Chapter 12 Flashcards
Mid-term Study
What is the functional role of a slope?
one of throughput: 1) evacuation of rock and debris
prepared by weathering and 2) of water carrying elements in solution
and suspension.
What is throughflow?
the lateral unsaturated flow of water in the soil zone, typically through a highly permeable geologic unit overlying a less permeable one. Water thus returns to the surface, as return flow, before or on entering a stream or groundwater.[1][2] Once water infiltrates into the soil, it is still affected by gravity and infiltrates to the water table or if permeability varies laterally travels downslope.[1] Throughflow usually occurs during peak hydrologic events (such as high precipitation). Flow rates are dependent on the hydraulic conductivity of the geologic medium
Where do slopes come from?
- Orogenic activity
- Linear erosion (e.g., Grand Canyon – 0.25 mm a−1 for 8Ma)
- Marine action
Slope form arises gradually
What is orogenic activity? (orogeny)
mountain-building process that takes place at a convergent plate margin when plate motion compresses the margin.
How is water transferred?
- Potential energy (ability to do work) of the water: water potential moves
along a gradient from high to low potential - Infiltration – movement of water into the soil (infiltration capacity)
- Three vertical moisture zones arise:
- wetting zone
- transmission zone
- saturated zone
Water potential moves along a gradient from __ to ___
high to low potential
What are the three vertical moisture zones?
wetting zone, transmission zone, saturated zone
Wetting zone
In this zone, the water content sharply decreases with depth from the water content of the transmission zone to near the initial water content of the soil.
Transmission zone
This zone is characterized by a small change in water content with depth. In general, the transmission zone is a lengthening unsaturated zone with uniform water content. The hydraulic gradient in this zone is primarily driven by gravitational forces.
saturated zone
The pore space in this zone is filled with water or saturated. Depending on the length of time elapsed from the initial application of the water, this zone will generally extend only to a depth of a few millimeters.
Darcy’s law
the capability of the liquid to flow via any porous media like a rock
q = K(H/L)
* q= discharge
* H/L = hydraulic gradient
(height/length)
* K = hydraulic conductivity
how much water is discharged as it goes through the soil matrix
what is the hydrological cycle?
movement of water into the soil and down through soil layers to the capillary zone etc
The larger the particle size ___ the more __
-larger the particle size= the more permeable; ease of water to permeate the ground; larger particles = bigger gaps vs smaller particles that have smaller gaps
soils are layered into horizons of __
different conductivities
Non-capillary macropores permit __
rapid
movement of water (karst, soil fauna, growth
and decay of roots, natural pipe network