Saturated Hydraulic Conductivity of Nine Soils According to Water Quality, Soil Texture, and Clay Mineralogy
Water quality affects soils by promoting their degradation by the accumulation of salts that will lead to salinization and sodification. However, the magnitude of these processes varies with soil attributes. Saturated hydraulic conductivity (K<sub>sat</sub>) is the rate at which water pa...
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2025-03-01
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| author | Clarissa Buarque Vieira Gabriel Henrique Maximo Clarindo Silva Brivaldo Gomes de Almeida Luiz Guilherme Medeiros Pessoa Fernando José Freire Valdomiro Severino de Souza Junior Hidelblandi Farias de Melo Luara Gabriella Gomes de Lima Rodrigo Francisco do Nascimento Paiva Jorge Freire da Silva Ferreira Maria Betânia Galvão dos Santos Freire |
| author_facet | Clarissa Buarque Vieira Gabriel Henrique Maximo Clarindo Silva Brivaldo Gomes de Almeida Luiz Guilherme Medeiros Pessoa Fernando José Freire Valdomiro Severino de Souza Junior Hidelblandi Farias de Melo Luara Gabriella Gomes de Lima Rodrigo Francisco do Nascimento Paiva Jorge Freire da Silva Ferreira Maria Betânia Galvão dos Santos Freire |
| author_sort | Clarissa Buarque Vieira |
| collection | DOAJ |
| description | Water quality affects soils by promoting their degradation by the accumulation of salts that will lead to salinization and sodification. However, the magnitude of these processes varies with soil attributes. Saturated hydraulic conductivity (K<sub>sat</sub>) is the rate at which water passes through saturated soil, which is fundamental to determining water movement through the soil profile. The K<sub>sat</sub> may differ from soil to soil according to the sodium adsorption ratio (SAR), water electrical conductivity (EC<sub>w</sub>), soil texture, and clay mineralogical assemblage. In this study, an experiment with vertical columns and constant-load permeameters was conducted to evaluate changes in soil K<sub>sat</sub> with waters comprising five EC<sub>w</sub> values (128, 718, 1709, 2865, and 4671 µS cm<sup>−1</sup>) and five SAR values [0, 5, 12, 20, and 30 (mmol<sub>c</sub> L<sup>−1</sup>)<sup>0.5</sup>] in combination. Horizons from nine northeastern Brazilian soils (ranging from tropical to semiarid) were selected according to their texture and clay mineralogical composition. The data obtained were fit with multiple regression equations for K<sub>sat</sub> as a function of EC<sub>w</sub> and SAR. This study also determined the null SAR at each EC<sub>w</sub> level, using K<sub>sat</sub> = 0 on each equation, to predict the SAR needed to achieve zero drainage on each soil for each EC<sub>w</sub> level and the threshold electrolyte concentration (C<sub>TH</sub>) that would lead to a 20% reduction of maximum K<sub>sat</sub>. Neither the EC<sub>w</sub> nor SAR of the applied waters affected the K<sub>sat</sub> of soils with a mineralogical assemblage of oxides and kaolinite such as Ferralsol, Nitisol, and Lixisol, with an average K<sub>sat</sub> of 2.75, 6.06, and 3.33 cm h<sup>−1</sup>, respectively. In smectite- and illite-rich soils, the K<sub>sat</sub> increased with higher EC<sub>w</sub> levels and decreased with higher SAR levels, especially comparing the soil’s estimated K<sub>sat</sub> for water with low EC<sub>w</sub> and high SAR in combination (EC<sub>w</sub> of 128 µS cm<sup>−1</sup> and SAR 30) and water with high EC<sub>w</sub> and low SAR in combination (EC<sub>w</sub> of 4671 µS cm<sup>−1</sup> and SAR 0) such as Regosol (4.95 to 10.94 cm h<sup>−1</sup>); Vertisol (0.28 to 2.04 cm h<sup>−1</sup>); Planosol (0 to 0.29 cm h<sup>−1</sup>); Luvisol (0.46 to 2.12 cm h<sup>−1</sup>); Cambisol (0 to 0.23 cm h<sup>−1</sup>); and Fluvisol (1.87 to 3.34 cm h<sup>−1</sup>). The C<sub>TH</sub> was easily reached in soils with high concentrations of highly active clays such as