scholarly journals Pre- and Post-Irrigation Mapping of Soil Salinity with Electromagnetic Induction Techniques and Relationships with Drainage Water Salinity

2011 ◽  
Vol 75 (1) ◽  
pp. 207-215 ◽  
Author(s):  
V. Urdanoz ◽  
R. Aragüés
Keyword(s):  
Soil Salinity ◽  
Electromagnetic Induction ◽  
Drainage Water ◽  
Water Salinity

Reuse of Drainage Water for Irrigation: Results of Imperial Valley Study: II. Soil Salinity and Water Balance

Hilgardia ◽  
1988 ◽  
Vol 56 (5) ◽  
pp. 17-44 ◽  
Author(s):  
James D. Rhoades ◽  
Frank T. Bingham ◽  
John Letey ◽  
Paul J. Pinter ◽  
Robert D. Lemert ◽  
...  
Keyword(s):  
Water Balance ◽  
Soil Salinity ◽  
Drainage Water ◽  
Imperial Valley

A simple numerical model to estimate water availability in saline soils

Soil Research ◽  
2018 ◽  
Vol 56 (3) ◽  
pp. 264 ◽  
Author(s):  
Mohammad Hossein Mohammadi ◽  
Mahnaz Khataar
Keyword(s):  
Numerical Model ◽  
Water Content ◽  
Soil Water ◽  
Water Uptake ◽  
Soil Salinity ◽  
Irrigation Water ◽  
Weighting Function ◽  
Water Salinity ◽  
Irrigation Water Salinity ◽  
Evapotranspiration Rate

We developed a numerical model to predict soil salinity from knowledge of evapotranspiration rate, crop salt tolerance, irrigation water salinity, and soil hydraulic properties. Using the model, we introduced a new weighting function to express the limitation imposed by salinity on plant available water estimated by the integral water capacity concept. Lower and critical limits of soil water uptake by plants were also defined. We further analysed the sensitivity of model results to underlying parameters using characteristics given for corn, cowpea, and barley in the literature and two clay and sandy loam soils obtained from databases. Results showed that, between two irrigation events, soil salinity increased nonlinearly with decreasing soil water content especially when evapotranspiration and soil drainage rate were high. The salinity weighting function depended greatly on the plant sensitivity to salinity and irrigation water salinity. This research confirmed that both critical and lower limits (in terms of water content) of soil water uptake by plants increased with evapotranspiration rate and irrigation water salinity. Since the presented approach is based on a physical concept and well-known plant parameters, soil hydraulic characteristics, irrigation water salinity, and meteorological conditions, it may be useful in spatio-temporal modelling of soil water quality and quantity and prediction of crop yield.

scholarly journals Salt Tolerance and Na Allocation in Sorghum bicolor under Variable Soil and Water Salinity

Plants ◽  
2020 ◽  
Vol 9 (5) ◽  
pp. 561 ◽  
Author(s):  
Roberta Calone ◽  
Rabab Sanoubar ◽  
Carla Lambertini ◽  
Maria Speranza ◽  
Livia Vittori Antisari ◽  
...  
Keyword(s):  
Salt Tolerance ◽  
Plant Growth ◽  
Sorghum Bicolor ◽  
Soil Salinity ◽  
Ion Homeostasis ◽  
Dry Weight ◽  
Water Salinity ◽  
Selective Absorption ◽  
Salt Leaching ◽  
Sensitive Organ

Salinity is a major constraint for plant growth in world areas exposed to salinization. Sorghum bicolor (L.) Moench is a species that has received attention for biomass production in saline areas thanks to drought and salinity tolerance. To improve the knowledge in the mechanisms of salt tolerance and sodium allocation to plant organs, a pot experiment was set up. The experimental design combined three levels of soil salinity (0, 3, and 6 dS m−1) with three levels of water salinity (0, 2–4, and 4–8 dS m−1) and two water regimes: no salt leaching (No SL) and salt leaching (SL). This latter regime was carried out with the same three water salinity levels and resulted in average +81% water supply. High soil salinity associated with high water salinity (HSS-HWS) affected plant growth and final dry weight (DW) to a greater extent in No SL (−87% DW) than SL (−42% DW). Additionally, HSS-HWS determined a stronger decrease in leaf water potential and relative water content under No SL than SL. HSS-HWS with No SL resulted in a higher Na bioaccumulation from soil to plant and in translocation from roots to stem and, finally, leaves, which are the most sensitive organ. Higher water availability (SL), although determining higher salt input when associated with HWS, limited Na bioaccumulation, prevented Na translocation to leaves, and enhanced selective absorption of Ca vs. Na. At plant level, higher Na accumulation was associated with lower Ca and Mg accumulation, especially in No SL. This indicates altered ion homeostasis and cation unbalance.

Soil Salinity Assessment by Electromagnetic Induction of Irrigated Land

1992 ◽  
Vol 56 (6) ◽  
pp. 1933-1941 ◽  
Author(s):  
J. M. H. Hendrickx ◽  
B. Baerends ◽  
Z. I. Raza ◽  
M. Sadig ◽  
M. Akram Chaudhry
Keyword(s):  
Soil Salinity ◽  
Electromagnetic Induction
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