长江流域径流模拟及其对极端降雨的响应

研究流域径流量变化可为水资源科学调配、利用开发、水旱灾害防治、水环境污染整治和国民经济可持续发展等提供重要依据.但近年来受全球变暖影响,极端气候事件,尤其是极端降雨的发生频率和强度出现了变化,直接或间接影响径流量变化.运用SWAT模型模拟1965~2019年间长江流域径流时空变化规律,分析了不同极端降雨条件下径流对降雨的响应.结果表明,1965~2019年间长江流域径流变化并不显著,流域总径流和中下游径流均经历了"枯-丰-枯-丰"4个阶段.极端降雨情景模拟发现,50 a一遇极端降雨下,长江上、中和下游代表性子流域日均径流变化率分别为6200%、21%和15%,月均径流变化率为355%、5%和1.3%,年均变化率为78%、1%和0.24%.而100 a一遇极端降雨下,3个子流域日均径流变化率分别为8000%、25%和17%,月均径流变化率为437%、7%和1.5%,年均变化率为96%、1.2%和0.28%.研究结果可为流域水资源管理和利用及洪涝灾害预测与防控等提供理论依据.     

Quality of roof runoff waters from an urban region (Gda sk, Poland)

The paper presents the results of testing of roof runoff waters from buildings in the city of Gda sk (Poland), carried out as a part of a broader research project aimed at the determination of pollutant levels in precipitation. The analytes determined included volatile organohalogen compounds, petroleum hydrocarbons, Na⁺, K⁺, NH₄⁺, Mg²⁺, Ca²⁺, F⁻, Cl⁻, NO₂⁻, NO₃⁻, PO₄³⁻, SO₄²⁻ ions, as well as organonitrogen, organophosphorus and organochlorine pesticides. In addition, the toxicity and pH of the samples were examined. The samples were collected over a period of six months, during or immediately following precipitation events. More than half of the samples (25) were found to be toxic, with inhibition exceeding 20%. The toxicity was weakly correlated to the levels of organonitrogen and organophosphorus pesticides in runoff waters. It was established that at least in some cases the roofing material affected the levels of the pollutants found in the samples.     

Strategies for determining soil-loss tolerance

Excessive soil losses due to erosion or lateral displacement by machinery impair productivity. Some soil loss is tolerable, but not so much that plant productivity diminishes. Thus productivity is the dominant concern in determining soil-loss tolerance. The effects of soil loss on productivity, however, are difficult to determine. Therefore, two alternatives are discussed for determining the limits of soil loss, or soil-loss tolerance. These alternatives are the maintenance of soil organic matter and, for shallow and moderately deep soils, the maintenance of soil depth. They are not new strategies, but our rapidly increasing knowledge of the dynamics of soil organic matter and the rates of soil formation from bedrock or consolidated sediments warrants the reconsideration of these alternatives. Reductions in either soil organic matter or the depth of shallow or moderately deep soils will lead to declining productivity. Soil organic matter, considered to be a surrogate for productivity, is much easier to monitor than is productivity. Also, there are many computer models for predicting the effects of management on soil organic matter. Recently compiled data on rates of soil formation suggest that soil losses of 1 t/a (2.24 Mg/ha yr) are greater than the rate of replenishment by the weathering of lithic or paralithic material in all but very wet climates.     

THE IMPORTANCE OF ACCURATE CURVE NUMBERS IN THE ESTIMATION OF STORM RUNOFF1

ABSTRACT: Storm runoff as calculated by the runoff curve number method is shown to be of varying sensitivity to both input rainfall and curve number. Using an assumed input error of 10%, a runoff error chart is given. Up to about 9 inches of rainfall, runoff is more sensitive to curve number than to rainfall. The importance of accurate curve number selection in this range is stressed.     

电解浮选用于活性污泥固液分离的研究

在装有Ti/RuO₂-IrO₂-TiO₂阳极、Ti阴极的电解浮选槽中进行了活性污泥固液分离的研究.考察了影响电解浮选性能的操作参数,这些参数包括水力停留时间、电流密度、进水SS浓度和进水pH值.研究表明,电解浮选是高效的固液分离单元,水力停留时间和电流密度是主要的影响因素.SS的去除率随着水力停留时间和电流密度的增加而增大;污泥负荷增加,SS的去除率下降;pH值影响电解产生微气泡的尺寸和污泥性质,但对SS的去除影响不大,实际应用中可以不调节pH值.进水SS约1 000mg/L时,当水力停留时间为20min,接触室电流密度为5 mA/cm²,分离区电流密度为2.5 mA/cm²,SS的去除率可达97%以上,此时的能耗为0.4～0.5(kW.h)/m³废水.电解浮选产生的浮渣含水率为95.9%,低于溶气气浮和二沉池的污泥含水率,对污泥减量化及其最终处置有较大的意义.     

