Abstract

Cultivation of highly salt-tolerant plants (i.e., halophytes), may provide a viable alternative to increase productivity compared to conventional salt-sensitive crops, increasing the economic potential of salt-affected lands that comprise ~20% of irrigated lands worldwide. In this study the Agricultural Policy/Environmental eXtender (APEX) model was adapted to simulate growth of the halophyte quinoa, along with salt dynamics in the plant-soil-water system. Model modifications included salt uptake and salt stress functions formulated using greenhouse data. Data from a field site were used to further parameterize and calibrate the model. Initial simulation results were promising, but differences between simulated and observed soil salinity and plant salt values during the growing season in the calibration suggest that additional improvements to salt uptake and soil salinity algorithms are needed. To demonstrate utility of the modified APEX model, six scenarios were run to estimate quinoa biomass production and soil salinity with different irrigation managements and salinities. Simulated annual biomass was sensitive to soil moisture, and root zone salinity increased in all scenarios. Further experiments are needed to improve understanding of crop salt uptake dynamics and stress sensitivities so that future model updates and simulations better represent salt dynamics in plants and soils in agricultural settings.

Highlights

  • Soil salinity is a major problem in-arid regions where evapotranspiration (ET) exceeds precipitation

  • This flattening caused salt stress to be less sensitive to soil salinity as it deviated from the optimal value defined by STX2

  • This study was an initial attempt at using Agricultural Policy/Environmental eXtender (APEX), a comprehensive watershed model, to simulate halophyte production alongside salt dynamics in the plant-soil-water system

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Summary

Introduction

Soil salinity is a major problem in (semi)-arid regions where evapotranspiration (ET) exceeds precipitation. Salinity negatively impacts crop productivity in nearly 20% of irrigated agricultural lands worldwide [1]. This percentage is expected to grow with increasing desertification, endangering the ability to provide enough food for growing human populations, especially in areas where food supplies are already scarce. Natural processes contribute to soil salinization, and management activities including irrigation with saline water can exacerbate this problem. Salinity can damage plants through reductions in osmotic potential and accumulation of toxic ions in plant tissue [2]. Soils with salinities greater than 4 dS/m are considered saline [4]

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