CEE 370 Environmental Engineering Principles Lecture #21 Water - PDF document

CEE 370 Lecture #21 10/28/2019 Print version Updated: 28 October 2019 CEE 370 Environmental Engineering Principles Lecture #21 Water Resources & Hydrology I: Groundwater Reading: Mihelcic & Zimmerman, Chapter 7 David Reckhow CEE 370 L#21 1 http://www.ec.gc.ca/water/images/nature/grdwtr/a5f2e.htm 2 CEE 370 L#23 David Reckhow Lecture #21 Dave Reckhow 1

CEE 370 Lecture #21 10/28/2019 D&M: Fig 6-19 Subsurface Hydrology  Aquifers  Confined, unconfined, perched, artesian  Saturated & unsaturated zone  Capillary fringe 3 CEE 370 L#23 David Reckhow 4 CEE 370 L#23 David Reckhow Lecture #21 Dave Reckhow 2

CEE 370 Lecture #21 10/28/2019 Artesian vs unconfined 5 CEE 370 L#23 David Reckhow Example 6 CEE 370 L#23 David Reckhow Lecture #21 Dave Reckhow 3

CEE 370 Lecture #21 10/28/2019 Example A 7 CEE 370 L#23 David Reckhow Hydraulic Gradient  Example B 8 CEE 370 L#23 David Reckhow Lecture #21 Dave Reckhow 4

CEE 370 Lecture #21 10/28/2019 9 CEE 370 L#23 David Reckhow More Definitions  Aquiclude – impermeable layer  Aquitard – less permeable than aquifer  Isotropic – aquifer conditions same in all directions  Anisotropic – properties differ in different directions  Homogeneous – characteristics uniform at different spatial locations  Heterogeneous – characteristics non-uniform  Springs – areas where water table intersects ground surface 10 CEE 370 L#21 David Reckhow Lecture #21 Dave Reckhow 5

CEE 370 Lecture #21 10/28/2019 Question  All else being equal, groundwater flows fastest in an aquifer composed of: A. Sand B. Loam C. Silt D. Clay E. Granite 11 CEE 370 L#21 David Reckhow Hydraulic Conductivity 12 CEE 370 L#23 David Reckhow Lecture #21 Dave Reckhow 6

CEE 370 Lecture #21 10/28/2019 Hydraulic Conductivity 7-25 13 CEE 370 L#23 David Reckhow  To next lecture 14 CEE 370 L#21 David Reckhow Lecture #21 Dave Reckhow 7