smectites. In sandy soils, the target C<sub>TH</sub> was only reached under extremely high SAR values, indicating a greater resistance of these soils to salinization/sodification. Due to their mineralogical assemblage, soils from tropical sub-humid/hot and semiarid climates were more affected by treatments than soils from tropical humid/hot climates, indicating serious risks of physical and chemical degradation. The results showed the importance of monitoring water quality for irrigation, mainly in less weathered, more clayey soils, with high clay activity to minimize the rate of salt accumulation in soils of the Brazilian semiarid region. Our study also proved that clay mineralogy had more influence on the K<sub>sat</sub> than clay concentration, mainly in soils irrigated with saline and sodic waters, and that soils with highly active smectite are more prone to degradation than soils with high concentrations of kaolinite. |
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| spelling | doaj-art-2b7f919b47ae4d33b10b5d126ef9c07c2025-08-20T02:24:42ZengMDPI AGAgronomy2073-43952025-03-0115486410.3390/agronomy15040864Saturated Hydraulic Conductivity of Nine Soils According to Water Quality, Soil Texture, and Clay MineralogyClarissa Buarque Vieira0Gabriel Henrique Maximo Clarindo Silva1Brivaldo Gomes de Almeida2Luiz Guilherme Medeiros Pessoa3Fernando José Freire4Valdomiro Severino de Souza Junior5Hidelblandi Farias de Melo6Luara Gabriella Gomes de Lima7Rodrigo Francisco do Nascimento Paiva8Jorge Freire da Silva Ferreira9Maria Betânia Galvão dos Santos Freire10Agronomy Department, Federal Rural University of Pernambuco, Recife 52171-900, Pernambuco, BrazilAgronomy Department, Federal Rural University of Pernambuco, Recife 52171-900, Pernambuco, BrazilAgronomy Department, Federal Rural University of Pernambuco, Recife 52171-900, Pernambuco, BrazilGraduate Program in Crop Production, Federal Rural University of Pernambuco, Serra Talhada 56909-535, Pernambuco, BrazilAgronomy Department, Federal Rural University of Pernambuco, Recife 52171-900, Pernambuco, BrazilAgronomy Department, Federal Rural University of Pernambuco, Recife 52171-900, Pernambuco, BrazilSoil Department, Federal University of Viçosa, Viçosa 36570-900, Minas Gerais, BrazilAgronomy Department, Federal Rural University of Pernambuco, Recife 52171-900, Pernambuco, BrazilAgronomy Department, Federal Rural University of Pernambuco, Recife 52171-900, Pernambuco, BrazilUS Salinity Laboratory (USDA-ARS), Riverside, CA 92507, USAAgronomy Department, Federal Rural University of Pernambuco, Recife 52171-900, Pernambuco, BrazilWater quality affects soils by promoting their degradation by the accumulation of salts that will lead to salinization and sodification. However, the magnitude of these processes varies with soil attributes. Saturated hydraulic conductivity (K<sub>sat</sub>) is the rate at which water passes through saturated soil, which is fundamental to determining water movement through the soil profile. The K<sub>sat</sub> may differ from soil to soil according to the sodium adsorption ratio (SAR), water electrical conductivity (EC<sub>w</sub>), soil texture, and clay mineralogical assemblage. In this study, an experiment with vertical columns and constant-load permeameters was conducted to evaluate changes in soil K<sub>sat</sub> with waters comprising five EC<sub>w</sub> values (128, 718, 1709, 2865, and 4671 µS cm<sup>−1</sup>) and five SAR values [0, 5, 12, 20, and 30 (mmol<sub>c</sub> L<sup>−1</sup>)<sup>0.5</sup>] in combination. Horizons from nine northeastern Brazilian soils (ranging from tropical to semiarid) were selected according to their texture and clay mineralogical composition. The data obtained were fit with multiple regression equations for K<sub>sat</sub> as a function of EC<sub>w</sub> and SAR. This study also determined the null SAR at each EC<sub>w</sub> level, using K<sub>sat</sub> = 0 on each