plant transpirations การใช้

Stable isotopes of water are also used in partitioning water sources for plant transpiration and groundwater recharge.
Irrigation water enters the atmosphere through evaporation and plant transpiration, and then falls as rain over the downwind Midwest.
When a soil becomes too dry, plant transpiration drops because the water is increasingly bound to the soil particles by suction.
Recent global studies using water stable isotopes show that not all soil moisture is equally available for groundwater recharge or for plant transpiration.
Pulses of low level moisture are transported primarily from the Gulf of California and eastern plant transpiration can add additional moisture to the atmosphere which will then flow into Arizona.