作 者：
王秋菊;刘峰;焦峰;孙兵;郭中原;常本超;张劲松;高中超;姜辉
单 位：
黑龙江省农业科学院;黑龙江省农业科学院耕作栽培研究所;黑龙江省农业科学院土壤肥料与环境资源研究所;黑龙江八一农垦大学
关键词：
土壤;作物;物理性质;水田;深耕;化学性质;产量
摘 要：
为明确深耕在不同类型水田土壤上的改土效果及对水稻产量的影响,该研究应用自主研发水田深耕犁,在黑土和盐化草甸土上开展深翻、浅翻与旋耕对比试验研究。结果表明,深耕在不同类型土壤上对水稻产量及土壤理化性质影响存在差异:1)黑土深翻区增产7.28%~8.37%,浅翻区增产6.02%~7.72%,盐化草甸土深翻区和浅翻区与旋耕相比第1年水稻产量差异不大;第2年减产9.96%~11.03%;2)翻耕促进黑土土壤养分均一化,耕作层土壤养分降低不明显,土层间养分含量差异变小,盐化草甸土深耕后造成表层养分浓度降低,0~20 cm土层浅翻区和深翻区土壤有机质与对照相比分别下降4.57和6.68 g/kg,全氮分别下降0.24和0.29 g/kg,碱解氮0~10 cm土层分别比对照降低2.31和11.52 mg/kg,pH值明显增加,0~30cm土层交换性Na+浓度增加;3)与对照相比,浅翻和深翻降低了黑土下层土固相比率、容重,提高土壤通气、透水性,>10~20 cm土层土壤固相比率比对照分别降低4.23%和3.23%,土壤容重下降0.09 g/cm3和0.08 g/cm3,通气系数分别提高3.04倍和3.42倍,透水系数提高1.71倍和1.14倍;>20~30 cm土层深翻区土壤固相比率降低1.86%,通气系数和饱和透水系数比对照提高0.86倍和1.87倍;盐化草甸土浅翻区和深翻区均有增加下层土固相率和容重,降低通气、透水性的趋势。盐化草甸土水田不适合深耕,黑土型水田土壤深耕可改善土壤理化性质,提高水稻产量。
译 名：
Effect on improving mollisol paddy soil and saline meadow soil by continuous deep ploughing
作 者：
Wang Qiuju;Liu Feng;Jiao Feng;Sun Bing;Guo Zhongyuan;Chang Benchao;Zhang Jinsong;Gao Zhongchao;Jiang Hui;Institute of Soil Fertilizer and Environment Resources, Heilongjiang Academy of Agricultural Sciences;Management Department of Scientific Research of Heilongjiang Academy of Agricultural Sciences;Heilongjiang Bayi Agricultural University;Institute of tillage and cultivation, Heilongjiang Academy of Agricultural Sciences;Irrigation experimental establishment of Heilongjiang;
单 位：
Institute of Soil Fertilizer and Environment Resources, Heilongjiang Academy of Agricultural Sciences%Management Department of Scientific Research of Heilongjiang Academy of Agricultural Sciences%Heilongjiang Bayi Agricultural University%Institute of tillage and cultivation, Heilongjiang Academy of Agricultural Sciences%Irrigation experimental establishment of Heilongjiang
关键词：
soils;;crops;;physical properties;;paddy soil;;deep ploughing;;chemical characteristics;;yield
摘 要：
Heilongjiang province is the main production area of Japonica Rice in China. In Heilongjiang Province, rice growing areas are mainly distributed along Rivers and low plains. Due to the short time of planting rice, the development of paddy soil, which still keeps the original soil characteristics, is not completed. Rotary tillage is the main way of soil preparation in spring. Tillage depth is persistently maintained at 8-12 cm in paddy soil, which results in thin tillage layer, shallow plough bottom, and restricts rice root extension. With the decrease of soil holding capacity, rice plants prone to lodging at the later stage of growth, and rice yield and quality are affected. When the tillage layer is thin, the soil nutrient capacity is low, and the natural fertility is restricted, it is often used to increase the yield of rice by adding chemical fertilizer. The increase in the amount of fertilizer is not only a waste of fertilizer, but also pollutes the environment. The experimental results of the Honghe farm in the Sanjiang plain showed that, with the increase of paddy field tillage depth from 10 cm to 15 cm, the yield increased by about 10%. Japanese statistics showed that the thickness of the plough layer was more than 16-18 cm, some of which were more than 20 cm. The yield of rice was closely related to the thickness of topsoil. At present, there is no clear conclusion about the suitable depth of soil in different types of paddy soils in Heilongjiang Province.In order to clarify the effect of deep tillage on different types of paddy soils, the experiment, using the self-developed paddy deep plough, was carried out to study the effects of deep ploughing, shallow ploughing and rotary tillage in black soil and salinized meadow soil. Results showed that the effects of deep tillage on rice yield and soil physical and chemical properties were different. First, black soil deep ploughing treatment increased yield by 7.28%-8.37%. there was no significant difference in grain yield between the deep ploughing and rotary tillage treatment of salinized meadow soil in first years, but in the second year rice yield decreased by 9.96%-11.03%. Second, plowing promoted the homogenization of soil nutrients in black soil, and the soil nutrient content was not significantly reduced, and the difference of nutrient content between soil layers became smaller. Deep tillage caused the decrease of nutrient concentration in salinized meadow soil. The soil organic matter content of the shallow and deep ploughing treatments respectively decreased by 4.57 and 6.68 mg/kg compared with the control in 0-20 cm layer of salinized meadow soil, and total nitrogen decreased by 0.24 and 0.29 g/kg. The alkali hydrolyzable nitrogen in 0-10 cm soil layer of the kind of soil respectively decreased by 2.31 and 11.52 mg/kg, and pH value increased significantly, and the exchangeable Na+ concentration increased in the 0-30 cm soil layer. Third, compared with the control, the shallow and deep ploughing decreased the solid ratio and bulk density of black soil, and increased soil aeration and water permeability. The soil solid ratio of 10-20 cm soil layer was decreased by 4.23% and 3.23%, respectively. The soil bulk density was decreased by 0.09 and 0.08 g/cm3, and the ventilation coefficient increased by 3.04 times and 3.42 times, and the permeability coefficient increased by 1.71 times and 1.14 times, respectively. The soil solid phase ratio of deep ploughing treatment in the 10-20 cm soil layer of black soil was reduced by 1.86%, and the ventilation coefficient and saturated permeability coefficient increased by 0.86 times and 1.87 times. Fourth, there was a tendency to increase the subsoil solid and bulk density and reduce the ventilation and permeability of salinized meadow soil in the shallow and deep ploughing areas. Deep tillage is not suitable for salinized meadow soil, the effect is obvious in black soil, deep tillage can improve soil physical and chemical characteristics and increasing yield.
