長(zhǎng)期秸稈還田對(duì)連作棉田秸稈腐解特性及土壤有機(jī)碳平衡的影響
[Abstract]:Xinjiang is an important commodity cotton base in China, and its yield accounts for 60% of the whole country. Due to its large planting area, long planting years and other factors, the soil-borne diseases are aggravated, the proportion of soil nitrogen, phosphorus and potassium is unbalanced, and the soil enzyme activity is decreased. Become the bottleneck of cotton development in Xinjiang. Straw returning to the field is an important measure for the sustainable development of agriculture, but it can release allelopathic substances through snow water, Rain Water leaching and microbial decomposition while slowing down the obstacles of continuous cropping in cotton fields, thus exacerbating the obstacles of continuous cropping. Therefore, the advantages and disadvantages of straw returning to the field exist at the same time. The study of straw decomposition and soil organic carbon balance can provide scientific basis for evaluating soil quality and fertility. Therefore, this experiment is based on long-term continuous cropping location test. The decomposition law of cotton stalk and the change of soil organic carbon balance in cotton field were studied under the condition of returning straw for a long time. The results are as follows: 1. The decomposition of the aboveground part and root of cotton stalk under different treatments showed a trend of "fast, slow and fast" on the whole. 1 the period of rapid decomposition of the aboveground part of cotton stalk in 10 a and 20 years treatment was the first 43 days after straw returning to the field and the period of the first 43 days and 365 days after the straw was returned to the field. The period of 43193d is slow decomposing period; In the first year, the rapid decomposition period of cotton roots occurred in the period of 43177d and 19335th day, respectively, while the period of rapid decomposition of cotton root appeared in the first 43 days and 193365th days in 10a and 20a, respectively. The decomposition of cotton roots with different treatments was slow in the other time periods. After one year of decomposition, the decomposition rates of the aboveground part and root of cotton stalk reached 47% and 39%, respectively. Compared with non-continuous cropping years, continuous cropping promoted the decomposition of straw in the initial stage (16 days), but after one year, there was no significant difference in the decomposition rate of straw among different continuous cropping treatments. 2. After the cotton stalk was decomposed for a year, cellulose, hemicellulose and soluble sugar in the cotton stalk were released in large quantities, while the remaining part was released slowly. The release of cellulose, hemicellulose and soluble sugar was not affected by different continuous cropping treatments, but the decomposition of lignin was affected by 3. 3%. From the straw returning to the field to the second year before sowing (the release rate of 193 d), C was 34.82% and 39.62%), the release rate of N was 40.48% and 49.88%, and the release rate was 28.84% 34.09% and 95.4444% (97.19%). The nutrient release patterns were all direct release, and the order of release rate of cotton stalk to C ~ (2 +) N ~ (+) P and K was KNCP.. It was concluded that 60% of C was immobilized in soil after returning cotton straw to the field according to the release rule of N N P and K in cotton straw. At the same time, it also provided a lot of nitrogen and potassium for the soil, but the release of phosphorus was less, so the input of potassium and nitrogen could be reduced and the input of phosphorus fertilizer could be reduced in the process of fertilization in the field. 4. In 1 year cotton field, when the returning rate of cotton stalk reached 72.04%, the organic carbon of 0 ~ 20 cm soil layer could be balanced, and the equilibrium value was 11.84 g kg-1.. With the increase of returning years, the content and storage of organic carbon in soil increased gradually. When the returning years reached 28 years, 30 years and 39 years respectively, the organic carbon of 0 ~ 20 cm,20~40 cm and 40 ~ 60 cm soil layer could reach equilibrium, respectively. The equilibrium values of soil layers were 17.2g kg-1,15.38 g kg-1 and 12.72g kg-1.5.0~60 cm, respectively, and there was a significant positive correlation between the soil organic carbon storage and straw carbon input. But according to the increasing rate of soil organic carbon, the increase rate of soil organic carbon was the fastest within 5 years after continuous cropping of cotton and straw, but the accumulation of organic carbon in each soil layer increased slowly after 5 years, when the returning years reached 26 years, The maximum soil organic carbon storage of 0 ~ 60 cm is 112.2 t hm-2..
【學(xué)位授予單位】:石河子大學(xué)
【學(xué)位級(jí)別】:碩士
【學(xué)位授予年份】:2016
【分類號(hào)】:S141.4
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