PESTICIDES AND PESTICIDE DEGRADATION PRODUCTS IN STORMWATER RUNOFF: SACRAMENTO RWER BASIN,CALIFORNIA1

ABSTRACT: Pesticides in stormwater runoff, within the Sacramento River Basin, California, were assessed during a storm that occurred in January 1994. Two organophosphate insecticides (diazinon and methidathion), two carbamate pesticides (molinate and carbofuran), and one triazine herbicide (simazine) were detected. Organophosphate pesticide concentrations increased with the rising stage of the hydrographs; peak concentrations were measured near peak discharge. Diazinon oxon, a toxic degradation product of diazinon, made up approximately 1 to 3 percent of the diazinon load. The Feather River was the principal source of organophosphate pesticides to the Sacramento River during this storm. The concentrations of molinate and carbofuran, pesticides applied to rice fields during May and June, were relatively constant during and after the storm. Their presence in surface water was attributed to the flooding and subsequent drainage, as a management practice to degrade rice stubble prior to the next planting. A photo-degradation product of molinate, 4-keto molinate, was in all samples where molinate was detected and made up approximately 50 percent of the total molinate load. Simazine, a herbicide used in orchards and to control weeds along the roadways, was detected in the storm runoff, but it was not possible to differentiate the two sources of that pesticide to the Sacramento River.     

基于河网水系变化的水灾危险性评价——以永定河流域京津段为例

城市化过程中不合理的土地利用导致河道填塞、河网缩减现象普遍，城市水灾增加。基于灾害系统思想，构建了基于河网水系变化的水灾危险性评价体系，并以永定河京津段为例进行了实证分析。结果表明：（1）近40年来研究区水系结构简单化趋势明显，河道长度减少了20．5％，条数减少了36．4％，水系调蓄能力下降，在同样的致灾强度下水灾危险性加大；（2）在假设暴雨重现期为50年的条件下，经济密度差异决定了水灾潜在危险区的空间格局，居民用地将成为水灾重度危险区；平原段水灾重度危险区占5．7％，中度危险区占33．1％，滨海段重度危险区占13．9％，中度危险区占26．8％。研究结果可为区域综合减灾、水灾预报提供依据。     

Ⅱ824-2综放工作面瓦斯综合治理试验研究

通过对淮北芦岭矿Ⅱ824-2综放工作面瓦斯综合治理的试验研究,摸索出了高瓦斯综放工作面瓦斯治理的有效方法,取得了较好的瓦斯抽放和通风排放效果.     

玉米芯为碳源实现酸性矿山废水生物处理

引入了一种新的碳源——玉米芯，对SRB法处理酸性矿山废水进行了更加深入的探索，分析了各种参数条件对s暖一还原效果的影响，确定了常温下这种碳源所需要的最适宜工况条件，探讨了硫酸盐矿山废水的水质资源化问题，并对山西矿山废水的生物治理进行了可行性实验验证。实验证明，玉米芯为碳源时，矿山废水中SO^2-4的出水值可达221．1mg／L，金属离子的浓度也都达到了生活饮用水的质量标准，所以玉米芯可作为酸性矿山废水资源化生物处理的合适有效碳源。     

塔河流域森林生态建设存在的主要问题及其策略

随着时间的推移,塔河流域生态环境恶化的现实已被越来越多的人们所认识。造成塔河中下游森林退化,生态环境恶化的主要原因除自然因素外,主要是人为不合理的社会经济活动的影响。目前塔河流域森林生态建设存在的主要问题有:第一水资源不合理的利用成为沙漠化和次生盐渍化的主要原因;第二传统的生活方式和掠夺式的生产方式使生态环境遭到破坏;第三耕地的增加,满足不了人口发展的需求,大面积的无序开荒,导致生态环境进一步恶化。为塔河中下游林地植被恢复、建设及防止退化的策略有:塔河中下游生态工程治理的原则;塔河中下游生态环境治理的基本思路;塔河流域生态环境治理的主要对策,合理利用水资源,坚持生产、生态建设并重,确保生态用水;要积极调整农村产业结构,正确处理林业和农业、林业和牧业以及林业和工业发展的关系;大力发展农村能源建设,从根本上解决农村薪材和生态保护之间矛盾;大力保护、恢复、发展荒漠林草植被,大力发展绿洲林业,建立荒漠生态环境和绿洲共同支撑的稳定的生态体系;积极实施林业生态工程和林果工程,建立较为完备和发达的生态和产业体系。     