浅谈青岛市雨水径流污染与控制措施

随着城市化的发展,水资源的污染和匮乏已经成为人们普遍关注的问题,而由此引出的对雨水径流污染的研究和控制也已不是新鲜话题。尤其对于将要承办2008年奥运会水上项目的青岛来说雨水的意义尤为重要。在对青岛市雨水水质实地调查后,结合国内外雨水研究的先进经验,对青岛市今后的雨水污染控制和利用提出了一些建议和意见。     

膜吸收器吸收CO2的影响因素研究

采用聚丙烯中空纤维膜吸收器,用水、NaOH和K2CO3 水溶液作为吸收剂进行高浓度CO2 吸收试验,考察了气体流率、吸收剂流率、质量分数以及流动方式对吸收率、传质系数和传质速率的影响.结果表明,随着气体流率增大,CO2的吸收率递减,总传质系数和总传质速率增加.在一定的气体流率下,吸收液流率增大,CO2的吸收率、总传质系数和总传质速率增大;吸收液浓度提高,吸收率增大,总传质系数和总传质速率提高.在气体流率较低时,质量分数为5%和8%的NaOH水溶液为吸收剂时的吸收率、总传质系数和总传质速率比较接近.随着气体流率增大,NaOH质量分数为8%时的吸收率、总传质系数和总传质速率增加的值大大超过NaOH质量分数为5%时增加的值.以水为吸收剂时,气体与吸收剂的流动方式为逆流时的吸收率、总传质系数和总传质速率高于并流时的值.     

Influence of super-absorbent polymer on the growth rate of gas hydrate

The growth rate of hydrate and morphology of methane hydrate formation were studied in a visual pressure cell at 5.5 MPa. The gas hydrate formation was carried out (coal mine methane (CMM) + tetrahydrofuran (THF) + sodium dodecyl sulphate (SDS) + H₂O) with and without SAP. Experimental data on the hydrate growth rate and induction time were obtained for three different CMM samples. The influence of SAP on hydrate growth rate was determined. Results showed that after the addition of SAP, with the methane concentration increased in CMM, the induction time was reduced by 9 min, 10 min and 3 min, and the growth rate was shortened by 0.56 × 10⁻⁶/m³ min⁻¹, 0.53 × 10⁻⁶/m³ min⁻¹ and 1.42 × 10⁻⁶/m³ min⁻¹, respectively. This study could be useful for the recovery of methane from CMM by forming hydrate in the chemical and mining industry.     

黄土区陡坡侵蚀过程试验研究

通过室内放水冲刷试验,结果表明,陡坡单宽径流能耗与单宽径流产沙率之间存在以下线性关系:Dr=18.672(ΔE - 0.751),说明土壤的可蚀性参数为18.672 g/J,发生坡面细沟侵蚀的临界径流能耗为0.751 J/(ms)。坡面单宽径流能耗随流量增大而增加,随坡度变化呈抛物线趋势,临界坡度出现在21和24之间。坡面上各段面单宽径流能耗均随流量的增大而增加,随着坡度逐渐增加,坡面上部段面能耗渐增,中部段面渐减,下部较稳定。坡面各段面侵蚀产沙也有类似特征。此研究对于深入了解黄土高原陡坡土壤侵蚀过程和机理具有重要意义。     

官厅流域农田地表径流磷流失初探

农田径流和侵蚀泥沙是磷进入官厅水库的主要非点污染源。针对该流域夏季农田暴雨径流发生的典型情景进行模拟降雨径流试验，对该流域农田地表径流泥沙和磷流失进行了初步的研究，结果表明，本降雨过程径流累积泥沙产量为30．5l～2493．34g／m^2，受雨强、坡度和作物覆盖的影响明显；径流溶解态磷(DP)中绝大部分是生物可利用性磷(DRP)，径流平均DP、DRP浓度都远大于水体允许临界值0．02mg／L，对官厅水体存在直接污染危害。径流累积全磷(TP)流失达O．0439～2．0798g/m^2；估算的流域农田径流全磷(TP)流失水平达2．67kg／(hm^2．a)以上，其颗粒态占969，0以上，可能成为官厅水库浮游生物长期丰富的潜在可利用磷源。降低农田土壤速效磷水平、减少水土侵蚀，是控制库区水华季节性发生和复原库区水体富营养化状态的关键。