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Characterizing the hysteretic effects of water and salinity stresses on root-water-uptake
Agricultural Water Management ( IF 5.9 ) Pub Date : 2024-10-25 , DOI: 10.1016/j.agwat.2024.109121 Tianshu Wang, Lining Liu, Qiang Zuo, Xun Wu, Yanqi Xu, Jianchu Shi, Jiandong Sheng, Pingan Jiang, Alon Ben-Gal
Agricultural Water Management ( IF 5.9 ) Pub Date : 2024-10-25 , DOI: 10.1016/j.agwat.2024.109121 Tianshu Wang, Lining Liu, Qiang Zuo, Xun Wu, Yanqi Xu, Jianchu Shi, Jiandong Sheng, Pingan Jiang, Alon Ben-Gal
Characterizing the effects of previous water and salinity stresses is critical for the evaluation of plant water status, which, in turn, is essential for understanding soil-plant water relations and optimizing irrigation schemes. Recent research has found that hysteresis of plant response following water stress alone can be described by an exponential function of the stress degree on the previous day. To explore and quantify the effects of hysteresis concerning salinity stress and combined water-salinity stress, a hydroponic experiment and a soil column experiment on winter wheat, and a field experiment on cotton were conducted. Like water stress, previous salinity stress and combined water-salinity stress also resulted in hysteretic effects on root-water-uptake. Leaf stomatal conductance and plant transpiration rate of stressed crops could only recover gradually from a previous stressed status after re-watering. When stress was mild, compensatory recovery was found, while incomplete recovery occurred when stress was severe. Although the recovery process was closely related to stress history and type, a recovery coefficient was quantified universally with an exponential function of the stress extent on the previous day (with a coefficient of determination R 2 ≥ 0.60). Consideration of hysteresis for water and salinity stresses with a mathematical model led to significant improvement in the simulation of both relative transpiration rate (R 2 = 0.94, root mean squared error RMSE = 0.04, maximal absolute error MAE = 0.12) and soil water content (R 2 = 0.90, RMSE = 0.01 cm3 cm–3 , MAE = 0.03 cm3 cm–3 ), especially during the recovery periods severely affected by historical stress. Consideration of hysteresis is expected to benefit regulation of soil water and salinity and thus enhance water use efficiency. However, the mechanisms underlying hysteresis, especially the compensatory recovery mechanisms, still need to be further investigated.
更新日期：2024-10-25
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