农村生活污水与小流域水环境协同治理的规则型构——基于临沂“兰山模式”的实践样本

如何对农村地区的流域水环境进行高效而低成本的治理,是当前农村资源环境治理面临的挑战之一。本文以山东临沂市兰山区柳青河水环境污染治理作为典型案例,从规则型构视角剖析行动规则对"兰山模式"的作用机制。其中,边界规则打破了农村生活污水与小流域水环境资源治理的边界,企业等新行动主体的资金、技术的溢出效应提高了治理效率;身份规则改变了行动主体的参与动机,加强了多方主体间的交互作用;选择规则减少了多方治理主体的责任冲突;聚合规则弥补了农户在环境治理中的缺位。在四项行动规则的共同作用下,"兰山模式"实现了农村生活污水与小流域水环境的协同治理,是农村水环境治理的实践样本。

小流域水污染的主要成因与防治对策分析

我国近年来发展重心落在了经济建设,而忽略了对水资源的环境保护,导致当前小流域水污染问题随着工业化进程的加快日益严峻,对人类健康造成严重威胁,破坏了生态平衡。本文针对当前小流域水污染及治理现状进行分析,分别阐述了导致小流域水污染的工业废水、生活污水、农业污染物三个问题关键点,并从工程治理、生态治理以及管理治理等三个维度提出了小流域水污染的相应治理措施,从而提升小流域水污染治理效率。

面向生态保护的丘陵地区小流域水土保持

为实现对丘陵地区小流域水土问题的有效改善,提升我国生态保护工作效率,本文在GIS空间分析等技术与方法协助下,将某丘陵区的一小流域中的道路细化为I~IV级,结合小流域道路分布特点,对面向生态保护的丘陵地区小流域水土保护计划目标、原则及实施流程进行分析,希望对我国丘陵地区小流域水综合治理目标的实现有所助益。

两级AO生化工艺在离子型稀土矿山小流域尾水处理站的工程应用

针对常规生物脱氮工艺脱氮效率低的问题,赣州稀土矿业公司采取两级AO生化工艺处理离子型稀土矿山小流域氨氮尾水,进水水质氨氮100~150 mg/L,总氮150~200 mg/L,出水水质氨氮<10 mg/L,总氮<30 mg/L,达到GB 26451—2011排放标准,氨氮脱除率可达94.1%以上,总氮脱除率可达85.9%,大大提高了脱氮效率,实现了氨氮废水达标排放。工程实践表明,本工艺处理效果良好和运行稳定,具有较好的社会与生态效益。

北方水源区生态输水小流域治理模式探讨

在我国北方水源区,水土流失严重和水资源严重短缺是最主要的生态和社会问题,传统的小流域治理模式已不适应形势的发展,甚至阻碍区域经济社会的全面进步,其水土保持生态建设方略应是把流域上下游水资源优化配置,将全流域的水资源可持续利用作为今后水土流失治理的重要目标,建设生态输水小流域。生态输水小流域治理以生态补偿为前提,强调对小流域进行生态功能分区与定位,总体治理思路是集水区总体弱化治理、生产生活区强化治理、复合区适度治理,水土保持措施配置以最大限度地向下游输水、输好水为原则。

菏泗水小流域推行小庄园开发治理的成效与经验

十几年来 ,梅县在菏泗水小流域治理中 ,坚持以科技为先导 ,寓水土流失治理于经济开发之中 ,使山上的水土流失治理与农户山下的经济开发有机结合起来 ,创出了小庄园治理模式 ,不仅使广大农民从水土保持生态环境建设中得到了实惠 ,而且使水土保持工程的维护管理得到了切实落实 ,保证了水土保持生态建设的持续健康发展 ,取得了显著的社会。

陈湾水小流域果树梯田的设计与施工

介绍果树梯田施工方法以抽槽法为优 ,施工放样应遵循“大弯就势、小弯取直”的原则 ,因地制宜地进行并块和加块 ;排灌沟系统、道路、防护林三者应尽可结合布设 .

