中国冰雪资源高质量开发：理论审视、实践转向与挑战应对

推动冰雪资源高质量开发,是实现联合国可持续发展目标的新路径与新模式,是践行“两山理论”的重要环节,也是落实全民健身国家战略、助力体育强国建设的重要手段。在实际建设的理论指导层面,社会学所倡导的幸福感理论明确了冰雪资源高质量开发的终极目标,资源经济学的资源价值理论为冰雪资源的价值认识及价格核算提供了科学工具,地理学的人地关系理论是探究空间分异规律及人地系统耦合路径的理论基石。基于我国冰雪资源开发实践的系列转变及现实挑战,提出我国冰雪资源高质量开发的实现路径,即坚持观念创新的发展方式、多重协调的发展要求、积极开放的发展理念以及主客共赢的发展目标。     

HYDROCLIMATIC VARIABILITY IN THE ROCKY MOUNTAINS1

ABSTRACT: The spatial and temporal variability of hydroclimatic elements were investigated in the central and northern Rocky Mountains (Colorado, Idaho, Montana, Utah, and Wyoming) during the 1951–1985 period. The three hydroclimatic elements studied were total water-year (October 1-September 30) streamflow (ST), winter (October 1-March 31) accumulated precipitation (PR), and April 1 snowpack (SN). An analysis of 14 virgin watersheds showed wide spatial djfferences in the temporal variability of SN, PR, and ST, and these were found to be caused largely by basin exposure to moist air flows. The more stable (low variability) basins were those exposed to prevailing northerly to westerly flow, while unstable (high variability) basins were exposed to occasional southwesterly to southeasterly moist flow. Snowpack was the better indicator of ST in 11 of the 14 watersheds, explaining 37 to 87 percent of the ST variance. Analysis of the spatial variability, based on all SN and PR data from across the study area, revealed 11 discrete climatic regions. Both SN and PR exhibited coherent regions of stable and unstable temporal variability. The average variability between stable and unstable regions differed by a factor of two, and the differences were best explained by the exposure of the mountain barrier to moist air flows.     

MINIMIZING THE IMPACT OF URBANIZATION ON LONG TERM RUNOFF1

Increasing concern about the problems caused by urban sprawl has encouraged development and implementation of smart growth approaches to land use management. One of the goals of smart growth is water resources protection, in particular minimizing the runoff impact of urbanization. To investigate the magnitude of the potential benefits of land use planning for water resources protection, possible runoff impacts of historical and projected urbanization were estimated for two watersheds in Indiana and Michigan using a long term hydrological impact analysis model. An optimization component allowed selection of land use change placements that minimize runoff increase. Optimizing land use change placement would have reduced runoff increase by as much as 4.9 percent from 1973 to 1997 in the Indiana study watershed. For nonsprawl and sprawl scenarios in the Michigan watershed for 1978 to 2040, optimizing land use change placement would have reduced runoff increase by 12.3 percent and 20.5 percent, respectively. The work presented here illustrates both an approach to assessing the magnitude of the impact of smart growth and the significant potential scale of smart growth in moderating runoff changes that result from urbanization. The results of this study have significant implications for urban planning.     

三峡库区典型退耕还林模式土壤养分流失控制

选择三峡库区典型退耕还林模式,包括园地(茶园)及林地(板栗)与原有坡耕地对照,观测并分析其土壤养分(氮磷)输出途径及数量情况,以评估实施退耕还林工程对流域土壤养分输出的影响.结果表明:1退耕后土壤养分氮磷年流失量(包括随泥沙和地表径流流失的量)减少;总氮(TN)年输出量从大到小依次为坡耕地(2 444.27 g·hm-2)茶园地(998.70g·hm-2)板栗林地(532.61 g·hm-2);总磷(TP)为坡耕地(1 690.48 g·hm-2)茶园地(488.06 g·hm-2)板栗林地(129.00 g·hm-2);与坡耕地比较,退耕还林模式(园地、林地)总氮、总磷年输出载荷分别减少了68.68%和81.75%.2茶园地、板栗林地与坡耕地相比,土壤养分速效态氮流失量明显减少,硝态氮(NO-3-N)输出总量依次为坡耕地(113.79g·hm-2)茶园地(73.75 g·hm-2)板栗林地(56.06 g·hm-2);铵态氮(NH+4-N)养分输出次序为茶园最大(69.34 g·hm-2),坡耕地次之(52.45 g·hm-2),板栗林地最小(47.23 g·hm-2).3硝态氮、铵态氮主要通过地表径流输出,所占总量比例分别为91.4%和92.2%;总氮和总磷主要通过泥沙输出,所占总量比例分别为86.6%和98.4%.通过退耕还林等措施,该地区地表径流以及土壤侵蚀输出明显减少,土壤养分流失得到有效控制.     

路面径流生态阻控技术研究——以改性麦饭石透水沥青路面为例

为强化透水沥青路面对路面径流中氮、磷的控制效果,采用铁盐联合碱热技术制备了涂层负载改性麦饭石蓄水层集料,并运用场发射扫描电子显微镜(SEM)、能谱分析仪(EDS)和X射线衍射(XRD)等手段对改性后麦饭石集料的表面形态、特征和化学成分进行了表征.同时,通过静态吸附试验对TP的吸附效果及其作用机理进行了对比研究.最后将改性麦饭石作为蓄水层集料应用于透水沥青路面中,通过模拟降雨和周期蓄水试验探究其净化机制.结果表明:相比于天然麦饭石,铁盐联合碱改性麦饭石的表面性状发生了明显变化,最大饱和吸附容量明显提高,对氨氮和磷酸盐的吸附容量分别从1.32 mg·g~(-1)和1.48 mg·g~(-1)提升到12.82 mg·g~(-1)和6.38 mg·g~(-1);降雨全过程中改性蓄水层路面对NH~+_4-N的整体去除效率可提高20%左右,对TP的净化效率至少可提高15%,蓄水阶段较模拟降雨阶段污染物的去除效果显著提高,改性后麦饭石蓄水层24 h后的出水水质均可达III类水标准,强化蓄水层和提高蓄水时间是提高路面径流净化效率的有效措施.因此,本实验中铁盐联合碱热技术制备的改性麦饭石可推荐用于海绵城市生态处理设施透水沥青路面中削减氨氮和总磷的污染负荷.     

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.     

SNOW: NATURE'S RESERVOIR1

ABSTRACT: Snow, one of Nature's greatest reservoirs, supplies most of the usable water in the Western United States. Reliable predictions of the quantity and timing of the release of this water are used in making management decisions involving irrigation, stock water and municipal water supplies, hydro-power generation, recreation, navigation, and pollution control Practically oriented research is vital for the proper development and management of this resource. In southwestern Idaho, the Northwest Watershed Research Center, ARS, USDA, is conducting intensive investigations for assessing snow Volumes, snow water content, and snow-melt over a watershed. Application of these research findings will result in better development and management of the water stored as snow in Nature's reservoir.     

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.