC-FB6F44900DD8Q58479051-240D9B23-32F1-4A5B-96E6-BA9F0C33B7ADQ58479054-303E4A46-99C0-4D40-A26B-2F5534AB2F64Q58479055-7FA134C9-C8B7-4673-AC76-DDB75524A873Q58479056-3857F4D5-BA5C-4CD2-9584-BFFDDB4E213CQ58479059-41E31353-32BC-47AF-8205-A293AFD2F7DEQ58479060-93961200-820F-45D5-B82A-577A1FFC9D3DQ58479062-5D408A3F-E593-44CE-8313-844194119E61Q58479063-B673DEEF-B79C-44B8-AB43-3FDBB6CFD7DDQ58479066-190D7D6D-C74E-4C41-A916-02274E3B3636Q58479070-0AAD11EC-7DD2-44E0-875D-DD7B562763F9Q58479071-5C881B28-B839-42FC-A650-817A23A9618EQ58479076-6B24D011-C5F0-464A-949F-811FD3AE9C00Q58479077-29550586-E746-4B82-AEF4-6040946945DF
P50
description
onderzoeker
@nl
researcher ORCID ID = 0000-0002-3494-4507
@en
name
Johannes Barth
@ast
Johannes Barth
@en
Johannes Barth
@es
Johannes Barth
@nl
type
label
Johannes Barth
@ast
Johannes Barth
@en
Johannes Barth
@es
Johannes Barth
@nl
prefLabel
Johannes Barth
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Johannes Barth
@en
Johannes Barth
@es
Johannes Barth
@nl
P1053
C-6723-2013
P106
P1153
25926907600
P21
P31
P3829
P3835
johannes-barth2
P496
0000-0002-3494-4507