https://www.selleckchem.com/products/e6446.html
The difference between probe derived and theoretical pore water velocity using natural tracers such as electrical conductivity and temperature was -4.9% and 5.2% for downward flow and 1.1% and 14.2% for upward flow, respectively. The difference porosity values calculated from mass and volume packed in the soil column and probe measure porosity ranged between -3.2% to 1.5%. Also, the calculated hydraulic conductivity differed from probe derived values by -8.9%. This article is protected by copyright. All rights reserved. This article is pr
Gefällt mir
Kommentar
Teilen
