模拟降雨下坡长对矿山坡面水土与氮磷流失的影响

Effects of Slope Length on Soil and Water Loss, as Well as Nitrogen-Phosphorus Loss from Mining Slopes Under Simulated Rainfall

  • 摘要:
    目的 为探究坡长对矿山坡面水土侵蚀及氮磷流失特征的影响,实现对矿区坡面土壤养分流失的预测,并为制定矿山水土流失防治措施提供理论依据。
    方法 通过室内人工模拟降雨的方法,分析在相同坡度及降雨强度下3种坡长(2 m、3 m、4.5 m)对矿山坡面产流、产沙及氮磷流失特征的影响,并构建“氮磷养分流失速率-产流速率/产沙速率”预测方程。
    结果 ① 4.5 m和3 m坡长较比2 m坡长初始产流所用时间分别提早了51.2%和18.6%,坡长与坡面初始产流时间呈现负相关关系。② 3 m和4.5 m坡长产流量较比2 m坡长增加了1.56和2.47倍,各坡面累计产流量均随降雨时间的增加而呈现幂函数趋势增加。3 m和4.5 m坡长产沙量较比2 m坡长增幅为2.17和2.73倍,各坡面累计产沙量均随降雨时间呈显著正相关关系。③径流总磷(TP)流失量仅占坡面总流失量的6% ~ 7%,坡面土壤中的磷素主要通过泥沙流失。坡面径流中总氮(TN)流失量是泥沙中的1.05 ~ 2.04倍,坡面土壤中氮素主要以坡面径流流失。④坡面氮、磷养分流失速率-产流速率预测方程LTP = 0.137R + 0.072(R2 = 0.821) ,LTN = 2.869R +5.38(R2 = 0.731);氮、磷养分流失率-产沙率预测方程DTP = 2.132E + 0.392(R2 = 0.804),DTN = 0.981E + 0.446(R2 = 0.795)。
    结论 在降雨强度为80 mm h−1、坡度10°时,缩短坡长在一定程度上会减少矿山坡面水土和氮磷养分流失量,且坡面土壤氮磷流失速率和坡面产流、产沙速率呈显著正相关关系,预测方程可以通过坡面产流速率和产沙速率有效地预测坡长单因子的氮磷流失量。

     

    Abstract:
    Objective This study aimed to explore the effects of slope length on soil and water erosion and nitrogen-phosphorus (N-P) loss characteristics on mining slopes, in order to predict soil nutrient loss on mining slopes and provide a theoretical basis for formulating measures to prevent and control soil and water erosion in mining areas.
    Methods The effects of three types of slope lengths (2 m, 3 m and 4.5 m) on the flow, sand and nitrogen (N) and phosphorus (P) loss characteristics of mine slopes under the same slope gradient and rainfall intensity were analyzed by simulating rainfall artificially and constructing a prediction equation of “N and P nutrient loss rate - flow rate/sand production rate”.
    Results ① Compared to the 2 m slope, the initial runoff time for the 4.5 m and 3 m slopes was advanced by 51.2% and 18.6%, which indicates a negative correlation between slope length and initial runoff time. ② The runoff yield at 3 m and 4.5 m slope lengths increased by 1.56 and 2.47 times compared with the 2 m slope length. The cumulative runoff yield on each slope showed a power function trend of increase with the increase of rainfall duration. The sediment yield at 3 m and 4.5 m slope lengths increased by 2.17 and 2.73 times compared with the 2 m slope length. The cumulative sediment yield on each slope showed a significant positive correlation with rainfall duration. ③ Total P (TP) loss via runoff accounted for only 6% - 7% of the total TP loss, indicating that P was primarily transported through sediment. In contrast, total N (TN) loss via runoff was 1.05 - 2.04 times higher than that via sediment, suggesting N predominantly migrated through runoff. ④ The predictive equations for the rate of N and P nutrient loss rate-production rate on the slope surface were: LTP = 0.137R + 0.072 (R2 = 0.821), LTN = 2.869R +5.38 (R2 = 0.731); N and P nutrient loss rate- sediment production rate prediction equation: DTP = 2.132E + 0.392 (R2 = 0.804), DTN = 0.981E + 0.446 (R2 = 0.795).
    Conclusion In the case of a rainfall intensity of 80 mm h−1 and a slope gradient of 10°, the shortening of the length of the slope will to a certain extent reduce the loss of soil, N and P nutrients from the slope face of the mining, the N and P loss rate from the soil and the slope face flow production, and the rate of sand production show a significant positive correlation. The prediction equation can effectively predict the N and P loss of single factor of slope length through the rate of slope flow and sand production.

     

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