• ISSN 1008-505X
  • CN 11-3996/S

隔年深翻20 cm有效改善江汉平原瘠薄型稻田水稻产量、养分吸收和土壤肥力

Plowing 20 cm deep every two years improves rice yield and 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—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15 cm、20 cm和25 cm,以常规旋耕(12 cm)为对照。头茬和再生稻成熟期,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年耕深20和25 cm处理显著增加了头茬稻产量9.58%和7.82%,深耕15、25 cm增加了再生稻产量分别增加了 9.58%和 25.15%,2023年各耕深处理对头茬稻、再生稻产量均无显著影响。深翻20、25 cm处理可提高头茬稻和再生稻的穗粒数或者结实率,耕作深度不影响有效穗数和千粒重。与常规旋耕相比,2022年3个深翻处理对头茬稻、再生稻籽粒、茎秆、地上部氮累积量无显著影响,2023年降低了头茬稻籽粒氮积累量,提高了茎秆氮积累量,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提高了头茬稻茎秆磷积累量,两年耕深处理对头茬稻、再生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个耕深处理提高了头茬稻籽粒钾积累量,2023年耕深15、20 cm处理提高了再生稻茎秆钾素累积量。3个耕深处理之间头茬稻和再生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%,0—10 cm土层影响最显著。试验两年后,耕深20和25 cm处理0—10和10—20 cm土层毛管孔隙度和通气孔隙度分别增加了2.24%~9.41%和1.52%~6.07%;深翻20和25 cm处理提高了20—30 cm土层有机质含量,深翻25 cm降低了0—10 cm土层碱解氮和速效磷含量,耕深15 cm处理也降低了0—10 cm土层速效磷含量,但提升了有效钾含量。
    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,可显著提升头茬和再生稻产量,并达到松土培肥的效果。

     

    Abstract:
    Objectives Deep plowing is a key measure to improve the soil structure of infertile paddy fields and enhance production capacity. We compared the effects of plowing 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 plowing depths of 15 cm, 20 cm, and 25 cm were set up in the experiment, with conventional rotary plowing (12 cm) as the control. At the maturity of 1st-crop and ratoon rice, 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, the plowing depths did not affect the yield of 1st-crop rice in 2022, plowing 15 cm and 25 cm deep increased the ratoon rice yield by 9.58% and 25.15% respectively; In 2023, plowing depth had no significant yield effects on both the first crop and ratoon rice, although plowing 20 cm and 25 cm increase the grain number per panicle or the seed setting rate of both the first crop of rice and the ratoon rice. Compared with control for the first crop rice, plowing depths did not show significant effect on the nitrogen accumulation in all parts of both rice in 2022, and deep plowing reduced the grain N accumulation but increased straw N accumulation of the first crop rice in 2023. Moreover, the straw N accumulation under the 25 cm deep plowing treatment was significantly higher than that under the 15 cm and 20 cm plowing depth treatments. Except that plowing 25 cm deep in 2022 increased the straw P accumulation of the first crop rice, plowing depths had no significant promoting effect on P accumulation in grains, straw, and above-ground parts of both the rice in the two years. In 2022, deep plowing increased the grain K accumulation of the first crop rice, and in 2023, plowing 15 and 20 cm treatments increased the straw K accumulation of the ratoon rice. In most cases, there was no significant difference in the accumulation of N, P and K the above-ground parts of both rices among the three plowing depth treatments. After two years of plowing 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 capillary porosity and aeration porosity in 0−10 cm and 10−20 cm soil layers increased by 2.24%−9.41% and 1.52%−6.07% respectively. Plowing 20 cm and 25 cm deep increased the organic matter content in 20−30 cm soil layer. The plowing 25 cm treatment reduced available N and P contents in 0−10 cm soil layer, plowing 15 cm deep reduced the available P content in the 0−10 cm soil layer but increased the available potassium content.

     

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