CAJ | 학술논문

以典型草原区大型露天煤矿排土场边坡不同治理措施为研究对象，利用标准径流场定位观测设施对不同治理措施植被生长-枯萎期间的次降雨产流产沙过程进行了连续观测，研究结果表明：在边坡植被恢复初期，由于实施治理措施对边坡的强烈扰动，不合理的治理措施导致边坡的土壤侵蚀量大于裸地；当植被盖度大于＞35%时，不同治理措施的拦沙、蓄水、入渗能力明显强于裸地；降雨强度与降雨量是边坡产流产沙的主控因子，随着降雨强度和降雨量的增加而增加；裸露边坡的土壤侵蚀模数最大，为14183 t/(km2·a)，生态袋一字型布设措施的土壤侵蚀模数最小，为5179 t/(km2·a)；生态袋一字型布设措施的土壤侵蚀模数是裸露边坡的36.5%，是沙地柏+绣线菊灌丛（植被恢复4 a）的81.5%。可见，排土场边坡是一种极强烈侵蚀的人工再塑地貌，对其采用合理的生物措施+工程措施的治理措施要优于单纯的生物措施，是控制矿区排土场边坡土壤侵蚀的最有效途径之一。
이전형초원구대형로천매광배토장변파불동치리조시위연구대상，이용표준경류장정위관측설시대불동치리조시식피생장-고위기간적차강우산유산사과정진행료련속관측，연구결과표명：재변파식피회복초기，유우실시치리조시대변파적강렬우동，불합리적치리조시도치변파적토양침식량대우라지；당식피개도대우＞35%시，불동치리조시적란사、축수、입삼능력명현강우라지；강우강도여강우량시변파산유산사적주공인자，수착강우강도화강우량적증가이증가；라로변파적토양침식모수최대，위14183 t/(km2·a)，생태대일자형포설조시적토양침식모수최소，위5179 t/(km2·a)；생태대일자형포설조시적토양침식모수시라로변파적36.5%，시사지백+수선국관총（식피회복4 a）적81.5%。가견，배토장변파시일충겁강렬침식적인공재소지모，대기채용합리적생물조시+공정조시적치리조시요우우단순적생물조시，시공제광구배토장변파토양침식적최유효도경지일。
Due to the natural factors and the irrational actions of human being, grassland ecological environment is very vulnerable. Though the resource exploitation in recent years has greatly accelerated the economic and social development, a series of ecological environmental disasters are brought up, and the soil erosion is aggravated at the same time. Environmental problem has become one of the most important issues which need to be resolved urgently in China's economic and social development. Therefore, this paper takes the different measures of dump slope at large opencast coal mine in typical steppe as the study object, the process of runoff and sediment yield was positionally observed by using the standard runoff field facility under different control measures in the vegetation growth stage. The results showed that the amount of soil erosion in the slope caused by unreasonable measures was greater than the bare land in the early stage of vegetation restoration on the slope, which indicated the strong disturbance from the implementation of management measures on the slope. If the vegetation coverage was greater than 35%, the capacity of sediment, water storage and infiltration of the slope under different measures were obviously stronger than the bare land. The rainfall and rainfall intensity were the main controlling factors of slope runoff and sediment yield, which was increased with the increasing of the rainfall intensity and rainfall. Erosion modulus of the bare slope was 14183 t/(km2·a), which was biggest among the treated slopes. Soil erosion modulus under the measure of the eco-bags with linear shape was 5179 t/(km2·a), which was the minimum among the treated slopes. It was 36.5% of the bare slope and 81.5% of Sabina vulgaris +Spiraea shrub (after 4-year restoration). So, the dump slope is a kind of artificial remodeling topography with very strong erosion. The effect of combining biological measures and engineering measures was much better than the single biological measure to control the soil erosion in the dump slope, and it was one of the most effective ways to control the soil erosion in the dump slope. In summary, by setting up different control measures on the mine slope, the surface water and sediment changes are observed during individual rainfall so as to clarify the dynamic rule among rainfall, runoff and sediment yield change. The result obtained may provide certain reference for the erosion control of typical steppe mine slope and its ecological restoration and reconstruction.