TEXT B Soil quality is one of the
most basic and perhaps least understood indicators of land health. Soil supports
plant growth and represents the living reservoir that buffers tile flows of
water, nutrients, and energy through an ecosystem. Soil quality refers to the
capacity of a soil to perform these beneficial functions and is determined by
its texture, structure, water-holding capacity, porosity, organic matter
content, and depth, among other properties. Because soils naturally vary in
their capacity to perform these functions, we must tie our understanding of soil
quality to landscapes and land use. We must understand soil quality for two
important reasons: First, we must match our use and management of land to soil
capability. Second, we must establish baseline understanding about soil quality
so we can recognize ongoing trends. If soil quality is stable or improving, we
have a good indicator that the ecosystem is sustainable. If soil quality is
deteriorating, the larger ecosystem will almost certainly decline with
it. People describe soil types in all kinds of ways such as
heavy, light, sandy, clay, loam, poor or good. Soil scientists describe soil
types by how much sand, silt and clay is present. This is called texture. It is
possible to change the texture by adding different things to the soil. You can
roughly estimate the texture of a soil by a simply method called "manual
texturing", through determining the feel of a moist sample when rubbed between
the thumb and forefinger. If the soil sample is predominantly sand, it will feel
very gritty. If it is predominantly silt, it will feel smooth or slippery to the
touch. And if it is predominantly clay, it will feel sticky.
Particle size has a lot to do with a soil’s drainage and nutrient holding
capacity. Sand is the largest particle and doesn’t hold many nutrients. Silt is
a soil particle whose size is between sand and clay. When wet, silt feels smooth
but not sticky. Clay is smooth when dry and sticky when wet. Soils high in clay
content are called heavy soils. Clay also can hold a lot of nutrients, but
doesn’t let air and water through it well. To better understand how big these
three soil particles are, think of them like this. If a particle of sand were
the size of a basketball, then silt would be the size of a baseball, and clay
would be the size of a golf ball. It can be inferred from the passage that a soil sample with little or no clay in it ______.
A.will feel smooth when wet B.may not keep its shape when molded C.will be difficult to classify D.may be sticky if too wet