Scanlon, T.M., Raffensperger, J.P. and Hornberger, G.M. (2001) Modeling Transport of Dissolved Silica in a Forested Headwater Catchment: Implications for Defining the Hydrochemical Response of Observed Flow Pathways. Water Resources Research, 37, 1071-1082.
http://dx.doi.org/10.1029/2000WR900278

has been cited by the following article:

• TITLE: Short Report: Identifying Sources of Subsurface Flow—A Theoretical Framework Assessing Hydrological Implications of Lithological Discontinuities

  AUTHORS: Martin Reiss, Peter Chifflard

  KEYWORDS: Subsurface Runoff, Soil Solution, Hillslope Hydrology, Cover Beds, Geochemical Barriers

  JOURNAL NAME: Open Journal of Modern Hydrology, Vol.4 No.3, July 4, 2014

  ABSTRACT: An integrative theoretical concept—combining scientific approaches from soil science and slope hydrology—is given as a framework to study the influence of depth functions of geochemical concentrations for trace elements, dissolved organic carbon and stable isotopes in the soil pore water of stratified soils on the chemical composition of the hillslope runoff. Combining investigations at the point and hillslope scale opens the opportunity to identify sources of subsurface runoff components using geochemical depth functions as proxies.