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The Soil Conservation and Domestic Allotment Act Pub. L. 74–461, enacted February 29, 1936) is a United States federal law that allowed the government to pay farmers to reduce production so as to conserve soil and prevent erosion.
Topsoil is composed of mineral particles and organic matter and usually extends to a depth of 5-10 inches (13–25 cm). Together these make a substrate capable of holding water and air which encourages biological activity.
During World War I prices shot up and farmers borrowed heavily to buy out their neighbors and expand their holdings. This gave them very high debts that made them vulnerable to the downturn in farm prices in 1920. Throughout the 1920s and down to 1934 low prices and high debt were major problems for farmers in all regions. [64]
Trump has argued that tariffs compel American companies to make goods on U.S. soil rather than purchasing from foreign suppliers. But some companies have other plans.
Agricultural production, marketing, and stabilization of prices. Agriculture and agricultural commodities. Animal industry and diseases. Crop insurance and soil conservation. Farm credit and farm security. Food from fresh waters. Food stamp programs. Forestry, and forest reserves and wilderness areas other than those created from the public domain.
Soils are the product of climate, organisms and topography, acting on parent (geologic) material over time. Thus the great diversity of geologic materials, geomorphic processes, climatic conditions, biotic assemblages and land surface ages in the United States is responsible for the presence of an enormous variety of mineral and organic soils.
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