2023
DOI: 10.3390/su15097456
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Water Dynamics and Hydraulic Functions in Sandy Soils: Limitations to Sugarcane Cultivation in Southern Brazil

Abstract: Crop cultivation on sandy soils is susceptible to water stress. Therefore, we determined the physical-hydric attributes of a Latossolo Vermelho distrófico (Oxisol) in northwestern Paraná state, Brazil. Soil samples were collected at depth ranges of 0 to 0.2 m, 0.2 to 0.4 m, and 0.4 to 0.6 m. We measured clay, silt, sand, fine and coarse sand contents, soil particle density, soil bulk density, total porosity, microporosity, and macroporosity. We also measured soil characteristics such as saturated and unsaturat… Show more

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Cited by 6 publications
(2 citation statements)
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References 51 publications
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“…The greater total porosity at the 0-20 cm soil depth layer can be justified due to the greater macroporosity of the surface layer, which allows better water storage and, therefore, greater total porosity [110][111][112]. This variable is the sum of macroporosity and microporosity and represents soil voids that can store water and air [113][114][115].…”
Section: Sugarcane Irrigation With Tse and Srw Improves Soil Physical...mentioning
confidence: 99%
“…The greater total porosity at the 0-20 cm soil depth layer can be justified due to the greater macroporosity of the surface layer, which allows better water storage and, therefore, greater total porosity [110][111][112]. This variable is the sum of macroporosity and microporosity and represents soil voids that can store water and air [113][114][115].…”
Section: Sugarcane Irrigation With Tse and Srw Improves Soil Physical...mentioning
confidence: 99%
“…Another example of tradeoffs in agricultural specialization is sugarcane production in southeastern Brazil. Brazil is the world's largest sugarcane producer but sandy soils in this major production area limit crop yields due to the lower water holding capacity of these soils [3].…”
mentioning
confidence: 99%