Estimating soil water content in a thorny forest ecosystem by time-lapse electrical resistivity tomography (ERT) and HYDRUS 2D/3D simulations

被引:2
|
作者
Faundez Urbina, Carlos A. [1 ]
Alanis, Daniel Cabrera [2 ]
Ramirez, Elizabeth [3 ]
Seguel, Oscar [4 ]
Fustos, Ivo J. [5 ]
Donoso, Pablo Diaz [2 ]
de Miranda, Jarbas Honorio [6 ]
Rakonjac, Nikola [7 ,8 ]
Palma, Sebastian Elgueta [9 ,10 ]
Galleguillos, Mauricio [11 ,12 ]
机构
[1] Pontificia Univ Catolica Valparaiso, Escuela Agron, Fac Ciencias Agron & Alimentos, Calle San Francisco S-N, Quillota, Chile
[2] Aquadetect, Dept Agrogeofis, Curico, Chile
[3] Univ Chile, Fac Ciencias Fis & Matemat, Santiago, Chile
[4] Univ Chile, Fac Ciencias Agron, Santiago, Chile
[5] Univ La Frontera, Fac Ingn & Ciencias, Dept Ingn Obras Civiles, Temuco, Chile
[6] Univ Sao Paulo, Dept Engn Biossistemas LEB, Escola Super Agr Luiz de Queiroz ESALQ USP, Piracicaba, Brazil
[7] Wageningen Univ, Soil Phys & Land Management Grp, Wageningen, Netherlands
[8] Ecole Polytech Fed Lausanne EPFL, Lab Ecohydrol, Lausanne, Switzerland
[9] Univ Amer, Fac Med Vet & Agron, Santiago, Chile
[10] Univ Amer, Nucl Ciencias Ambientales & Alimentarias NCAA, Santiago, Chile
[11] Univ Adolfo Ibanez, Fac Ingn & Ciencias, Penalolen, Chile
[12] Univ Chile, Ctr Climate & Resilience Res CR2, Santiago, Chile
关键词
applied geophysics; HYDRUS; 1D; Vachellia caven; water balance; water transfer models; UNSATURATED HYDRAULIC PARAMETERS; SENSITIVITY-ANALYSIS; DRIP IRRIGATION; CONDUCTIVITY; DYNAMICS; ZONE; MODELS; PATTERNS; SCALES; FLOW;
D O I
10.1002/hyp.15002
中图分类号
TV21 [水资源调查与水利规划];
学科分类号
081501 ;
摘要
Determination of soil volumetric water content theta in forest ecosystems is particularly challenging due to deep rooting systems and unknown soil vertical and spatial heterogeneity. This research aims to test two undisturbed methods, electrical resistivity tomography (ERT) and HYDRUS 2D/3D, for 2D theta determination in a thorny forest ecosystem. The experiment consisted of infiltrating 10 L of water lasting 60 min. During infiltration, ERT measured apparent resistivity by time-lapse measurements, and theta was measured with an FDR probe (EnviroSCAN) at 33, 63, 83, 97, and 163 cm depth close to the infiltration site. At the end of infiltration, a soil pit was dug, and 100 measurements of theta were performed with a TDR in a 10 x 10 cm regular grid. Archie law transformed soil resistivity (ERT) into theta using manual calibration, verified by an independent dataset. The 2D theta profile obtained by ERT was qualitatively compared with the HYDRUS 2D/3D one. HYDRUS 2D/3D was parametrized with calibrated parameters obtained with HYDRUS 1D using 106 days of theta obtained with EnviroSCAN. The results of HYDRUS 1D calibration and verification were satisfactory, with RMSE and Nash-Sutcliffe coefficients ranging from 0.021 to 0.034 cm(3 )cm(-3) and 0.11 to 0.77, respectively. The forward HYDRUS 2D/3D theta simulation disagrees with EnviroSCAN data for 33 cm depth. However, it follows the trend with near to zero variation of water content at 63 cm depth. Water content determination by ERT was satisfactory with RMSE for calibration and verification of 0.017 and 0.021 cm(3) cm(-3). HYDRUS 2D/3D and ERT comparisons were not equal, with a shallower wetting front by ERT and a deeper one for HYDRUS. Still, both wetting fronts agree with the wetting depth estimated by EnviroSCAN. We conclude that both methods are an alternative for theta determination in heterogeneous and deep soils of forest ecosystems.
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页数:17
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