Water Movement in Soil

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Water- What is it ? ‣ Water is a di-polar, “charged” molecule ‣ The charges create bonds ‣ These bonds create adhesive and cohesive forces among molecules and surroundings Hydrogen atom Oxygen atom 105 o + -
- + H-bond + - + - BONDS AND WATER DIPOLES
Page 1 and 2: Water Movement in Soil James L. And
Page 3 and 4: CIDWT/University Disclaimer These m
Page 5 and 6: Water movement ‣ Why is this impo
Page 7 and 8: Hydrologic Cycle Precipitation ET S
Page 9 and 10: RAINFALL (48-54 Inches/Year) POTENT
Page 11 and 12: Precipitation Septic System Well In
Page 13: Water thru the Soil Treatment Area
Page 17 and 18: Flow to the System ‣ Amounts •
Page 19 and 20: System geometry Infiltrative surfac
Page 21 and 22: Drainage Contour Lines Drainfield D
Page 23 and 24: Drainage Contour Lines DRAINFIELD D
Page 25 and 26: Flow pattern in sub-surface surface
Page 27 and 28: Saturated Conditions Pores are fill
Page 29 and 30: HYDROLOGY OF A SEPTIC SYSTEM Infilt
Page 31 and 32: Soil terms ‣ Soil Horizon ‣ Soi
Page 33 and 34: What is unsaturated flow • Matric
Page 35 and 36: Pore size & unsaturated flow ‣ La
Page 37 and 38: Capillary Fringe ‣ Unsaturated zo
Page 39 and 40: Flow pattern in a gravity trench
Page 41 and 42: Flow pattern in a gravity trench
Page 43 and 44: Pressure distribution
Page 45 and 46: Soil treatment area sizing ‣ Sewa
Page 47 and 48: LTAR ‣ Texture/ Structure ‣ Oth
Page 49 and 50: Saturated soils contain free Free w
Page 51 and 52: Auger hole in soil is filled with a
Page 53 and 54: Water below water table has pressur
Page 55 and 56: Finding saturation in soils Identif
Page 57 and 58: Darcy’s law Flow (Q)/At = Ksat x
Page 59 and 60: Calculating Ksat ‣ In lab process
Page 61 and 62: Calculation of Q ‣ A = 1 ft 2 ‣
Page 63 and 64: Lateral movement Linear Loading Rat
Page 65:
Bouma Study ‣ Biomat = LTAR ‣ B
Page 68 and 69:
Putting it together Backfilled Soil
Page 70 and 71:
Summary of Influences on System per
Page 72 and 73:
Hydrologic cycle Precipitation Sept
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Water Movement in Soil

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