The bigger the particle size, the more drainage the soil would have. The smaller the particle sizer, the less drainage the soil would have. ITS EASY
Factors that affect evaporation include temperature, humidity, wind velocity, exposed surface area, porosity of soil, grain size of soil particles, soil water content, matric potential, and sun intensity.
Because depends on how the soil is
glaciers pushed soil from New England to the middle colonies
Tornadoes do not cause significant weathering, though they can cause localized soil erosion.
Soil texture is only one of the parameters used to determine the kind of crops that can be grown. temperature, humidity , top soil dept and drainage are other very important parameters, When the question is asked "what kind of vegetation is supported" the simple answer is any kind f vegetation. Characterization of soil texture is a very technical science, and the mixing of 4 characteristics seems a frivolous question or an uninformed opinion
Loam soil typically has a particle size that falls between sand and clay, making it a mixture of different particle sizes. The particle size ranges from 0.002 to 0.02 mm, allowing for good drainage and moisture retention in the soil.
The three basic textures a soil can have are sand (largest particle size), silt (medium particle size), and clay (smallest particle size). The relative proportions of these particles in a soil determine its texture and properties such as water retention and drainage.
soil ferility
The largest particle size in soil is known as gravel, which typically ranges from 2 to 64 millimeters in diameter. Gravel particles are larger than sand and silt particles and contribute to soil drainage and aeration.
Sandy soil allows water to pass through it the fastest due to its large particle size and good drainage properties. Clay soil, on the other hand, has the slowest drainage due to its smaller particle size and tendency to compact. Loam soil provides a good balance between sand, silt, and clay, allowing for both water drainage and moisture retention.
what about soil are you asking about? In terms of texture earthworms and organic matter can affect it. In terms of acidity soil particle size and acid rain can affect it.
Size matters
The texture or particle size of soil determines its porosity, permeability, water-holding capacity, and ability to support plant growth. Finer particles like clay hold more water and nutrients but might have poor drainage, while larger particles like sand have good drainage but may not retain nutrients well.
Sandy soil will allow water to pass through fastest due to its larger particle size and better drainage properties.
Soil particle size influences the soil's physical properties like porosity, permeability, and water holding capacity, which affect plant growth. It also plays a role in determining soil fertility and the rate at which nutrients are released to plants. Additionally, soil particle size affects soil composition and structure, influencing its ability to support various types of vegetation.
The texture or particle size of soil determines its permeability (how well water can flow through it), its ability to retain nutrients, and its drainage properties. Soils with different textures will have varying capacities to support plant growth and overall ecosystem function.
Soil particles come in a range of sizes, from very fine particles like clay to larger particles like sand and gravel. The size of soil particles influences properties like water retention, drainage, and nutrient availability in the soil. Particle size distribution is an important factor in determining soil texture and overall soil quality.