浅谈加快承德水土保持发展途径

从推进水功能涵养区建设和绿色经济发展出发,分析加强水土保持地位作用、探讨加快水土保持步伐的对策及措施。

Inter-annual variation of streamflow,precipitation and evaporation in a small humid watershed(Chengcun Basin,China)

For sustainable water resource management,it is important to determine the relationship between streamfl ow and other variables that infl uence availability of water resources.However,many catchments do not have suffi cient data to allow for a more detailed study of these relationships.We faced a similar challenge in the Chengcun Basin(limited historical data: from 1986–1999); and therefore we used a new approach to overcome this.We found that,using nonparametric trend methods in conjunction with the climate elasticity analyses and the 2D visualization of hydrologic data,it is possible to assess the relationships between streamfl ow and other hydro-climatic variables.In the past,streamfl ow trends in the basin were more correlated with precipitation than with potential evapotranspiration(PET).In addition,there is a gradual shift in the hydrological regime of the catchment,which may affect the occurrence of available water resources and activities that depend on them.In addition,based on our climate sensitivity analyses,the streamfl ow is dependent and more sensitive to variations in precipitation than to PET(δQ=0.79δP+0.42δE; precipitation elasticity,ε P=1.32; PET elasticity,ε E=-2.10).Therefore pending more detailed studies,the use of our approach will provide a rapid means to assess the variation of water resources(streamfl ow)in a watershed.In the future,we hope to carry out related research in other watersheds and also perform a more detailed studies to improve upon the results of this study.

Evaluation of the Quantity of Eroded Land in Mountains Watersheds of Vithkuqi Area （District of Korca）-Albania

Soil erosion represents one of the most important destructive phenomenon of the soil, through surface and depth erosion. The activity of water erosion in Albania is favoured from some factors like relief, geological structure, slope, soil, etc. Erosion depth growth is closely related with the vegetal cover ravage high rate and in the first instance that of woodland flora in sloping ground. The degradation of the flora or total destruction of it is defined from many factors, but in notably from social-economical system of every country. It can be also seen some special areas in our country were the results of the human negative impacts in natural environment. The erosion phenomenon is more problematic, especially during intensive raining time.

Cu behaviors and effects of mine drainage in Kosaka River,Hokuroku mining district,Northeast Japan

Focusing on the origin of the heavy metal,this study aims to build an imputed method to estimate the heavy metal content in river water by making a distinction between the heavy metal of natural origins and that caused by human activities.Supported by GIS,Kosaka watershed within the Hokuroku basin was divided into several sub-watershed polygons and the outflows of water and Cu were calculated for each polygon.Compared with the natural origin,the dominant Cu emissions affected the river water more significantly in local.Based on the mass balance closure,the heavy metal content of Cu in the Kosaka River was estimated by the conflux accumulation of tributaries and mine drainages.The estimated Cu concentrations were checked by comparing with the actually measured values at monitoring points along the Kosaka River and the results are coincidence with each other in general.It is revealed that the mainstream water quality could be estimated by seizing the water quality of upstream tributaries and human drainages.

Spatiotemporal Variation of Riverine Nutrients in a Typical Hilly Watershed in Southeast China Using Multivariate Statistics Tools

The water quality of lakes can be degraded by excessive riverine nutrients.Riverine water quality generally varies depending on region and season because of the spatiotemporal variations in natural factors and anthropogenic activities.Monthly water quality measurements of eight water quality variables were analyzed for two years at 16 sites of the Tianmuhu watershed.The variables were examined using hierarchical cluster analysis(HCA) and factor analysis/principal component analysis(FA/PCA) to reveal the spatiotemporal variations in riverine nutrients and to identify their potential sources.HCA revealed three geographical groups and three periods.Two drainages comprising towns and large villages were the most polluted, six drainages comprising widely distributed tea plantations and orchards were moderately polluted, and eight drainages without the factors were the least polluted.The river was most polluted in June when the first heavy rain(daily rainfall > 50 mm) occurs after fertilization and the number of rainy days is most(monthly number of rainy days > 20 days).Moderate pollution was observed from October to May, during which morethan 60% of the total nitrogen fertilizer and all of the phosphorus fertilizer are applied to the cropland, the total manure is applied to tea plantations and orchards, and a monthly rainfall ranging from 0 mm to 164 mm occurs.The remaining months were characterized by frequent raining(i.e., number of rainy days per month ranged from 5 to 24) and little use of fertilizers, and were thus least polluted.FA/PCA identified that the greatest pollution sources were the runoff from tea plantations and orchards,domestic pollution and the surface runoff from towns and villages, and rural sewage, which had extremely high contributions of riverine nitrogen, phosphorus,and chemical oxygen demand, respectively.The tea plantations and orchards promoted by the agricultural comprehensive development(ACD) were not environmentally friendly.Riverine nitrogen is a major water pollution parameter in hilly watersheds affected by ACD, and this parameter would not be reduced unless its loss load through the runoff from tea plantations and orchards is effectively controlled.

