秸稈深還不同年限對土壤水分物理性質(zhì)及抗剪強度的影響
[Abstract]:China is a big country in straw production, the total amount of straw in China exceeded 760 million t in 2006. Jilin Province is one of the main grain producing areas in China. The yield of corn straw in 2010 is about 24 million tons and the value is about 1.5 billion yuan. However, the value of straw resources has not been fully utilized. In Northeast China, about 30% of crop straw is burned directly after harvest, which not only wastes precious resources, but also causes air pollution and endangers traffic safety. Increase the hidden danger of fire and other aspects of great harm. In addition, the northeast black soil region, as the main grain producing area, is facing the serious problem of soil degradation. Since the reclamation, the black soil thickness, soil physical and chemical properties and fertility in the black soil region have deteriorated day by day, and some areas have lost their agricultural production capacity. Straw contains abundant nutrient raw materials, which can release a large amount of organic matter and nutrients needed by soil, plant and animal in the course of mineralization. In this paper, the problems of straw resource burning and farmland black soil degradation are discussed. Maize straw was applied to the subsurface layer of soil (20 ~ 40 cm),) to solve the problems of straw resources, and to improve soil fertility, permeability and water storage capacity. In the past, the physical and chemical properties of the topsoil were mainly studied after straw mulching and superficial application, so there was little research on the physical characteristics of straw depth and soil subsurface layer. The main conclusions are as follows: (1) the growth status and yield of maize were significantly improved compared with the control. (2) the soil total porosity, non-capillary porosity, maximum water holding capacity and capillary water holding capacity of the surface and subsurface layer of straw were increased in the treatment of NPK O 12. The field water holding capacity was significantly increased, among which the straw treatment data reached the peak value two years later. (3) Straw depth also enhanced the soil osmotic capacity, and the water stable infiltration value in the second year of straw depth was significantly higher than that of other treatments. (4) Straw depth could also promote the transformation from 0.25 mm microaggregate to 0.25 mm large aggregate. Among them, the effect of straw depth was the most significant after 2 years. (5) with the increase of water content, the cohesion of soil increased first and then decreased, while the angle of internal friction decreased linearly. The results showed that straw depth could effectively reduce soil cohesion and internal friction angle, and the second year straw depth had the largest decrease in soil cohesion and internal friction angle, followed by the first year. In the third year, the cohesion and internal friction angle of soil increased, but still lower than CK..
【學位授予單位】:吉林農(nóng)業(yè)大學
【學位級別】:碩士
【學位授予年份】:2015
【分類號】:S141.4
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