the water which is added in the soil should be usefull for compaction of soil to know the dry density of the soil
The term plastic limit speaks to the characteristics of (fine grained) soil and how it behaves with different moisture content. Let's keep it simple. If the soil is nearly saturated, it will be "very" plastic and will act like play dough. If it's dry, it crumbles. There are no plastic characteristics. Different soils (different clay, sand or whatever in their content) act a bit differently with the same moistue content. Some will still be more plastic than others with a given moisture content. That's where the lab comes in. A given soil sample will have to be experimented on to determine its plastic limit. Wikipedia has an article posted on Atterberg limits, which include this soil characteristic. As this is WikiAnswers, a link is provided.
how do forest soils different from prairie soils
1.Red soil
Three percent is the percentage of organic matter in average soil. Organic matter content may range from one percent in the sandiest soils to five percent in the healthiest soils. Its percentage varies according to the amount of living or once-living animal and plant matter, the degree of moisture infiltration and percolation, and the soil pH.
Soils with a high clay content are poor draining and run off and standing surface water is likely.
The water content corresponding to the maximum dry unit weight or maximum dry density is know that as optimum moisture content.(o.M.c.) or optimum water content (o.w.c) maximum dry density is achieved at higher O.M.C.for cohesive soils or fine grained soils s compared to cohesionless soils.(sand 6-10%0
speedy moisture test are use to determine the moisture in the different soils.
speedy moisture test are use to determine the moisture in the different soils.
because of their sizes. As they are very close to each other they can have higher Moisture content, they can also hold the water for a very long time when compared to coarse grained.
There are no such thing as "earths measurements" - unless you are referring to the ways in which different earths (i.e., soils) are measured. Soils are typically measured in terms of density, PH, moisture, salinity, sand content, organic content, and biological content. Nitrogen and phosphorus measurements are also common. If you are looking for commonly reffered to measurements of the planet earth, consider asking for "earth's measurements." Or consult the wikipedia page for "earth."
Robin P. Gardner has written: 'Density and moisture content measurements bynuclear methods' -- subject(s): Soil moisture, Soils, Density, Radioactive gages, Measurement
A. van Wambeke has written: 'Calculated soil moisture and temperature regimes of South America' -- subject(s): Soil moisture, Soil temperature, Soils 'Calculated soil moisture and temperature regimes of Africa' -- subject(s): Maps, Measurement, Soil moisture, Soil temperature, Soils 'Soil moisture and temperature regimes of Central America, Caribbean, Mexico (SMSS technical monograph)' 'Management properties of ferralsols' -- subject(s): Ferralsols, Red soils, Soils
The term plastic limit speaks to the characteristics of (fine grained) soil and how it behaves with different moisture content. Let's keep it simple. If the soil is nearly saturated, it will be "very" plastic and will act like play dough. If it's dry, it crumbles. There are no plastic characteristics. Different soils (different clay, sand or whatever in their content) act a bit differently with the same moistue content. Some will still be more plastic than others with a given moisture content. That's where the lab comes in. A given soil sample will have to be experimented on to determine its plastic limit. Wikipedia has an article posted on Atterberg limits, which include this soil characteristic. As this is WikiAnswers, a link is provided.
it is the process of densifying granular soils. especially soils with silt content upto 20%
Sand content is part of many different native "soils", but they are not exactly the same thing. Loam soil - the best kind for growing things - is made up of fairly equal proportions of sand, silt, clay and organic matter. Some soils are high in clay (called "heavy" soils). Some soils are high in sand content - the soil in my own yard for example. So in a sentence: Sand is a component of most soils - it is not "soil" by itself.
how do forest soils different from prairie soils
Geoffrey Richard Lister has written: 'Observations on the growth and physiology of Pinus strobus L. seedlings grown under various conditions of soil moisture and nitrogen and phosphorus nutrition' -- subject(s): Soils, Growth, Pine, Soil moisture, Phosphorus content, Trees