Abstract

Temporal and spatial resolution of satellite images are coarse and cannot provide the real-time, meter-scale resolution monitoring required in many applications, such as precision agriculture. Since high resolution thermal infrared data provide one means to observe canopy temperature variance, we developed an algorithm (three-temperature model, 3T) to estimate transpiration rate at meter-scale pixels and detected transpiration variation for soybean under different upper irrigation limits: No irrigation, 35% of field capacity (FC), 55% of FC, and 75% of FC, denoted as W0, W1, W2, and W3, respectively. The spatial patterns of the transpiration rate indicated that heterogeneity is common in farmland. Transpiration rates in the wet treatment (i.e., W3) were consistently higher than that in the dry treatment (i.e., W0). Transpiration rates reached peak values at around 12:30–14:30 and most of values showed that W3 > W2 > W1 > W0, with 0.91 mm/h, 0.89 mm/h, 0.79 mm/h, and 0.62 mm/h during the reproductive period, respectively. In general, the transpiration rate of soybean increased with increasing irrigation quantities. With a higher irrigation total, soil water content increased gradually, and then the transpiration rate increased. Although land surface temperature decreased by only 8.57 K (Kelvin), 6.33 K, and 5.47 K, respectively, the transpiration rate increased by 78%, 60%, and 40%, respectively, for the W3, W2, and W1 treatment compared with the W0 treatment. The magnitude of transpiration change is greater than that of canopy temperature, but both parameters are strongly interrelated with each other through a non-linear correlation. Heterogeneity of canopy leaf temperature and transpiration is mainly due to physical and biological interactions. Understanding transpiration rate and canopy temperature heterogeneity under different irrigation treatments can not only help in scheduling irrigation, but also in enhancing water utilization efficiency in irrigated agriculture. The real-time monitoring of crop transpiration at meter-scale is of great importance for large irrigation systems, especially for precision irrigation, and will have great application prospects in the near future.

Highlights

  • Agriculture in water stressed and arid environments is maintained through irrigation

  • According to many other studies [46,47,48,49,50,51,52,53,54], we can conclude that heterogeneity of canopy temperature mainly results from physical and biological interactions, which are affected by climatic conditions, environmental conditions, canopy structure complexity, canopy parameters and ecosystem functions

  • This paper introduced a method (3T model + high resolution thermal infrared remote sensing) to estimate transpiration rates of plants at meter-scale pixels

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Summary

Introduction

Agriculture in water stressed and arid environments is maintained through irrigation. In order to effectively manage water resources in these areas, it is necessary to optimize the use of irrigation water by reducing water losses [1]. Evapotranspiration (ET, soil evaporation (E) + vegetation transpiration (T)) is a critical component in the water cycle and the energy flow between the land surface and Agronomy 2019, 9, 8; doi:10.3390/agronomy9010008 www.mdpi.com/journal/agronomy. Evapotranspiration accounts for approximately 60% of annual land precipitation on a global basis [2] and about 80–90% of consumptive water use for crop production in semi-arid regions [3]. It is essential to estimate how much water is transpired by a crop for better allocation of water resources and improving water-use efficiency in the irrigated agriculture

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