原平市耕地土壤养分时空演变特征及影响因素

Spatiotemporal Evolution Characteristics and Influencing Factors of Cultivated Land Soil Nutrients in Yuanping County

  • 摘要:
    目的 明确原平市耕地土壤肥力时空演变特征并明确主要影响因素,为原平市耕地质量提升和科学施肥提供理论支持。
    方法 基于原平市1980年、2008年和2021年土壤有机质、全氮、有效磷和速效钾数据,采用改进的内梅罗指数法计算了土壤综合肥力指数;结合GIS和地统计学方法刻画了土壤肥力时空演变特征及主要影响因素;使用随机森林方法明确了不同年份的主控因素。
    结果 ① 1980 ~ 2021年间土壤肥力指数由0.76增加到1.24,土壤肥力整体得到大幅提升。② 41年间土壤有机质和全氮增幅明显,分别增加了5.67 g kg−1和0.45 g kg−1;有效磷含量由6.54 mg kg−1增加至13.8 mg kg−1;速效钾则呈现先减少后增加的趋势,由1980年的120.13 mg kg−1降低至2008年的97.12 mg kg−1,之后回升至1980年的水平。③ 1980 ~ 2008年间有35%的耕地有机质由五级提升至四级水平,约42%的耕地全氮由五级提升至四级水平;市域约53.9%的耕地有效磷由四级提升至三级水平,而有41%的耕地速效钾由三级降至四级水平。2008 ~ 2021年间约9.2%的耕地有机质由四级提升至三级水平,有9%的耕地全氮由四级提升至三级水平,均呈现于市域中部;有效磷水平在这一阶段无明显变化,而48%耕地速效钾由四级提升至三级水平。④ 1980年土壤肥力主控因素为土壤有效磷和速效钾,贡献率分别为32.1%和30.6%;2021年有效磷(27.9%)、速效钾(24.3%)、有机质(23.4%)和全氮(24.4%)对土壤肥力的贡献相近。
    结论 41年来原平市耕地土壤肥力大幅提升,86.2%的耕地由四级提升到三级水平,土壤肥力整体呈现“东西低中部高”的分布格局。中部的新原乡、中阳乡和沿沟乡部分耕地土壤全氮、有效磷与速效钾含量较1980年有所下降,主要是受种植结构变化和施肥比例的影响。今后应根据各乡镇种植结构变化制定施肥策略,均衡土壤养分,进而提升土壤肥力。

     

    Abstract:
    Objective The aim was to analyze the spatiotemporal evolution of cultivated land soil fertility in Yuanping County and identify the main influencing factors, in order to provide theoretical support for soil quality improvement and scientific fertilization.
    Method Data on soil organic matter (SOM), total nitrogen (TN), available phosphorus (AP), and available potassium (AK) from 1980, 2008 and 2021 in Yuanping County were used. The comprehensive soil fertility index (SFI) was calculated using an improved Nemerow index method. GIS and geostatistical methods were employed to characterize the spatiotemporal evolution of soil fertility and to identify its main influencing factors. A random forest model was used to determine the dominant control factors for different years.
    Result ① The comprehensive SFI index increased significantly from 0.76 in 1980 to 1.24 in 2021, indicating a substantial overall improvement in soil fertility. ② Over the 41-year period, SOM and TN increased markedly, rising by 5.67 g kg1 and 0.45 g kg1. AP increased from 6.54 mg kg1 to 13.8 mg kg1. AK showed an initial decrease followed by an increase, dropping from 120.13 mg kg1 in 1980 to 97.12 mg kg1 in 2008, and then recovering to the level in 1980. ③ From 1980 to 2008, SOM and TN increased significantly in all areas except for the eastern cultivated land. SOM in approximately 35% of the cultivated land increased from level V to level IV, and TN in about 42% of them promoted from level V to level IV. Approximately 53.9% of the cultivated land in the city improved its AP from level IV to level III, while 41% of them experienced a decrease in AK from level III to level IV. Between 2008 and 2021, about 9.2% of cultivated land showed an improvement in SOM from level IV to level III, and 9% of them showed an improvement in TN from level IV to level III, both primarily located in the central part of the county. AP levels showed no significant change during this period, but 48% of the cultivated land showed an increase in AK from level IV to level III. ④ In 1980, the dominant factors controlling soil fertility were AP and AK, with contribution rates of 32.1% and 30.6%. By 2021, the contribution rates of AP (27.9%), AK (24.3%), SOM (23.4%), and TN (24.4%) to soil fertility were similar.
    Conclusion Over the past 41 years, the soil fertility of cultivated land in Yuanping County had significantly improved, with 86.2% of the cultivated land improving from level IV to level III. The overall spatial distribution of soil fertility showed a "low in the east and west, high in the central region" pattern. In some parts of Xinyuan, Zhongyang, and Yangou townships in the central region, the content of TN, AP and AK had decreased compared to 1980, primarily due to changing in planting structure and fertilization ratios. Therefore, the future fertilization strategies should be tailored to the planting structure changing in each township to balance soil nutrients and further improving soil fertility.

     

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