equation, to predict the SAR needed to achieve zero drainage on each soil for each EC<sub>w</sub> level and the threshold electrolyte concentration (C<sub>TH</sub>) that would lead to a 20% reduction of maximum K<sub>sat</sub>. Neither the EC<sub>w</sub> nor SAR of the applied waters affected the K<sub>sat</sub> of soils with a mineralogical assemblage of oxides and kaolinite such as Ferralsol, Nitisol, and Lixisol, with an average K<sub>sat</sub> of 2.75, 6.06, and 3.33 cm h<sup>−1</sup>, respectively. In smectite- and illite-rich soils, the K<sub>sat</sub> increased with higher EC<sub>w</sub> levels and decreased with higher SAR levels, especially comparing the soil’s estimated K<sub>sat</sub> for water with low EC<sub>w</sub> and high SAR in combination (EC<sub>w</sub> of 128 µS cm<sup>−1</sup> and SAR 30) and water with high EC<sub>w</sub> and low SAR in combination (EC<sub>w</sub> of 4671 µS cm<sup>−1</sup> and SAR 0) such as Regosol (4.95 to 10.94 cm h<sup>−1</sup>); Vertisol (0.28 to 2.04 cm h<sup>−1</sup>); Planosol (0 to 0.29 cm h<sup>−1</sup>); Luvisol (0.46 to 2.12 cm h<sup>−1</sup>); Cambisol (0 to 0.23 cm h<sup>−1</sup>); and Fluvisol (1.87 to 3.34 cm h<sup>−1</sup>). The C<sub>TH</sub> was easily reached in soils with high concentrations of highly active clays such as smectites. In sandy soils, the target C<sub>TH</sub> was only reached under extremely high SAR values, indicating a greater resistance of these soils to salinization/sodification. Due to their mineralogical assemblage, soils from tropical sub-humid/hot and semiarid climates were more affected by treatments than soils from tropical humid/hot climates, indicating serious risks of physical and chemical degradation. The results showed the importance of monitoring water quality for irrigation, mainly in less weathered, more clayey soils, with high clay activity to minimize the rate of salt accumulation in soils of the Brazilian semiarid region. Our study also proved that clay mineralogy had more influence on the K<sub>sat</sub> than clay concentration, mainly in soils irrigated with saline and sodic waters, and that soils with highly active smectite are more prone to degradation than soils with high concentrations of kaolinite.https://www.mdpi.com/2073-4395/15/4/864salinitysodicitythreshold electrolyte concentrationgranulometric compositionmineralogical assemblage |
| spellingShingle | Clarissa Buarque Vieira Gabriel Henrique Maximo Clarindo Silva Brivaldo Gomes de Almeida Luiz Guilherme Medeiros Pessoa Fernando José Freire Valdomiro Severino de Souza Junior Hidelblandi Farias de Melo Luara Gabriella Gomes de Lima Rodrigo Francisco do Nascimento Paiva Jorge Freire da Silva Ferreira Maria Betânia Galvão dos Santos Freire Saturated Hydraulic Conductivity of Nine Soils According to Water Quality, Soil Texture, and Clay Mineralogy Agronomy salinity sodicity threshold electrolyte concentration granulometric composition mineralogical assemblage |
| title | Saturated Hydraulic Conductivity of Nine Soils According to Water Quality, Soil Texture, and Clay Mineralogy |
| title_full | Saturated Hydraulic Conductivity of Nine Soils According to Water Quality, Soil Texture, and Clay Mineralogy |
| title_fullStr | Saturated Hydraulic Conductivity of Nine Soils According to Water Quality, Soil Texture, and Clay Mineralogy |
| title_full_unstemmed | Saturated Hydraulic Conductivity of Nine Soils According to Water Quality, Soil Texture, and Clay Mineralogy |
| title_short | Saturated Hydraulic Conductivity of Nine Soils According to Water Quality, Soil Texture, and Clay Mineralogy |
| title_sort | saturated hydraulic conductivity of nine soils according to water quality soil texture and clay mineralogy |
| topic | salinity sodicity threshold electrolyte concentration granulometric composition mineralogical assemblage |
| url | https://www.mdpi.com/2073-4395/15/4/864 |
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