Term
Benefits of vegetation along streams |
|
Definition
-Grasses best on banks -Trap sediment transported from streams -Make streams deeper/narrow -Problem w/ trees is they are big & die, fall in stream destabalizing & causing turbulence.(Large woody debris) |
|
|
Term
Measurements of Area: -Acre in feet -Mile in acres -Hector in acres -Kilometer:Miles -Mile:kilometers |
|
Definition
-Acre:43,560sq ft(size of football field including sidelines. -Mile: 640acres -Hector: 2.5 Acres -Kilometer: 0.62 Miles -Mile: 2.7 km sq |
|
|
Term
|
Definition
Particle size, sand,silt or clay? determines acquisition, retention, transmittion of water. |
|
|
Term
How are "peds" held together? |
|
Definition
electrochemical bonds & organic gels- they allow for more aeration of water/air, root system growth, porosity. |
|
|
Term
What is rock gravity density? |
|
Definition
2.7 jules, soil is about 1/2 rock so around 1.35 jules. |
|
|
Term
How much does a cubic ft of water weigh? Soils? |
|
Definition
Water=62.4lbs, soil=90lbs |
|
|
Term
|
Definition
Alluvium= material along streambanks. colluvium= material accumulating on hillsides, didnt make it down to streams. |
|
|
Term
|
Definition
wind deposited accumulation |
|
|
Term
What are some soil forming factors? Clorpt equation! |
|
Definition
-Climate:MOST IMPORTANT, water makes all chem. & physical reactions possible, too much water= leaching.(30 inches is best amount!), temperature, and wind. -organisms, includes humans -relief: the terrain: sunny/shady sides, flood plains etc. -Parent Material -TIME |
|
|
Term
What is podzolization and where does it occur? |
|
Definition
Podzolization= Soils stripped of most nuitrients, white soil: spodisols; occurs in humid regions with excess water. |
|
|
Term
Why are there no forests in the midwest? |
|
Definition
Indians burned them all down. |
|
|
Term
How did prairies grow in the west? Not enough precipitation. |
|
Definition
|
|
Term
|
Definition
-Sheet: raidrops have large impact when hit move layer of topsoil. -Rill: gullies small enough to move over. -Gully: large channels, too big for vehicles to move over -Stream erosion |
|
|
Term
Problems of erosion in water |
|
Definition
-lost productivity, decrease in aggregates -exposure of subsoil/loss of topsoil/lack infiltration, fertility. -Sediment is greatest pollutor of water in world; fills harbors/rivers, costly to dredge; chokes out fish |
|
|
Term
What is terminal velocity? |
|
Definition
-30feet More intense the rain/greater size of raindrops= closer to terminal velocity -Can be decreased by vegetation: directly- interception of leaves, can increase effects in tall canopies, forming very large raindrops easier to reach terminal velocity. |
|
|
Term
|
Definition
earthworms, ants, termites, bugs, moles, etc. |
|
|
Term
Structure on effects of raindrops |
|
Definition
-Very powerful: Well structured soil can prevent. -Cementing material -organic gels -minerals(calcium carbonate) -Clay -CEC |
|
|
Term
What are some wind erosion factors? |
|
Definition
-Preponderance: Direction wind is coming from, just one or multiple? -Soil structure: strong aggregates, anything larger than 1mm won't move. -Surface ridges(furrows): tilled land into ridges reduce velocity, BUT must be correct, can create turbulence if incorrect and increase erosion in tunnels. -Length of field: longer the stretch, more the erosion -avalanching: long area creates "Fetching"= creation of waves like that of a deep ocean= more velocity and grip it gets. As soil moves downwind it usually more smooth the further down. -Vegetative cover: more cover= more windbreak. -Keep land wet and it wont erode from wind! avoid wilting point!(15 bars) |
|
|
Term
Who creates soil surveys? |
|
Definition
Natural resources Conservation Services. -started in 1899, mapped soils directly on topography. -1950-70's, got mucher better: showed land best for farming, urban development, etc.(class 1_) & land not even good enough to walk on (class 8) |
|
|
Term
Factors of soil structure: Clay, organic |
|
Definition
-Clay: upto 40% clays in soil is beneficial more than that is not. -Organic material @ a certain concentration can be adverse. |
|
|
Term
|
Definition
-Most erosion occurs on banks of streams when wet, water aquires pore pressure, breaks off easily. -Floodplains: Usually don't erode, low slope lots of vegetation.
-Wetter then bank, less the strength -Grazers can can erode through hooves or eating vegetation on banks. |
|
|
Term
|
Definition
Rocks stored along streams to prevent erosion. |
|
|
Term
What grains get lost in stream erosion? |
|
Definition
-Sand is most easily eroded, not large enough to resist or small enough for cohesion. -Clay: once loses cohesion, lost in water indefinately. |
|
|
Term
What are the factors of stream power? |
|
Definition
-Density: sediment load(minor role) -Velocity -Depth: deeper the water more the power. -multiply all together to find power. |
|
|
Term
What is avg soil loss tolerance? |
|
Definition
2-5 tons/acre-year(T-FACTOR) --1 ton= 200lbs -Soil regenerates 1 inch/century! |
|
|
Term
What are some tolerance factors(T-factors)? |
|
Definition
Depth of existing soil type/depth of parent material fertility of subsoil- always less fertile than topsoil |
|
|
Term
What is the universal soil loss equation? |
|
Definition
Annual soil loss= rainfall*soil erodibility*angle of slope*length of slope*vegetative cover*conservation.(last two are cultural factors, changable) |
|
|
Term
|
Definition
suspension: 1/2 mm & smaller suspended in air, can move 1000's of miles. Saltation: 1/2 mm and up, bouncing across landscape. surface creep: 1 mm & larger |
|
|
Term
Major problems of wind erosion |
|
Definition
-fine particles sorted & carried off which can cause major loss of nuitrients. -Abrasion of plants & materials -air pollution -deposition. |
|
|
Term
What are some factors to crop cover under the annual soil loss equation? |
|
Definition
C= crop factor obtained from percent of rain that strikes vegetation before falling on soil surface(Crop canopy), prior land use, surface cover & surface roughness. X= slope. |
|
|