1.The degree to which water clings to the soil is the most important soil water characteristic to a growing plant. This concept is often expressed as soil moisture tension. Soil moisture tension is negative pressure and commonly expressed in units of bars. During this discussion, when soil moisture tension becomes more negative it will be referred to as "increasing" in value. Thus, as soil moisture tension increases (the soil water pressure becomes more negative), the amount of energy exerted by a plant to remove the water from the soil must also increase. One bar of soil moisture tension is nearly equivalent to -1 atmosphere of pressure (1 atmosphere of pressure is equal to 14.7 pounds per square inch at sea level).
2. A soil that is saturated has a soil moisture tension of about 0.001 bars, or less, which requires little energy for a plant to pull water away from the soil. At field capacity most soils have a soil moisture tension between 0.05 and 0.33 bars. Soils classified as sandy may have field capacity tensions around 0.10 bars, while clayey soil will have field capacity at a tension around 0.33 bars. At field capacity it is relatively easy for a plant to remove water from the soil.
3.The wilting point is reached when the maximum energy exerted by a plant is equal to the tension with which the soil holds the water. For most agronomic crops this is about 15 bars of soil moisture tension. To put this in perspective, the wilting point of some desert plants has been measured between 50 and 60 bars of soil moisture tension.
4.The presence of high amounts of soluble salts in the soil reduces the amount of water available to plants. As salts increase in soil water, the energy expended by a plant to extract water must also increase, even though the soil moisture tension remains the same. In essence, salts decrease the total available water in the soil profile.
ofcourse.humidity add moisture in the soil......
A test for soil moisture is to:1. weigh a brown paper bag2. add a sample of your soil to that bag3. weigh the total weight of the bag plus the soil4. put the bag of soil in an oven for 24 hours at 200 degrees5. reweigh the bagsubtract the final/dry weight of the bag from the initial soil bag weight and that number will be the weight of moisture that has left the soil.
The soil curve, also known as the soil moisture characteristic curve, typically shows the relationship between soil water content and soil suction (or tension). It generally shows that as soil suction increases, soil water content decreases. The curve can vary depending on soil type and compaction.
Factors that influence soil moisture include precipitation, temperature, evaporation rates, soil composition, and topography. Other factors such as vegetation cover, drainage patterns, and human activities can also impact soil moisture levels. Ultimately, the balance between water inputs and outputs in the soil determines its moisture content.
Soil moisture utilisation refers to the ability of plants to access and use water stored in the soil for their growth and development. It is a crucial factor in determining plant health and productivity, as inadequate soil moisture can lead to water stress and hinder plant growth. Farmers often monitor and manage soil moisture levels to ensure optimal conditions for plant growth.
To determine the moisture content of soil, you can use a soil moisture meter or follow the oven-drying method. With a soil moisture meter, insert the probe into the soil and read the moisture level displayed. For the oven-drying method, weigh a soil sample, dry it in an oven, and weigh it again to calculate the moisture content.
Capillary moisture refers to water that is held in the tiny spaces between soil particles through capillarity, which is the ability of water to move through small pores due to surface tension. This moisture is crucial for plant growth as it is accessible to roots, providing essential hydration and nutrients. Capillary moisture is distinct from gravitational water, which drains away, and hygroscopic water, which is tightly bound to soil particles and unavailable to plants. Understanding capillary moisture helps in effective soil management and irrigation practices.
ofcourse.humidity add moisture in the soil......
The soil in a region is saturated, and rainfall is greater than the need for the moisture.
A test for soil moisture is to:1. weigh a brown paper bag2. add a sample of your soil to that bag3. weigh the total weight of the bag plus the soil4. put the bag of soil in an oven for 24 hours at 200 degrees5. reweigh the bagsubtract the final/dry weight of the bag from the initial soil bag weight and that number will be the weight of moisture that has left the soil.
Soil moisture meters are devices to measure the soil moisture for irrigation messuring. Some devices have data logging or georeferencing capabilities.Some of the other functions of soil moisture meter:Monitoring the soil moistureMonitor salinity and temperatureTo check the electrical conductivityTrack and manage salinity levels
Evaporation process in the hydrologic cycle puts soil moisture in the atmosphere. The moisture is evaporated.
The soil curve, also known as the soil moisture characteristic curve, typically shows the relationship between soil water content and soil suction (or tension). It generally shows that as soil suction increases, soil water content decreases. The curve can vary depending on soil type and compaction.
the worm stirs up the soil to moisture it
Factors that influence soil moisture include precipitation, temperature, evaporation rates, soil composition, and topography. Other factors such as vegetation cover, drainage patterns, and human activities can also impact soil moisture levels. Ultimately, the balance between water inputs and outputs in the soil determines its moisture content.
The film of moisture helps to prevent excessive evaporation from the soil surface, providing a protective barrier that helps retain soil moisture. It also helps to regulate soil temperature, reduce weed growth, and protect the soil from erosion.
geology) In soil mechanics, the resistance of particles to being pulled apart due to the surface tension of the moisture film surrounding each particle. Also known as film cohesion.