Losses of water stop when the film of water around soil particles reaches 0.0002 mm. Water held from the surface of the soil particles to 0.0002 mm is essentially immobile and can only be completely removed with high temperatures (greater than 100 degrees Celsius).
(Losses of water; stop; T:when the film of water around soil particles reaches 0.0002 mm) (the film of water around soil particles; reaches; 0.0002 mm. Water held from the surface of the soil particles to 0.0002 mm is essentially immobile and can only be completely removed with high temperatures (greater than 100 degrees Celsius)) (0.0002 mm; held; from the surface of the soil particles) Context(0.0002 mm held,List([74, 95))):(to 0.0002 mm; is; essentially immobile)
0.0002 mm held,List([74, 95))
Losses of water the film of water around soil particles 0.0002 mm to 0.0002 mm
stop reaches held is
T:when the film of water around soil particles reaches 0.0002 mm
0.0002 mm. Water held from the surface of the soil particles to 0.0002 mm is essentially immobile and can only be completely removed with high temperatures (greater than 100 degrees Celsius)
from the surface of the soil particles
essentially immobile