Spatial, Vertical, and Temporal Soil Water Content Variability Affected by Low-Pressure Drip Irrigation in Sandy Loam Soil: A Soil Bin Experimental Study

Drip irrigation pressure is considered a key parameter for controlling and designing the drip irrigation system in sandy soils. Understanding soil water content (SWC) movements under varying pressures can enhance water use efficiency and support sustainable irrigation strategies for crops in arid regions. The objectives of this study were to investigate the effects of irrigation pressure on the spatial, vertical, and temporal variability of SWC in sandy loam soil using surface drip irrigation. Experiments were carried out in a soil bin located in a greenhouse. SWC sensors were placed at depths 10, 20, 30, 40, and 50 cm to monitor SWC variability under low, medium, and high drip irrigation pressures (25, 50, and 75 kPa) at a constant emitter flow rate of 3 L/h. A pressure controller was used to regulate drip irrigation pressure, while microcontrollers communicated with SWC sensors, collected experimental data, and automatically recorded the outputs. At low irrigation pressure, water content began to increase at 0.53 h and saturated at 3.5 h, with both values being significantly lower at medium and high pressures. The results indicated that lower pressures led to significant variability in water movement at shallow depths (10 to 30 cm), becoming uniform at deeper layers but requiring longer irrigation times. Competitively higher pressures showed uniform water distribution and retention statistically throughout the soil profiles with shorter irrigation times. The variation in water distribution resulting in non-uniform coverage across the irrigated area demonstrates how pressure changes affect the flow rate of the emitter. The results provide information maps with soil water data that can be adjusted with irrigation pressure to maximize water use efficiency in sandy loam soils, aiding farmers in better irrigation scheduling for different crops using surface drip irrigation techniques in arid environments.

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Publication Details

Journal
Agronomy
Published
2024-11-28
DOI
https://doi.org/10.3390/agronomy14122848
Citations
4
Primary Topic
Soil Moisture and Remote Sensing
Type
article
Field-Weighted Citation Impact
0.82

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article

Spatial, Vertical, and Temporal Soil Water Content Variability Affected by Low-Pressure Drip Irrigation in Sandy Loam Soil: A Soil Bin Experimental Study

Yuri Jang, Mohammod Ali, Md. Aminur Rahman, Sun‐Ok Chung et al.
4 citations
Agronomy
Soil Moisture and Remote Sensing
0.82
article

Spatial, Vertical, and Temporal Soil Water Content Variability Affected by Low-Pressure Drip Irrigation in Sandy Loam Soil: A Soil Bin Experimental Study

Yuri Jang, Mohammod Ali, Md. Aminur Rahman, Sun‐Ok Chung, Md Asrakul Haque, Hongbin Jin, Md Razob Ali
article en
4 citations

Abstract

Drip irrigation pressure is considered a key parameter for controlling and designing the drip irrigation system in sandy soils. Understanding soil water content (SWC) movements under varying pressures can enhance water use efficiency and support sustainable irrigation strategies for crops in arid regions. The objectives of this study were to investigate the effects of irrigation pressure on the spatial, vertical, and temporal variability of SWC in sandy loam soil using surface drip irrigation. Experiments were carried out in a soil bin located in a greenhouse. SWC sensors were placed at depths 10, 20, 30, 40, and 50 cm to monitor SWC variability under low, medium, and high drip irrigation pressures (25, 50, and 75 kPa) at a constant emitter flow rate of 3 L/h. A pressure controller was used to regulate drip irrigation pressure, while microcontrollers communicated with SWC sensors, collected experimental data, and automatically recorded the outputs. At low irrigation pressure, water content began to increase at 0.53 h and saturated at 3.5 h, with both values being significantly lower at medium and high pressures. The results indicated that lower pressures led to significant variability in water movement at shallow depths (10 to 30 cm), becoming uniform at deeper layers but requiring longer irrigation times. Competitively higher pressures showed uniform water distribution and retention statistically throughout the soil profiles with shorter irrigation times. The variation in water distribution resulting in non-uniform coverage across the irrigated area demonstrates how pressure changes affect the flow rate of the emitter. The results provide information maps with soil water data that can be adjusted with irrigation pressure to maximize water use efficiency in sandy loam soils, aiding farmers in better irrigation scheduling for different crops using surface drip irrigation techniques in arid environments.

AgronomyVol. 14(12)
Chungnam National University (KR)
Ministry of Agriculture, Food and Rural Affairs, Korea Institute of Planning and Evaluation for Technology in Food, Agriculture and Forestry
Openalex Percentile: Top 29%
Soil Moisture and Remote Sensing
0.82
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