南方地區(qū)冷浸田土壤質量調查與評價指標體系研究
[Abstract]:The cold soaking field in southern China has a series of characteristics, such as large area, wide distribution, low yield, poor physical properties, accumulation of organic matter, strong reduction, low soil temperature, lack of available nutrients, poor permeability and so on. In this study, the soil physicochemical and biological characters of cold soaking field were investigated, the main obstacle factors of cold soaking field were determined, and the evaluation index of soil quality was screened. The minimum data set for soil quality evaluation was established. The results are of great significance for soil quality evaluation and soil improvement in cold soaking fields. The main results were as follows: (1) soil organic matter (44.04 鹵1.52 g/kg), total nitrogen (2.27 鹵0.08 g/kg), C / N (11.34 鹵0.26) were significantly higher in cold soaking field than in non-cold soaking field. The soil contents of total phosphorus, total potassium, alkali-hydrolyzed nitrogen and available potassium in cold soaking field were not significantly different from those in non-cold soaking field, and the content of total phosphorus, total potassium, alkali-hydrolyzed nitrogen and available potassium in cold soaking field were higher than that in non-cold soaking field, respectively. Soil available phosphorus (5.39 鹵0.92 mg/kg) in cold soaking field was significantly lower than that in non cold impregnated field and 84.6% lower than that in non cold impregnated field. The soil water content, available iron, available manganese, available zinc, Fe2, Mn2 and total content of reductive substances in cold-soaked field were significantly higher than those in non-cold-soaked field, the average values were 45.13 mg/kg,117.11 mg/kg,6.42 mg/kg, and 905.44 mg/kg,117.11 mg/kg,6.42 mg/kg, respectively. 956.10 mg/kg,61.36 mg/kg,2.48 cmol/kg, was 37. 6% higher than that in non-cold soaking fields, including 91. 5% 108. 1 and 17. 0% about 3. 34. 5% and 1. 43. 1% 217.9. (2) soil microbial biomass carbon (228.24 鹵69.37 mg/kg) and phosphatase activity (95.31 鹵11.62 mg/kg/h) were significantly lower than those in non-cold soaking field (43.8g / 25.2, respectively); (2) soil microbial biomass C (228.24 鹵69.37 mg/kg) and phosphatase activity (95.31 鹵11.62 mg/kg/h) were significantly lower than those in non-cold soaking field (P < 0.05). The activity of catalase in cold soaking field was significantly higher than that in non cold soaking field and was 21. 1% higher than that in non-cold soaking field. (3) the number of nematode in soil in cold soaking field was 301.95 / 100g dry soil, which was significantly lower than that in non-cold soaking field (584.31 鹵151.30 dry soil). The community composition and nutritional structure of soil nematodes in cold immersion field and non cold impregnated field were similar, and the general characteristics were plant parasitic nematode, bacterial nematode, nematode eating fungus nematode predation and omnivorous nematode. Dominant nematodes are widely distributed in rice fields in southern China, including (Filenchus), (Hirschmanniella), and (Cephalobus), (Aphelenchoides). The diversity index (H') and richness index (SR) of soil nematode community in cold soaking field were significantly higher than those in non cold impregnated field. (4) paired sample t test and principal component analysis were used. The results showed that the minimum data sets of soil quality evaluation in cold soaking field were total nitrogen, available phosphorus, available manganese, Fe2, pH, richness index (SR), and the soil quality index of cold soaking field was significantly lower than that of non cold soaking field. To sum up, the soil nutrient content is not low, but the soil moisture and reducing material are too much, so water conservancy engineering improvement is the primary task of soil improvement in cold soaking field. In addition, tillage improvement and fertilization improvement are also important ways to increase yield of cold soaking field.
【學位授予單位】:南京農業(yè)大學
【學位級別】:碩士
【學位授予年份】:2015
【分類號】:S159.2
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