Environmental factors and groundwater behavior in an agricultural experimental basin of the Brazilian central plateau

被引:12
|
作者
Salles, Leandro de Almeida [1 ,3 ]
Furquim Werneck Lima, Jorge Enoch [2 ]
Roig, Henrique Llacer [3 ]
Malaquias, Juaci Vitoria [2 ]
机构
[1] Inst Brasilia Ambiental IBRAM, SEPN 511 Bloco C Edificio Bittar, BR-70750543 Brasilia, DF, Brazil
[2] Empresa Brasileira Pesquisa Agr EMBRAPA, Ctr Pesquisa Agr Cerrados CPAC, BR 020,Km 18, BR-08223 Caixa, Brazil
[3] Univ Brasilia, Inst Geociencias, Campus Univ Darcy Ribeiro, BR-70910900 Brasilia, DF, Brazil
关键词
Geostatistics; Statistical modeling; Groundwater recharge/water budget; Geographic information system; GEOGRAPHICALLY WEIGHTED REGRESSION; MANAGEMENT-SYSTEMS; QUALITY INDICATORS; NON-STATIONARITY; WATER-QUALITY; ATTRIBUTES; CERRADO; SEDIMENT; OXISOL; STREAMFLOW;
D O I
10.1016/j.apgeog.2018.02.007
中图分类号
P9 [自然地理学]; K9 [地理];
学科分类号
0705 ; 070501 ;
摘要
Knowledge of groundwater storage in tropical soils of the Cerrado biome is relevant because of its importance for stream flow regime in Brazil's central plateau, where rivers are perennial during the drought period of the year. The purpose of this study was to: (i) identify environmental variables capable of explaining the amplitude of groundwater variation in points of an agricultural basin in the Cerrado; and (ii) develop a statistical model to simulate the amplitude of water table variation from the chosen variables. The study was developed with monthly data obtained from 35 piezometric wells located at the Upper Jardim experimental river basin (105 km(2)), collected between 17/02/2004 and 01/10/2012. Two multivariate analysis methodologies were used: (i) Ordinary Least Squares regression (OLS); and (ii) Geographical Weighted Regression (GWR). Groundwater amplitude in the studied period was correlated with independent variables related to soil's physical properties and related to the basin's geomorphology, where six explanatory variables were selected to compose the statistical model. The results indicate that both OLS and GWR methodologies were capable of establishing correlations between the response and the explanatory variables. However, GWR managed to capture local correlations between the explanatory and the dependent variable that were not obtained by the OLS. Despite the complexity of groundwater behavior in tropical soils, this study demonstrates the possibility to estimate with data collected near the surface, how much water is stored in porous aquifers and groundwater behavior in soils of the Brazilian central plateau, being of great use to unmonitored river basins.
引用
收藏
页码:272 / 281
页数:10
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