南方地区冷浸田土壤质量调查与评价指标体系研究
[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 卤1.52 g/kg), total nitrogen (2.27 卤0.08 g/kg), C / N (11.34 卤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 卤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 卤69.37 mg/kg) and phosphatase activity (95.31 卤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 卤69.37 mg/kg) and phosphatase activity (95.31 卤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 卤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.
【学位授予单位】:南京农业大学
【学位级别】:硕士
【学位授予年份】:2015
【分类号】:S159.2
【参考文献】
相关期刊论文 前10条
1 刘占军;艾超;徐新朋;张倩;吕家珑;周卫;;低产水稻土改良与管理研究策略[J];植物营养与肥料学报;2015年02期
2 王飞;李清华;林诚;何春梅;钟少杰;李昱;林新坚;;福建冷浸田土壤质量评价因子的最小数据集[J];应用生态学报;2015年05期
3 贡璐;张雪妮;冉启洋;;基于最小数据集的塔里木河上游绿洲土壤质量评价[J];土壤学报;2015年03期
4 王思潮;曹凑贵;李成芳;熊又升;汪金平;;耕作模式对冷浸田水稻产量和土壤特性的影响[J];中国生态农业学报;2014年10期
5 徐祥玉;张敏敏;刘晔;袁家富;熊又升;周平刚;;磷钾调控对冷浸田水稻产量和养分吸收的影响[J];植物营养与肥料学报;2014年05期
6 熊又升;徐祥玉;张志毅;王娟;袁家富;刘光荣;徐昌旭;毛创业;;垄作免耕影响冷浸田水稻产量及土壤温度和团聚体分布[J];农业工程学报;2014年15期
7 邵玲玲;邹平;杨生茂;叶静;陶林富;俞巧钢;符建荣;;不同土壤改良措施对冷浸田温室气体排放的影响[J];农业环境科学学报;2014年06期
8 张绪美;沈文忠;李梅;;太仓市水稻土表层EC分布特征分析[J];土壤;2014年03期
9 陈娜;廖敏;张楠;徐培智;解开治;徐昌旭;刘光荣;;Fe~(2+)对水稻生长及土壤微生物活性的影响[J];植物营养与肥料学报;2014年03期
10 王飞;李清华;林营志;林诚;林新坚;刘玉洁;;冷浸田地下水位与农田小气候生境特征研究[J];农业现代化研究;2014年03期
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