新疆和田河绿色走廊演变机制及生态环境保护初析

和田河绿色走廊是塔里木盆地中南北穿越塔克拉玛干沙漠的三条绿色走廊之一，具有重要的政治经济、生态、交通意义。绿色走廊的演变受到构造运动、气候波动和人为干扰等因素的影响。其中，人为干扰是绿色走廊现代生态环境演变过程中最重要最活跃的控制因素。建议加强流域水资源总体规划与统筹管理，兼顾生产、生活和生态用水，逐步改变农村居民燃料能源结构，从而保护绿色走廊生态健康。     

塔里木河下游绿色走廊的生态问题与治理对策

从经济、军事和生态三个角度分析了保护塔里木河下游绿色走廊的必要性,概括了该区域的生态环境现状,即河水矿化度升高、地下水位下降从而导致植被的退化和沙漠化加剧的问题。最后提出了以水资源合理利用为前提和中心的治理对策。     

塔里木河中游段治理中的牧区水利建设

塔里木河中下游地区生态环境急剧恶化,最主要的原因是中游段河水近一半21×108m3被人为的散失,造成下游河水所剩无几,致使尾闾台特玛湖干涸。解决的根本办法是将中下游段两岸的农牧民迁出,实现人为耗水为零。近期切实可行的办法是积极开展牧区水利建设,改变牧业生产方式,集中高效利用塔河水资源,发展人工草地,改良天然草场,实现牧业生产生态环境的协调发展,人与自然和谐相处。     

NUTRIENT CONCENTRATION CRITERIA AND CHARACTERIZATION OF PATTERNS IN TROPHIC STATE FOR RIVERS IN HETEROGENEOUS LANDSCAPES1

ABSTRACT: A method is demonstrated for the development of nutrient concentration criteria and large scale assessment of trophic state in environmentally heterogeneous landscapes. The method uses the River Environment Classification (REC) as a spatial framework to partition rivers according to differences in processes that control the accrual and loss of algae biomass. The method is then applied to gravel bed rivers with natural flow regimes that drain hilly watersheds in New Zealand's South Island. An existing model is used to characterize trophic state (in terms of chlorophyll a as a measure of maximum biomass) using nutrient concentration, which controls the rate of biomass accrual, and flood frequency, which controls biomass loss. Variation in flood frequency was partitioned into three classes, and flow data measured at 68 sites was used to show that the classes differ with respect to flood frequency. Variation in nutrient concentration was partitioned at smaller spatial scales by subdivision of higher level classes into seven classes. The median of flood frequency in each of the three higher level classes was used as a control variable in the model to provide spatially explicit nutrient concentration criteria by setting maximum chlorophyll a to reflect a desired trophic state. The median of mean monthly soluble reactive phosphorus and soluble inorganic nitrogen measured at 68 water quality monitoring sites were then used to characterize the trophic state of each of the seven lower level classes. The method models biomass and therefore allows variation in this response variable to provide options for trophic state and the associated nutrient concentrations to achieve these. Thus it is less deterministic than using reference site water quality. The choice from among these options is a sociopolitical decision, which reflects the management objectives rather than purely technical considerations.     

SIMULATING THE IMPACT OF DRAINAGE DESIGN IN A COLD CLIMATE WITH ADAPT1

ABSTRACT: Surface and subsurface drainage make crop production economically viable in much of southern Minnesota because drainage allows timely field operations and protects field crops from extended periods of flooded soil conditions. However, subsurface drainage has been shown to increase nitrate/nitrogen losses to receiving waters. When engaging in drainage activities, farmers are increasingly being asked to consider, apart from the economic profit, the environmental impact of drainage. The Agricultural Drainage and Pesticide Transport model (ADAPT) was used in this study to evaluate the impact of subsurface drainage design on the soil water balance over a two‐year period during which observed drainage discharge data were available. Twelve modeling scenarios incorporated four drainage coefficients (DC), 0.64 cm/d, 0.95 cm/d, 1.27 cm/d, and 1.91 cm/d, and three drain depths, 0.84 m, 1.15 m, and 1.45 m. The baseline condition corresponded to the drainage system specifications at the field site: a drain depth and spacing of 1.45 m and 28 m, respectively (DC of 0.64 cm/d). The results of the two‐year simulation suggested that for a given drainage coefficient, soils with the shallower drains (but equal DC) generally have less subsurface drainage and can produce more runoff (but reduced total discharge) and evapotranspiration. The results also suggested that it may be possible to design for both water/nitrate/nitrogen reduction and crop water needs.