Chapter 4: Water Management Flashcards
How much of the absorbed water may be transpired into the air by a tree?
As much as 95% (a large tree can absorb hundreds of gallons of water in a day)
available water
water remaining in the soil after gravitational water has drained and before the permanent wilting point has been reached; capillary water while hygroscopic water is unavailable for water
What causes wilting?
When the available water in the soil decreases to a point at which a plant cannot take up enough to replace the water lost through transpiration.
water-holding capacity
ability of a soil to hold moisture; total amount of water held by a soil after drainage occurs (when it is at field capacity); varies with soil texture (sand, silt, and clay content)
What types of soils have a greater water-holding capacity?
Fine-textured soil (clays) have a greater water-holding capacity than coarse-textured soils (sands); that is why sandy soils need to be irrigated for shorter periods, but more frequently than clay soils; water needs to be applied slowly and over extended periods of time if infiltration rate is low
infiltration
downward entry of water into the soil; or entry of fine particles into drainage or aeration systems, can lead to system clogging and failure; or downward entry of materials from one soil or fill layer to another, as when a gravel road surface mixes with underlying soil
percolation
movement of water through/within the soil
infiltration rates
speed at which water penetrates the soil
percolation rates
speed at which water moves through the soil
What influences percolation and infiltration rates?
type of soil (clay soils usually have much lower infiltration rates and percolation rates than sandy soils), soil structure (soil with poor structure, such as compacted soils, have lower infiltration and percolation rates), and bulk density
Adaptations to survive in arid regions?
develop extensive root systems (deep, spreading roots to make use of soil moisture over a large volume and tap into water sources found deep underground), shed leaves, become virtually dormant and dry completely, have small leaves, waxy cuticle, tiny leaf hairs, and sunken stomata
turgid
fully hydrated to a normal state of distension
When do drought stress symptoms develop?
When water loss from the foliage exceeds the rate at which it can be replaced via uptake by the root system.
desiccation
severe drying out; dehydration
Generally, what is better? Frequent shallow watering or infrequent deep soakings?
Infrequent deep soakings because it encourages the development of a deeper root system and more drought-tolerant trees; soils high in clay can be improved when allowed to dry out between irrigations because the natural shrinking and swelling of the soil can improve the soil structure and water infiltration rate; frequent shallow watering encourages surface rooting and compacts the soil surface, reducing the infiltration rate; however mulch and soil high in organic matter should not be allowed to completely dry out because they resist rewetting