|
|
||||||||
a Departement of Environmental Sciences and Land Use Planning, Université catholique de Louvain-la-Neuve (UCL), Louvain-la-Neuve, Belgium
b HortResearch, PB 11030, Palmerston North, New Zealand
c Battelle, Pacific Northwest Division, USA
* Corresponding author (vandervelde{at}geru.ucl.ac.be)
Root zone drainage measurements are needed to improve fertilizer management in areas where agriculture may be impacting groundwater supplies. We present results of field tests where drainage was measured with two types of suction (resolution of 0.16 and 1.6 mm tip1) and a nonsuction (resolution of 0.22 mm tip1) water flux meter (WFM). The soil was a microstructured weathered volcanic ash located on a coral atoll subject to intense rainfall and located in the Kingdom of Tonga. Our objectives were to evaluate water flux measurements by comparing them with (i) simple water balance estimates of cumulative fluxes, (ii) cumulative fluxes deduced from soil moisture content changes, and (iii) simulated fluxes using HYDRUS-1D. Soil hydraulic properties were obtained at five soil depths. During the 60-d evaluation period rainfall totaled 340 mm. The WFMs were installed in duplicate using disturbed soil. The consistency of the shape of the drainage curves measured with the WFMs, those derived from soil moisture changes, and those obtained with modeling led us to conclude that soil disturbance during WFM installation did not severely influence measurements. This was attributed to the strong microaggregation and disturbance introduced by plowing. Water balance and HYDRUS model estimates of drainage corresponded well with the measurement by nonsuction WFMs. Suction WFMs overestimated drainage, possibly due to flow convergence created by wick and divergence barrier lengths being not properly sized for the observed flow conditions. After the evaluation period some of the WFMs failed to respond. Nevertheless, flux meters are seen as promising tools to provide remote and continuous measurement of root zone drainage.
Abbreviations: C-WFM, capacitance water flux meter DOY, day of year ET0, reference crop evapotranspiration SMC, soil moisture content T-WFM, tipping bucket water flux meter WFM, water flux meter Z-WFM, nonsuction WFM with zero tension
This article has been cited by other articles:
![]() |
J. Sansoulet, Y.-M. Cabidoche, P. Cattan, S. Ruy, and J. Simunek Spatially Distributed Water Fluxes in an Andisol under Banana Plants: Experiments and Three-Dimensional Modeling Vadose Zone J., May 27, 2008; 7(2): 819 - 829. [Abstract] [Full Text] [PDF] |
||||
![]() |
J. Mertens, V. Tuts, J. Diels, J. Vanderborght, J. Feyen, and R. Merckx Design and Testing of a Drop Counter for Use in Vadose Zone Water Samplers Vadose Zone J., April 14, 2008; 7(2): 434 - 438. [Abstract] [Full Text] [PDF] |
||||
![]() |
J. Mertens, J. Diels, J. Feyen, and J. Vanderborght Numerical Analysis of Passive Capillary Wick Samplers prior to Field Installation Soil Sci. Soc. Am. J., January 1, 2007; 71(1): 35 - 42. [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 |
Soil Science Society of America Journal | ||||
| Journal of Plant Registrations | Journal of Environmental Quality |
The Plant Genome | |||