TY - JOUR
T1 - Drip irrigation improves spring wheat water productivity by reducing leaf area while increasing yield
AU - Yang, Danni
AU - Li, Sien
AU - Wu, Mousong
AU - Yang, Hanbo
AU - Zhang, Wenxin
AU - Chen, Ji
AU - Wang, Chunyu
AU - Huang, Siyu
AU - Zhang, Ruoqing
AU - Zhang, Yunxuan
N1 - CENPERM[2023]
PY - 2023
Y1 - 2023
N2 - To mitigate the climate change-induced water shortage and realize the sustainable development of agriculture, drip irrigation, a more efficient water-saving irrigation method, has been intensively implemented in most arid agricultural regions in the world. However, compared to traditional border irrigation, how drip irrigation affects the biophysical conditions in the cropland and how crops physiologically respond to changes in biophysical conditions in terms of water, heat and carbon exchange remain largely unknown. In view of the above situation, to reveal the mechanism of drip irrigation in improving spring wheat water productivity, paired field experi-ments based on drip irrigation and border irrigation were conducted to extensively monitor water and heat fluxes at a typical spring wheat field (Triticum aestivum L.) in Northwest China during 2017-2020. The results showed that drip irrigation improved yield by 10.3 % and crop water productivity (i.e., yield-to-evapotranspiration-ratio) by 15.6 %, but reduced LAI by 16.9 % in contrast with border irrigation. Under drip irrigation, the lateral development of spring wheat roots was promoted by higher soil temperature combined with frequent dry-wet alternation in the shallow soil layer (0-20 cm), which was the basis for efficient absorption of water and fer-tilizer, as well as efficient formation of photosynthate. Meanwhile, drip irrigation increased net radiation and decreased latent heat flux by inhibiting leaf growth, thereby increased sensible heat, causing a higher soil temperature (+1.10 degrees C) and canopy temperature (+1.11 degrees C). Further analysis proved that soil temperature was the key factor affecting yield formation. Based on the above conditions, the decrease in leaf distribution coef-ficient (-0.030) led to the decrease in evapotranspiration (-5.7 %) and the increase in ear distribution coeffi-cient (+0.029). Therefore, drip irrigation emphasized the role of soil moisture in the soil-plant-atmosphere continuum, enhanced crop activity by increasing field temperature, especially soil temperature, and finally improved yield and water productivity via carbon reallocation. The study revealed the mechanism of drip irri-gation for improving spring wheat yield, and would contribute to improving Earth system models in representing agricultural cropland ecosystems with drip irrigation and predicting the subsequent biophysical and biogeo-chemical feedbacks to climate change.
AB - To mitigate the climate change-induced water shortage and realize the sustainable development of agriculture, drip irrigation, a more efficient water-saving irrigation method, has been intensively implemented in most arid agricultural regions in the world. However, compared to traditional border irrigation, how drip irrigation affects the biophysical conditions in the cropland and how crops physiologically respond to changes in biophysical conditions in terms of water, heat and carbon exchange remain largely unknown. In view of the above situation, to reveal the mechanism of drip irrigation in improving spring wheat water productivity, paired field experi-ments based on drip irrigation and border irrigation were conducted to extensively monitor water and heat fluxes at a typical spring wheat field (Triticum aestivum L.) in Northwest China during 2017-2020. The results showed that drip irrigation improved yield by 10.3 % and crop water productivity (i.e., yield-to-evapotranspiration-ratio) by 15.6 %, but reduced LAI by 16.9 % in contrast with border irrigation. Under drip irrigation, the lateral development of spring wheat roots was promoted by higher soil temperature combined with frequent dry-wet alternation in the shallow soil layer (0-20 cm), which was the basis for efficient absorption of water and fer-tilizer, as well as efficient formation of photosynthate. Meanwhile, drip irrigation increased net radiation and decreased latent heat flux by inhibiting leaf growth, thereby increased sensible heat, causing a higher soil temperature (+1.10 degrees C) and canopy temperature (+1.11 degrees C). Further analysis proved that soil temperature was the key factor affecting yield formation. Based on the above conditions, the decrease in leaf distribution coef-ficient (-0.030) led to the decrease in evapotranspiration (-5.7 %) and the increase in ear distribution coeffi-cient (+0.029). Therefore, drip irrigation emphasized the role of soil moisture in the soil-plant-atmosphere continuum, enhanced crop activity by increasing field temperature, especially soil temperature, and finally improved yield and water productivity via carbon reallocation. The study revealed the mechanism of drip irri-gation for improving spring wheat yield, and would contribute to improving Earth system models in representing agricultural cropland ecosystems with drip irrigation and predicting the subsequent biophysical and biogeo-chemical feedbacks to climate change.
KW - Drip irrigation
KW - Energy balance
KW - Root water uptake
KW - Carbon allocation
KW - Water productivity
KW - CLIMATE-CHANGE IMPACTS
KW - USE EFFICIENCY
KW - WINTER-WHEAT
KW - DEFICIT IRRIGATION
KW - SOIL-MOISTURE
KW - GRAIN-YIELD
KW - ROOT-GROWTH
KW - AGRICULTURE
KW - MANAGEMENT
KW - RATIO
U2 - 10.1016/j.eja.2022.126710
DO - 10.1016/j.eja.2022.126710
M3 - Journal article
VL - 143
JO - European Journal of Agronomy
JF - European Journal of Agronomy
SN - 1161-0301
M1 - 126710
ER -