Stable Isotopes in Precipitation and Atmospheric Moisture of Pailugou Catchment in Northwestern China′s Qilian Mountains

Hydrogen and oxygen isotopes in precipitation have been widely used as effective traces to investigate hydrological processes such as evaporation and atmospheric moisture source. This study analyzed δD and δ^(18)O of precipitation in continuous event-based samples at three stations of Pailugou Catchment from November 2012 to December 2013. The δ^(18)O and δD values ranged from-32.32‰ to +3.23‰ and from-254.46‰ to +12.11‰, respectively. Results show that the δ^(18)O displayed a distinct seasonal variation, with enriched values occurring in summer and relatively depleted values in winter, respectively. There was a statistically significant positive correlation between the δ^(18)O and δD values and local surface air temperature at all the three stations. The nearest Global Network of Isotopes in Precipitation(GNIP) station(Zhangye), compared to the Meteoric Water Lines for this study, showed the obvious local evaporation effects with lower intercept and slope. Additionally, d-excess(δD- 8δ^(18)O) parameter in precipitation exhibited an anti-phase seasonal variability with the δ^(18)O. The 96-h back trajectories for each precipitation event using Hybrid Single Particle Lagrangian Integrated Trajectory(HYSPLIT) model indicated a dominant effect of westerly air masses in summer and the integrated influence of westerly and polar air masses in winter.

The Global Science of Integrated Water Governance

Abstract： This study discusses the benefits of establishing a broader discipline of water science, based on the organizing mechanism of PES-W （payments for ecosystem services on the watershed scale）. PES-W is derived from an extension of governance analyses of 163 watershed-based PES （payments for ecosystem services） programs, and from the integrative decision mechanism of IPES （integrated payments for ecosystem services） to generalize the PES approach. PES-W reflects three interrelated perspectives fundamental to the global science of integrated water governance： （1） the ecological and economic perspective to integrate human incentives for integrated water resources governance; （2） the sociological and ecological perspective to form partnerships for meta-monitoring and recta-funding for integrated watershed governance; and （3） the scientific and sociological perspective to develop organizing botmdaries based on technology, lifestyle, entrepreneurship and organizing infrastructure for integrated aquatic ecosystem governance. This study is intended to communicate with the international scientific communities for establishing an advanced, academic, and practical multidisciplinary field of the global science of integrated water governance as a critical condition for sustainable development in human societies.

Study of soil and water conservation Function on Slope with Different Planting Patterns for a Typical Small Watershed in Karst Region of Guizhou Province

Ten runoff plots with different planting patterns were established for experimental observation in Yangjichong small watershed of Longli County in Karst region of Guizhou Province. Results show that under the same rainfall condition, shrub land, natural grassland and abandoned land presented the best function of soil and water conservation. The function of soil and water conservation was poor for arbor planting pattern, because the shrub layer, herb layer and forest floor were not formed. Because of no-tillage, surface crust and other effects, the function of soil and water conservation in slope farmland was better than that in runoffplots with arbor planting pattern.

Study on Hydrography and Small-Scale Process over Zhoushan Sea Area

This paper mainly analyzes the tidal characteristics and small-scale mixing process near Zhoushan Islands. First, the spectral analysis and wavelet analysis are adopted for the measured tide level data and tidal current data from the Zhoushan sea area, which indicate that the main tidal cycle near Hulu Island and Taohua Island is semi-diurnal cycle, the diurnal cycle is subordinate. Both their intensities are changed periodically, meanwhile, the diurnal tide becomes stronger when semi-diurnal tide becomes weak. The intensity of baroclinie tidal current weakens at first and then strengthens from top to bottom. Then, in this paper, the Gregg-Henyey （G-H） parameterization method is adopted to calculate the turbulent kinetic energy dissipation rate based on the measured temperature and tidal current data. The results of which shown that the turbulent kinetic energy dissipation rate around Hulu Island is higher than that around Taohua Island. In most cases, the turbulent kinetic energy dissipation rate during spring tide is larger than that during the neap tide; the turbulent kinetic energy dissipation rate in the surface layer and the bottom layer are higher than that in the intermediate water; the changes of turbulent kinetic energy dissipation rate and tidal current are basically synchronous The modeled turbulent kinetic energy dissipation rate gets smaller with the increase of the stratification, however, gets larger with the increase of shearing.

