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    坡度与种植年限对陡坡茶园土壤养分与可蚀性的影响

    Effects of slope and planting years on soil nutrients and erodibility in steep slope tea garden.

    • 摘要: 为探究陡坡茶园开发过程中的土壤质量变化特征,选取陕西省商南县规模化茶园为研究区,系统分析了不同坡度(10~40°)与种植年限(1~20年)对茶园土壤可蚀性及养分演变的影响。结果表明:(1)茶园土壤的铵态氮、速效磷、总氮和有机质随坡度增加而降低,与对照组相比,40°时茶园土壤的总氮与有机质分别显著降低了41.13%和66.67%,硝态氮在坡度>20°后显著下降了70.59%(P<0.05),40°坡度茶园砂粒占比达到最高,粘粒与粉粒含量下降,使土壤可蚀性较对照组(0°茶园)降低31.17%。(2)40°陡坡茶园中,新垦茶园因表土扰动且茶树养分吸收旺盛,5年茶园有机质含量下降并导致土壤可蚀性显著增加(P<0.05),随着种植年限延长(10~20年),植被覆盖度提高,根系活动和凋落物输入促使有机质含量提升28.31%,氮循环速率增加,土壤抗蚀性增强。(3)土壤可蚀性与粉粒、粘粒呈显著正相关(P<0.05),相关系数分别为0.94、0.84。与砂粒呈显著负相关(P<0.05),相关系数为0.94。表明细颗粒流失加剧养分失衡与结构劣化,而粗颗粒虽抑制侵蚀,但其是因细颗粒流失而形成,并且削弱了保水保肥能力。(4)陡坡茶园土壤质量呈现“初期退化-后期恢复”的阶段性特征,初期退化在40°新垦茶园表现的尤为突出,建议新垦期通过植被覆盖、排水措施、有机肥施用等措施以缓解土壤侵蚀和养分失衡风险。本研究可为陡坡茶园持续经营与水土资源协同调控提供依据。

       

      Abstract: To investigate the characteristics of soil quality changes during the development of steep-slope tea gardens, a large-scale tea garden in Shangnan County, Shaanxi Province, was selected as the study area. A systematic analysis was conducted to examine the effects of different slopes (10-40°) and planting durations (1-20 years) on soil erodibility and nutrient evolution in tea gardens. The results showed that: (1) The levels of ammonium nitrogen, available phosphorus, total nitrogen, and organic matter in tea garden soils decreased with increasing slope angle. Compared with the control group, the total nitrogen and organic matter in tea garden soils at a 40° slope angle decreased significantly by 41.13% and 66.67%, respectively. nitrate nitrogen decreased significantly by 70.59% (P &lt; 0.05) at slopes greater than 20°, and the sand particle content reached its highest level at a 40° slope, while clay and silt content decreased, resulting in soil erodibility being 31.17% lower than the control group (0° tea garden). (2) In the 40° steep slope tea garden, newly cultivated tea gardens experienced soil erosion due to topsoil disturbance and vigorous nutrient absorption by tea plants, resulting in a decrease in organic matter content and a significant increase in soil erosion potential (P &lt; 0.05) over five years. As planting duration increased (10-20 years), vegetation cover improved, root activity and litter input promoted a 28.31% increase in organic matter content, nitrogen cycling rates increased, and soil erosion resistance strengthened. (3) Soil erodibility showed a significant positive correlation with silt and clay particles (P &lt; 0.05), with correlation coefficients of 0.94 and 0.84, respectively. It also showed a significant negative correlation with sand particles (P &lt; 0.05), with a correlation coefficient of 0.94. This indicates that the loss of fine particles exacerbates nutrient imbalance and structural degradation, while coarse particles, though inhibiting erosion, they are formed due to the loss of fine particles and weaken water and nutrient retention capacity. (4) Soil quality in steep-slope tea gardens exhibits a phased characteristic of “initial degradation followed by later recovery,” with initial degradation being particularly pronounced in newly cultivated tea gardens with a slope of 40°. It is recommended that during the initial cultivation period, measures such as vegetation coverage, drainage measures, and application of organic fertilizers be implemented to mitigate the risks of soil erosion and nutrient imbalance. This study provides a basis for the sustainable management of steep-slope tea gardens and the coordinated regulation of water and soil resources.

       

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