• ISSN 1008-505X
  • CN 11-3996/S

隔年深翻20 cm以上有效改善江汉平原瘠薄型稻田再生稻产量、养分吸收和土壤肥力

Deep tillage exceeding 20 cm every two years improves ratoon rice yield, nutrient uptake and soil fertility of infertile paddy fields in Jianghan Plain

  • 摘要:
    目的 深翻是改善瘠薄型稻田耕层结构和提升产能的关键措施。研究深翻对长江河流冲积物发育的瘠薄型水稻土头季和再生季水稻养分吸收、产量及不同土层理化性质的影响,为确定合适的深翻深度提供依据。
    方法 2022和2023年连续在江汉平原进行了田间定位试验,该区稻田犁底层为13~22 cm。设置耕深分别为15、20和25 cm,以常规旋耕(12 cm)为对照。头季和再生季稻成熟期,齐地收割地上部植株,分为茎、叶、穗样品,调查生物量和稻谷产量、产量构成因素,分析各部位养分吸收量。于试验开始前取0—20 cm土层土样,每年试验结束时,分别取0—10、10—20、20—30 cm土层土样,测定理化性质。
    结果 与对照相比,2022年深耕15和25 cm再生季稻产量分别增加了19.01%和25.15%,2023 年各耕深处理对头季稻、再生季稻产量均无显著影响。深翻20、25 cm处理可提高头季稻和再生季稻的穗粒数,耕作深度不影响有效穗数和结实率。与常规旋耕相比,2022年3个深翻处理对头季稻籽粒、茎秆、地上部氮累积量无显著影响,2023年显著降低头季稻籽粒氮积累量,提高了再生季稻茎秆氮积累量,且深翻25 cm的茎秆氮积累量还显著高于15、20 cm耕深处理;除2022年耕深25 cm显著提高了头季稻籽粒、茎秆及地上部磷积累量外,两年耕深处理对头季稻、再生季稻籽粒和茎秆以及地上部磷积累量无显著提升效果;2022年3个耕深处理显著提高了头季稻茎秆钾积累量,2023年耕深15、20 cm 处理显著提高了再生季稻茎秆钾素累积量。3 个耕深处理之间头季稻和再生季稻地上部氮、磷、钾积累量大多情况下无显著差异。耕深20和25 cm处理两年后,0—30 cm 土层容重降低了1.80%~5.36%,总孔隙度增加了 2.62%~5.13%,对0—10 cm 土层影响最显著。试验两年后,耕深20和25 cm处理增加了0—20 cm土层毛管孔隙度,提高了20—30 cm土层有机质含量,深翻25 cm处理降低了0—10 cm土层碱解氮和速效磷含量,耕深15 cm处理降低了0—10 cm土层速效磷含量。
    结论 长江河流冲积物发育的瘠薄型稻田,隔年深翻20 cm以上,可提升头季稻和再生季稻产量,并达到松土培肥的效果。

     

    Abstract:
    Objectives Deep tillage is a key measure to improve the soil structure of infertile paddy fields and enhance production capacity. We compared the effects of tillage depths on the yield of the first crop and ratoon rice, and the physical and chemical properties of infertile paddy soil in Jianghan Plain.
    Methods Field experiments were conducted in the Jianghan Plain in 2022 and 2023. The plow layer of the paddy fields in this area was 13−22 cm deep. Three tillage depths of 15 cm, 20 cm, and 25 cm were set up in the experiment, with conventional rotary tillage (12 cm) as the control. At the maturity of the main crop and ratoon crop, the aboveground parts of the rice plant were collected and divided into stem, leaf, and spike samples, the rice biomass, nutrient accumulation in each part, yield and yield components were investigated. The 0−20 cm soil samples at the beginning, and the 0−10 cm, 10−20 cm, and 20−30 cm soil samples of each treatment at the end of the experiment were collected to analyze the physical and chemical properties.
    Results Compared with the control, tillage 15 cm and 25 cm deep increased the ratoon rice yield by 19.01% and 25.15% respectively in 2022, and tillage depth had no significant yield effects on both the first crop and ratoon rice in 2023. Deep ploughing at a depth of 20−25 cm could increase the number of grains per spike of the first crop and the regrowth crop. The ploughing depth did not affect the number of effective spikes and the rate of fruiting. Compared with conventional tillage, the three deep ploughing treatments in 2022 had no significant effect on the nitrogen accumulation of the main crop rice grains, stems, and above-ground parts. In 2023, the nitrogen accumulation of the main crop rice grains was significantly reduced, while the nitrogen accumulation of the ratoon crop rice stems was increased. Moreover, the nitrogen accumulation of the stems in the 25 cm deep ploughing treatment was significantly higher than that in the 15 cm and 20 cm ploughing treatments. Except for the 25 cm ploughing depth in 2022, which significantly increased the phosphorus accumulation of the main crop rice grains, stems, and above-round parts, the two-year ploughing depths had no significant effect on the phosphorus accumulation of rice grains, stems, and above-ground parts of both the main crop and the ratoon crop. In 2022, the three ploughing depths significantly increased the potassium accumulation of the main crop rice stems, and in 2023, the 15 cm and 20 cm ploughing depths significantly increased the potassium accumulation of the ratoon crop rice stems. In most cases, there was no significant difference in the nitrogen, phosphorus, and potassium cumulation of the above-ground parts of the main crop and ratoon rice among the three ploughing depths. After two years of tillage 20 cm and 25 cm deep, the soil bulk density of 0−30 cm soil layers decreased by 1.80%−5.36%, and the total porosity increased by 2.62%−5.13%, with the most significant effect observed in the 0−10 cm soil layer. The treatments with tillage depths of 20 cm and 25 cm increased the capillary porosity in the 0−20 cm soil layer and enhanced the organic matter content in the 20−30 cm soil layer. The treatment of deep tillage at 25 cm reduced the available nitrogen and available phosphorus contents in the 0−10 cm soil layer, while the treatment with a tillage depth of 15 cm decreased the available phosphorus content in the 0−10 cm soil layer.
    Conclusions For the infertile paddy fields formed by the alluvial deposits of the Yangtze River, a deep tillage of more than 20 cm every two years can increase the yields of the first crop rice and the ratoon rice, and achieve the effect of loosening the soil and enriching it.

     

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