Characterization of the Constructions Materials Used in the Hydroelectric Power Plants in the Sedano＇s Valley, Burgos （Spain）

Small hydropower plants for electricity generation were first built in Spain in the early 1880s. The Spanish peninsula is characterized by its rugged landscape, fast flowing rivers and steep gradients. A clear example of this is the remarkable area of the upper Ebro river basin where powerful water flows are found that are ideal for electricity generation. Between 1900 and 1930, the river Ebro was a major source of energy for industrial areas such as Alava, Vizcaya, Vitoria, Miranda de Ebro, Burgos and La Rioja. Between 1951-1965, the use of these small hydropower plants declined due to the construction of alternatives by industrialists in the Basque Country, which in most cases led to their deterioration. They were rescued in the late twentieth century, thanks to private sector initiatives which funded their rehabilitation. This study examines two small-scale hydraulic power plants in the province of Burgos at Medina de Pomar and at Quintanilla Escalada; both buildings were used for generating electricity and had living quarters for the workers and now represent historic architectonic and industrial heritage. The study documents their architectonic features and the restoration processes that have permitted one of them to remain in operation up until the present day.

Geochemical tracing and modeling of surface and deep water–rock interactions in elementary granitic watersheds(Strengbach and Ringelbach CZOs, France)

From the study of the Strengbach and Ringelbach watersheds we propose to illustrate the interest of combining the geochemical tracing and geochemical modeling approaches on surface and deep borehole waters,to decipher the diversity of the water flow and the associated water–rock interactions in such elementary mountainous catchments. The results point to a clear geochemical typology of waters depending on the water circulations(deep vs. hypodermic) within the substratum.

Soil Erosion and Sediment Control Effects in the Three Gorges Reservoir Region, China

The Three Gorges Reservoir, the world’s largest hydropower reservoir, receives a significant sediment yield from soil erosion. Sloping farmland is the main source, exacerbated by changes in land use from relocating the inhabitants, and from engineering projects related to dam construction. Related geo-hazards, including landsliding of valley-side slopes, will further increase the sediment yield to the completed reservoir. Integrated watershed management, begun extensively in 1989, has effectively controlled soil erosion and sediment delivery to date. What is described here as the Taipinxi Mode of integrated watershed management, based on its application in the 26.14 km2 watershed of that name in Yiling District, has been successful and is recommended for the entire region. The effects of this set of erosion-mitigation measures are assessed, using experienced formulas for soil and water conservation and information from remote sensing. The amount of soil erosion, and of sediment delivery to the reservoir were reduced by 43.75–45.94 × 106 t y-1, and by 12.25–12.86 × 106 t y-1, respectively, by 2005, by which time the project had been operative for 16 years.

Effect of Drainage Ditch Layout on Nitrogen Loss by Runoff from an Agricultural Watershed

A comparison experiment was performed, by designing one field ditch （D1 treatment）, two field ditches （D2 treatment）, three field ditches （D3 treatment）, and no field ditch （CK treatment）, in an upland of a small agricultural watershed in Nanjing-Zhenjiang hilly regions to observe the farmland surface runoff and N loss characteristics under the different layouts of field ditch. As the layout density of field ditch increased, the drainage effect was improved, the timing of the runoff peak was advanced, and also the peak flow was augmented. At the same time, both the concentration and accumulated transfer flux of total nitrogen （TN） were improved, and thereinto the accumulated transfer fluxes of TN under D3, D2 and D1 treatments were increased by 1.46, 1.34 and 1.16 times, respectively, than that under CK treatment. However, the accumulated transfer fluxes of nitrate-nitrogen （NO3-N） and ammonium-nitrogen （NH4＋-N） under D3, D2 and D1 treatments were reduced by 33.9%, 21.4% and 8.6%, and 35.8%, 24.7% and 12.2%, respectively, compared with those under CK treatment. Under CK treatment, the NO3-N and NH4＋-N concentrations were more sensitive to rainfall intensity than the TN concentration. There were significant linear relationships between the transfer fluxes of TN, NO3-N and NH^-N and the runoff flux, with the correlation coefficients of 0.942, 0.899 and 0.912, respectively. In addition, this correlation was also influenced by the layout density of field ditch. Therefore, the environmental effect should be taken into account when designing and constructing field ditches. Especially in the regions of severe fertilizer loss, the approaches of properly increasing the drainage area and decreasing the layout density of field ditch could be adopted under the precondition of avoiding crops from waterlogging.