|
|
||||||||
,b
a Laboratory of Soil and Water, Katholieke Universiteit Leuven, Vital Decosterstraat 102, B-3000 Leuven, Belgium
b Soil Physics, Inst. of Terrestrial Ecology, Swiss Federal Institute of Technology, ETHZ, Grabenstrasse 11a, CH-8952 Schlieren, Switzerland
* Corresponding author currently at, Inst. for Chemistry and Dynamics of the Geosphere, ICG-IV Agrospere, Research Center Jülich, D-52425 Jülich, Germany; (j.vanderborght{at}fz-juelich.de)
To investigate transport processes in soils, detailed information about the spatial distribution of solutes is required. We describe a method to obtain concentration maps of fluorescent tracers on cross sections of soil cores with a high spatial resolution. The fluorescence signal of two dye tracers, brilliant sulfaflavine (BF; 1H-Benz(de)isoquinoline-5-sulfonic acid, 2,3-dihydro-6-amino-1,3-dioxo-2-(p-tolyl)-, monosodium salt) and sulforhodamine B (SB; xanthylium, 3,6-bis(diethylamino)-9-(2,4-disulfophenyl)-, inner salt, sodium salt), was imaged on the exposed cross sections. The fluorescence signal was corrected for variable illumination light intensity and optical properties of the soil across the exposed surface. Correction factors for varying optical soil properties were derived from the image of the reflected excitation light at the exposed surface. Linear calibration relations related the corrected fluorescence image to the total tracer concentration (Ct) map, that is, mass of dye dissolved in the soil solution and sorbed to the soil particles per unit volume bulk soil. Corrections for varying optical properties of the soil surface were important to reduce the uncertainty of the concentration that was estimated from the fluorescence signal. For BF, the calibration relations were different for different soil materials and a soil specific calibration had to be used. Variations in background fluorescence were an important source of uncertainty of the BF concentration estimates but can be overcome by applying higher concentrations. For SB, variations in calibration relations and in the background fluorescence were considerably smaller, and so is the uncertainty of the estimated SB concentrations.
Abbreviations: BF, brilliant sulfaflavine CCD, charge-coupled device SB, sulforhodamine B TDR, time domain reflectometry
This article has been cited by other articles:
![]() |
S. E. Oswald, M. Menon, A. Carminati, P. Vontobel, E. Lehmann, and R. Schulin Quantitative Imaging of Infiltration, Root Growth, and Root Water Uptake via Neutron Radiography Vadose Zone J., August 13, 2008; 7(3): 1035 - 1047. [Abstract] [Full Text] [PDF] |
||||
![]() |
A. E. Rosenbom, V. Ernstsen, H. Fluhler, K. H. Jensen, J. C. Refsgaard, and H. Wydler Fluorescence Imaging Applied to Tracer Distributions in Variably Saturated Fractured Clayey Till J. Environ. Qual., March 1, 2008; 37(2): 448 - 458. [Abstract] [Full Text] [PDF] |
||||
![]() |
M. Persson, S. Haridy, J. Olsson, and J. Wendt Solute Transport Dynamics by High-Resolution Dye Tracer Experiments--Image Analysis and Time Moments Vadose Zone J., August 16, 2005; 4(3): 856 - 865. [Abstract] [Full Text] [PDF] |
||||
![]() |
M. Persson Accurate Dye Tracer Concentration Estimations Using Image Analysis Soil Sci. Soc. Am. J., June 2, 2005; 69(4): 967 - 975. [Abstract] [Full Text] [PDF] |
||||
![]() |
T. Gimmi and N. Ursino Mapping Material Distribution in a Heterogeneous Sand Tank by Image Analysis Soil Sci. Soc. Am. J., September 1, 2004; 68(5): 1508 - 1514. [Abstract] [Full Text] [PDF] |
||||
![]() |
J. Vanderborght, P. Gahwiller, and H. Fluhler Identification of Transport Processes in Soil Cores Using Fluorescent Tracers Soil Sci. Soc. Am. J., May 1, 2002; 66(3): 774 - 787. [Abstract] [Full Text] [PDF] |
||||
| HOME | HELP | FEEDBACK | SUBSCRIPTIONS | ARCHIVE | SEARCH | TABLE OF CONTENTS |
| The SCI Journals | Agronomy Journal | Crop Science | |||
| Journal of Natural Resources and Life Sciences Education |
Vadose Zone Journal | ||||
| Journal of Plant Registrations | Journal of Environmental Quality |
The Plant Genome | |||