Abstract

Evaluating the impacts of warming on water balance components in the groundwater–soil–plant–atmosphere continuum (GSPAC) and crop growth are crucial for assessing the risk of water resources and food security under future global warming. A water transformation dynamical processes experimental device (WTDPED) was developed using a chamber coupled with a weighing lysimeter and groundwater supply system, which could simultaneously control both climatic and ground-water level conditions and accurately monitor water fluxes in the GSPAC. Two experiments with maize under increased temperature by 2 °C (T-warm) and ambient temperature (T-control) scenarios were conducted via the WTDPED. The duration of growing season decreased from 125 days under T-control to 117 days under 2 °C warming. There was little difference of total evapotranspiration (ET) (332.6 mm vs. 332.5 mm), soil water storage change (∆W) (−119.0 mm vs. −119.0 mm), drainage (D) (−13.6 mm vs. −13.5 mm) between T-control and T-warm experiments. The average daily ET for maize significantly increased by approximately 6.7% (p < 0.05) in the T-warm experiment, especially during the sixth leaf to tasseling—silking stage with an increase of 0.36 mm with respect to the T-control experiment. There were evident decreases in LAI (leaf area index), whereas non-significant decreases in mean stem diameter, crop height and leaf chlorophyll content under T-warm compared to T-control experiment. However, the chlorophyll content increased by 12% during the sixth leaf to tasseling–silking stage under 2 °C warming, which accelerated the photosynthesis and transpiration rate. The grain yield and water-use efficiency (WUE) for maize increased by 11.0% and 11.1% in the T-warm experiment, respectively, especially due to enhanced growth during the sixth leaf to tasseling–silking stage. This study provided important references for agricultural planting and water management to adapt to a warming environment.

Highlights

  • Climate change, especially warming, has substantial effects on the agricultural water cycle and crop yield [1,2]

  • Our results indicated that the responses of water balance and crop growth during the whole growing season for maize to warming were complicated

  • The water transformation dynamical processes experimental device (WTDPED) device comprising a chamber, weighing lysimeters and groundwater supply system was applied to quantify the responses of water fluxes at different groundwater–soil– plant–atmosphere continuum (GSPAC) interfaces and crop development at 2 ◦ C warming for maize

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Summary

Introduction

Especially warming, has substantial effects on the agricultural water cycle and crop yield [1,2]. Global warming accelerates the hydrological cycle, including changes in the. Water 2018, 10, 1660 precipitation, evapotranspiration (ET), soil water depletion as well as drainage in the groundwater–soil–. Increasing temperature alters the crop development including the duration of the potential growing season, length of maturation time and crop yield [7,8]. The alternation of ET and yield due to global warming can result in large variability of water-use efficiency (WUE) [9,10]. Global mean surface temperature will rise by about 2 ◦ C for Representative Concentration Pathway (RCP) 8.5 (high confidence) by the mid-21st century relative to the 1986–2005 period [11].

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