soil texture


Also found in: Wikipedia.

soil texture

1. In a mass of soil, the relative proportion of clay particles to the sand and silt particles.
2. The particle-size distribution of a mass of soil.
References in periodicals archive ?
However, specific soil characteristics, such as soil texture, or the chemical parameters of pH, nitrogen, and carbon content, have not been described at the spatial scale of the individual burrow, except in the context of comparing gopher mound soil to the surrounding matrix (Simkin et al, 2004).
This is why it is important to determine the optimum conditions for an efficient infection, evaluating potentially important factors such as inoculum density, temperature, humidity, and soil texture.
To make the crumb, mix all the dry ingredients together and then melt the butter and add the dry mix and form to a soil texture.
2016) and this successful use of nematodes as biological tool is critically dependent upon many other factors such as soil moisture, air and soil temperatures, soil texture, application time and crop variability and features (Kaya, 1993; Gaugler, 2002).
The rate at which a particular soil can absorb water is called the infiltration rate, which depends on soil texture, organic matter (OM) content, soil moisture content, compaction and other cultural practices that can affect the physical properties of soil (Lado et al.
Water is held against the roots by uneven or irregular layers of soil texture.
The data of soil texture has been presented in (Table 2) which is the relative measurement of sand, silt and clay particles, having size less than 2mm [19, 20].
Among their topics are the politics of maize agriculture in post-classic Central Mexico, modeling the caloric landscapes of the past, soil texture and agricultural resilience in the prehistoric southwest: farming on Arizona's Perry Mesa, reforestation and the origins of the modern industrial tree farm, and southern slow foods: ecological awareness through gourmet heritage.
The general soil texture is loamy (particle proportions are approximately 50% sand, 35% silt and 15% clay).
The effects of soil compaction can persist in a forest soil for several decades depending on soil texture, machine activity, soil water content, and other soil conditions at the time of harvesting (Kozlowski, 1999; Demir et al.
soil taxonomical classification, soil texture was defined for the different soil types of Kundahpalam watershed.