• ISSN 1008-505X
  • CN 11-3996/S

红壤丘陵区稻田土壤剖面肥力特征及其与产量的关系

The profile fertility characteristics of paddy fields and their relationship with yields in red soil hilly region

  • 摘要:
    目的 探究不同产量稻田土壤肥力的剖面特征,明确调控作物产量的关键环境因子,以提高低产田、稳定高产田的粮食产量,实现“藏粮于地”的国家战略目标。
    方法 试验在江西进贤进行,稻田年产量>15000 kg/hm2、12000~15000 kg/hm2和<10000 kg/hm2的地块分别代表高产、中产和低产土壤,选取高、中、低产量稻田样点各3个,采集耕作层、犁底层和潴育层土壤样品,测定耕作层厚度、容重、土壤紧实度、pH、阳离子交换量(CEC)、有机质含量、全量和有效氮磷钾含量、微生物生物量碳 (MBC) 和氮 (MBN) 等,并对土壤剖面性质和水稻产量进行线性相关分析和随机森林分析。
    结果 1)高产田耕作层最厚,在16 cm左右,而低产田在13 cm左右,高产田耕作层土壤容重最小,为1.09 g/cm3,而低产田为1.21 g/cm3,高产田犁底层厚度和紧实度均最高,低产田最低。2)高、中、低产田土壤pH、碳氮磷养分含量和微生物生物量均表现为高产田>中产田>低产田,在土壤剖面上具有明显的“表聚”特征。高产田耕作层土壤有机质、全氮、有效氮、全磷和有效磷含量分别为38.82 g/kg、2.33 g/kg、198.54 mg/kg、0.81 g/kg和33.04 mg/kg,而低产田耕作层分别为29.75 g/kg、1.89 g/kg、158.71 mg/kg、0.62 g/kg和23.51 mg/kg。高产田耕作层土壤MBC和MBN含量分别为929.2、42.5 mg/kg,而低产田分别为533.6、30.8 mg/kg。3)在3个产量水平稻田土壤中钾素含量均随土层深度增加而增加,在低产田表现尤其明显,低产田耕作层全钾含量为8.12 g/kg,但母质层为10.77 g/kg。4)相关性分析和随机森林分析结果表明,水稻产量与耕作层土壤pH、有机质、全量和有效氮磷钾含量、微生物生物量碳氮以及微生物生物量碳氮比、耕作层厚度均呈显著正相关,这些变量可以解释水稻产量变化的53.7%,其中,微生物生物量碳、微生物生物量碳氮比和耕作层厚度是影响作物产量最重要的环境因素,其解释能力分别为9.2%、8.7%和7.9%。
    结论 耕作层厚度和耕作层微生物生物量是调控水稻产量的关键环境因素。相比低产田,高中产田耕作层厚,耕作层土壤容重低、有机质含量高,供肥保肥能力强。因此,增加耕作层厚度和提高微生物生物量是改良中、低产田的关键。

     

    Abstract:
    Objectives Red paddy soils are important cultivated land resources for the food safety of China, however, the large proportion of middle and low yield fields need improvement to take the responsibility. We compared the fertility variation characteristics across soil profiles in different yield levels, to propose the key points of low yield field improvement and serve the national strategic goal of “storing grain in the ground”.
    Methods The research was carried out in Jinxian County, Jiangxi Province. The paddy soils were divided into high-, middle- and low-yield fields according to annual rice yield of >15000 kg/hm2, 12000−15000 kg/hm2 and <10000 kg/hm2. At the three yield level fields, soil samples were collected on the arable layer, plough pan and waterlogged layer for measurement of layer depth, bulk density, penetration resistance, pH, cation exchange capacity (CEC), organic matter, total and available NPK, and microbial biomass carbon (MBC) and nitrogen (MBN). The relationship between soil profile properties and rice yield was analyzed using the linear correlation analysis and random forest analysis.
    Results In high and low yield fields, the plough layer depth is around 16 cm and 13 cm, soil bulk density was 1.09 g/cm3 and 1.21 g/cm3, respectively. The plough pan thickness and density were in descent order of high-, middle- and low-yield fields. The chemical properties of plough layer in high-yield fields are organic matter 38.82 g/kg, total N 2.33 g/kg, available N 198.54 mg/kg, total P 0.81 g/kg, available P 33.04 mg/kg, while those in low yield fields were 29.75 g/kg, 1.89 g/kg, 158.71 mg/kg, 0.62 g/kg, 23.51 mg/kg, respectively. The MBC and MBN of plough layer were 929.2 mg/kg and 42.5 mg/kg in high-yield fields, while those were 533.6 mg/kg and 30.8 mg/kg in low yield fields, respectively. The soil pH and the organic C, N, P, and microbial biomass showed obvious “surface aggregation” characteristics along soil profile, and declined with the yield from high to low level. However, the K content in all the tested fields increased with the soil profile down to deep, especially in low yield fields. The total K content was 8.12 g/kg in the plough layer, and increased to 10.77 g/kg in the parent material horizon. The results of correlation analysis and random forest analysis showed that rice yield was positively (P<0.05) correlated with the tested soil properties in plough layer, and these properties explained 53.7% of rice yield differences. Among them, MBC, MBC/MBN and plough layer depth were the most important factors affecting rice yield, with the explanatory power of 9.2%, 8.7% and 7.9%, respectively.
    Conclusions The thickness and the microbial biomass of the plough layer are the key environmental factors regulating rice yield. Compared with low-yield fields, high-yield fields have thicker plough layer with lighter bulk density and higher organic matter in it. So the key measurements for low-yield field improvement are the construction of thick and fertile plough layer.

     

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