chapter 5 Flashcards
What is soil formed from?Or how is soil formed?
the weathering of rocks
—-> it is the highly weathered outer layer of the Earth’s crust
What is soil composed of?
-Inorganic material: rocks, sand, silt and clay
-humus= partly decayed organic matter
-pore spaces (filled with water or air)
-living microorganisms (ex. Bacteria that decompose organic debris)
How many natural occurring elements does the earth include? And how are most found?in the form of what?
92
Most are found in the form of inorganic compounds called minerals.
What do rocks consist of? And what does this result in?
Most rocks consist of several different minerals (ex. Iron, calcium, potassium, sulphur, magnesium…)
This results in having different types of rocks
What are the 3 main types of inorganic soil particles?
sand, silt and clay. Different types of soil are mixtures of these particles in different proportions
What does the breaking down of rocks yield?
–Gravel(>2mm and mainly considered inert)
–Sand is large, coarse and gritty; it drains water quickly, but does not hold much water. It is good for aeration.
—Silt is medium in size.
—Clay is microscopic, sticky when wet, holds a lot of water but does not drain easily
What is a good soil?What does it allow?
loam soil that contains an ideal combination of sand, silt, and clay, which allows good drainage, water storage, and aeration
Topsoil
Most roots are found in the topsoil.
The topsoil contains soil mineral particles of different sizes (< 2 mm in diameter), humus, and living organisms (worms, insects…).
The topsoil is characterized by their relative amount of sand, silt and clay.
Soil composition determines the degree of water and nutrient binding to the soil particles.
Which minerals are available for uptake by the roots?
Only minerals that are dissolved in water, found in spaces or pores between soil particles,
What charge do both minerals and organic soil particles tend to have?
negative charge
they attract positive ions.
Mineral availability
*The negatively charged anions remain in solution
*The anions create a charge gradient (voltage) between soil and root cells.
*Consequently, positive ions move out of root cells
*Roots have proton (H+) pump: they actively pump H+ out and into soil.
*Creating a strong potential/electrochemical gradient.
*The gradient causes K+ and other positive ions to enter the roots via ion channels.
*Some anions enter roots (actively) via co-transporters
What affects root transport of minerals?
Membrane potential maintained by the root, water potential difference inside and outside the root.
Pores in soil
*About half of the soil volume is occupied by pores
*Pores may be filled with air or water.
*Some of this water is unavailable because it drains immediately due to gravity
*However, water that is held in small pores is readily available to plants.
*A balance of air and water in the soil is essential for root growth.
Acid soils
*The pH of a soil affects the release of minerals from weathering rock.
*For example, at low pH, aluminum, which is toxic to many plants and stunts (inhibits) root growth, is released.
(Example: most soils in the tropical Americas (ex. Columbia) are acidic; and aluminum-toxicity reduces corn yield).
*Most plants grow best at a slightly acidic pH.
*About 26% of the world’s arable soil is considerably more acidic than optimal pH for plant growth.
*Efforts are underway to breed more (aluminum) tolerant plants and to clean up polluted soil
Saline soils
–Accumulation of salt ions, usually Na+ and Cl-, changes the water potential in soil.
—Leading to a loss of water and turgor in plants.
—Saline soils most commonly occur in dry areas where salts are introduced through irrigation; and rain is not sufficient to wash the salts down beyond root area; so water evaporates, leaving salts behind in topsoil.
—Also saline soils can occur when overwatering pulls salts from the lower soil levels into the topsoil.
—In such areas, rain is not sufficient to remove the salts, which gradually accumulate in the soil