ARS Home : USDA ARS · face. The flow is expressed using Darcy's law while making three main...
14
Transcript of ARS Home : USDA ARS · face. The flow is expressed using Darcy's law while making three main...
![Page 1: ARS Home : USDA ARS · face. The flow is expressed using Darcy's law while making three main assumptions: (1) the local hydraulic gradient is constant in time and equal to the local](https://reader034.fdocuments.net/reader034/viewer/2022042805/5f61fe1e642cc778cc3413ca/html5/thumbnails/1.jpg)
![Page 2: ARS Home : USDA ARS · face. The flow is expressed using Darcy's law while making three main assumptions: (1) the local hydraulic gradient is constant in time and equal to the local](https://reader034.fdocuments.net/reader034/viewer/2022042805/5f61fe1e642cc778cc3413ca/html5/thumbnails/2.jpg)
![Page 3: ARS Home : USDA ARS · face. The flow is expressed using Darcy's law while making three main assumptions: (1) the local hydraulic gradient is constant in time and equal to the local](https://reader034.fdocuments.net/reader034/viewer/2022042805/5f61fe1e642cc778cc3413ca/html5/thumbnails/3.jpg)
![Page 4: ARS Home : USDA ARS · face. The flow is expressed using Darcy's law while making three main assumptions: (1) the local hydraulic gradient is constant in time and equal to the local](https://reader034.fdocuments.net/reader034/viewer/2022042805/5f61fe1e642cc778cc3413ca/html5/thumbnails/4.jpg)
![Page 5: ARS Home : USDA ARS · face. The flow is expressed using Darcy's law while making three main assumptions: (1) the local hydraulic gradient is constant in time and equal to the local](https://reader034.fdocuments.net/reader034/viewer/2022042805/5f61fe1e642cc778cc3413ca/html5/thumbnails/5.jpg)
![Page 6: ARS Home : USDA ARS · face. The flow is expressed using Darcy's law while making three main assumptions: (1) the local hydraulic gradient is constant in time and equal to the local](https://reader034.fdocuments.net/reader034/viewer/2022042805/5f61fe1e642cc778cc3413ca/html5/thumbnails/6.jpg)
![Page 7: ARS Home : USDA ARS · face. The flow is expressed using Darcy's law while making three main assumptions: (1) the local hydraulic gradient is constant in time and equal to the local](https://reader034.fdocuments.net/reader034/viewer/2022042805/5f61fe1e642cc778cc3413ca/html5/thumbnails/7.jpg)
![Page 8: ARS Home : USDA ARS · face. The flow is expressed using Darcy's law while making three main assumptions: (1) the local hydraulic gradient is constant in time and equal to the local](https://reader034.fdocuments.net/reader034/viewer/2022042805/5f61fe1e642cc778cc3413ca/html5/thumbnails/8.jpg)
![Page 9: ARS Home : USDA ARS · face. The flow is expressed using Darcy's law while making three main assumptions: (1) the local hydraulic gradient is constant in time and equal to the local](https://reader034.fdocuments.net/reader034/viewer/2022042805/5f61fe1e642cc778cc3413ca/html5/thumbnails/9.jpg)
![Page 10: ARS Home : USDA ARS · face. The flow is expressed using Darcy's law while making three main assumptions: (1) the local hydraulic gradient is constant in time and equal to the local](https://reader034.fdocuments.net/reader034/viewer/2022042805/5f61fe1e642cc778cc3413ca/html5/thumbnails/10.jpg)
![Page 11: ARS Home : USDA ARS · face. The flow is expressed using Darcy's law while making three main assumptions: (1) the local hydraulic gradient is constant in time and equal to the local](https://reader034.fdocuments.net/reader034/viewer/2022042805/5f61fe1e642cc778cc3413ca/html5/thumbnails/11.jpg)
![Page 12: ARS Home : USDA ARS · face. The flow is expressed using Darcy's law while making three main assumptions: (1) the local hydraulic gradient is constant in time and equal to the local](https://reader034.fdocuments.net/reader034/viewer/2022042805/5f61fe1e642cc778cc3413ca/html5/thumbnails/12.jpg)
![Page 13: ARS Home : USDA ARS · face. The flow is expressed using Darcy's law while making three main assumptions: (1) the local hydraulic gradient is constant in time and equal to the local](https://reader034.fdocuments.net/reader034/viewer/2022042805/5f61fe1e642cc778cc3413ca/html5/thumbnails/13.jpg)
![Page 14: ARS Home : USDA ARS · face. The flow is expressed using Darcy's law while making three main assumptions: (1) the local hydraulic gradient is constant in time and equal to the local](https://reader034.fdocuments.net/reader034/viewer/2022042805/5f61fe1e642cc778cc3413ca/html5/thumbnails/14.jpg)