These tools will no longer be maintained as of December 31, 2024. Archived website can be found here. PubMed4Hh GitHub repository can be found here. Contact NLM Customer Service if you have questions.


BIOMARKERS

Molecular Biopsy of Human Tumors

- a resource for Precision Medicine *

258 related articles for article (PubMed ID: 29732535)

  • 21. Strontium isotopes as tracers of water-rocks interactions, mixing processes and residence time indicator of groundwater within the granite-carbonate coastal aquifer of Bonifacio (Corsica, France).
    Santoni S; Huneau F; Garel E; Aquilina L; Vergnaud-Ayraud V; Labasque T; Celle-Jeanton H
    Sci Total Environ; 2016 Dec; 573():233-246. PubMed ID: 27565532
    [TBL] [Abstract][Full Text] [Related]  

  • 22. Hydrochemical evolution and groundwater flow processes in the Galilee and Eromanga basins, Great Artesian Basin, Australia: a multivariate statistical approach.
    Moya CE; Raiber M; Taulis M; Cox ME
    Sci Total Environ; 2015 Mar; 508():411-26. PubMed ID: 25497681
    [TBL] [Abstract][Full Text] [Related]  

  • 23. Closed-form approximations for two-dimensional groundwater age patterns in a fresh water lens.
    Greskowiak J; Röper T; Post VE
    Ground Water; 2013; 51(4):629-34. PubMed ID: 23025689
    [TBL] [Abstract][Full Text] [Related]  

  • 24. Identifying aquifer type in fractured rock aquifers using harmonic analysis.
    Rahi KA; Halihan T
    Ground Water; 2013; 51(1):76-82. PubMed ID: 22463080
    [TBL] [Abstract][Full Text] [Related]  

  • 25. Investigating groundwater flow between Edwards and Trinity aquifers in central Texas.
    Wong CI; Kromann JS; Hunt BB; Smith BA; Banner JL
    Ground Water; 2014; 52(4):624-39. PubMed ID: 24033308
    [TBL] [Abstract][Full Text] [Related]  

  • 26. Modeling flow into horizontal wells in a Dupuit-Forchheimer model.
    Haitjema H; Kuzin S; Kelson V; Abrams D
    Ground Water; 2010; 48(6):878-83. PubMed ID: 20331744
    [TBL] [Abstract][Full Text] [Related]  

  • 27. Groundwater flow velocities in a fractured carbonate aquifer-type: Implications for contaminant transport.
    Medici G; West LJ; Banwart SA
    J Contam Hydrol; 2019 Apr; 222():1-16. PubMed ID: 30795856
    [TBL] [Abstract][Full Text] [Related]  

  • 28. Analytical model for computing residence times near a pumping well.
    Simpson MJ; Clement TP; Yeomans FE
    Ground Water; 2003; 41(3):351-4. PubMed ID: 12772828
    [TBL] [Abstract][Full Text] [Related]  

  • 29. A new method for estimating recharge to unconfined aquifers using differential river gauging.
    McCallum AM; Andersen MS; Acworth RI
    Ground Water; 2014; 52(2):291-7. PubMed ID: 23550897
    [TBL] [Abstract][Full Text] [Related]  

  • 30. Recharge and residence times of groundwater in hyper arid areas: The confined aquifer of Calama, Loa River Basin, Atacama Desert, Chile.
    Herrera C; Godfrey L; Urrutia J; Custodio E; Jordan T; Jódar J; Delgado K; Barrenechea F
    Sci Total Environ; 2021 Jan; 752():141847. PubMed ID: 33207522
    [TBL] [Abstract][Full Text] [Related]  

  • 31. Evolution model of δ³⁴S and δ¹⁸O in dissolved sulfate in volcanic fan aquifers from recharge to coastal zone and through the Jakarta urban area, Indonesia.
    Hosono T; Delinom R; Nakano T; Kagabu M; Shimada J
    Sci Total Environ; 2011 Jun; 409(13):2541-54. PubMed ID: 21507462
    [TBL] [Abstract][Full Text] [Related]  

  • 32. Assessment of confined aquifer response to recharge variations and water inflow distributions using analytical approach.
    Zarif Sanayei HR; Javdanian H; Rakhshandehroo GR
    Environ Sci Pollut Res Int; 2021 Sep; 28(36):50878-50889. PubMed ID: 33973116
    [TBL] [Abstract][Full Text] [Related]  

  • 33. Use of Groundwater Level Fluctuations near an Operating Water Supply Well to Estimate Aquifer Transmissivity.
    Pozdniakov S; Ivanov P; Davis P; Sizov N
    Ground Water; 2021 Jan; 59(1):49-58. PubMed ID: 32588432
    [TBL] [Abstract][Full Text] [Related]  

  • 34. Interaction of Aquifer and River-Canal Network near Well Field.
    Ghosh NC; Mishra GC; Sandhu CS; Grischek T; Singh VV
    Ground Water; 2015; 53(5):794-805. PubMed ID: 25294130
    [TBL] [Abstract][Full Text] [Related]  

  • 35. A Black Hills-Madison Aquifer origin for Dakota Aquifer groundwater in northeastern Nebraska.
    Stotler R; Harvey FE; Gosselin DC
    Ground Water; 2010; 48(3):448-64. PubMed ID: 19840126
    [TBL] [Abstract][Full Text] [Related]  

  • 36. Assessing the recharge of a coastal aquifer using physical observations, tritium, groundwater chemistry and modelling.
    Santos IR; Zhang C; Maher DT; Atkins ML; Holland R; Morgenstern U; Li L
    Sci Total Environ; 2017 Feb; 580():367-379. PubMed ID: 27989474
    [TBL] [Abstract][Full Text] [Related]  

  • 37. Highly parameterized inversion of groundwater reactive transport for a complex field site.
    Carniato L; Schoups G; van de Giesen N; Seuntjens P; Bastiaens L; Sapion H
    J Contam Hydrol; 2015 Feb; 173():38-58. PubMed ID: 25528244
    [TBL] [Abstract][Full Text] [Related]  

  • 38. An improved method of recharge sources analysis and its application in an unconfined aquifer.
    Huang Y; Yan N; Zheng X; Liu G
    J Environ Manage; 2021 Jul; 290():112582. PubMed ID: 33930696
    [TBL] [Abstract][Full Text] [Related]  

  • 39. Mobilization of arsenic and other naturally occurring contaminants in groundwater of the Main Ethiopian Rift aquifers.
    Rango T; Vengosh A; Dwyer G; Bianchini G
    Water Res; 2013 Oct; 47(15):5801-18. PubMed ID: 23899878
    [TBL] [Abstract][Full Text] [Related]  

  • 40. Characteristics and origin of clogging-functional bacteria during managed aquifer recharge: A laboratory study.
    Xia L; You H; Liu J; Wu W; Lin L
    J Environ Manage; 2022 Jun; 312():114880. PubMed ID: 35305358
    [TBL] [Abstract][Full Text] [Related]  

    [Previous]   [Next]    [New Search]
    of 13.