长江上游小型水库枯水期水质对景观组成、配置和水库特征的响应

长江流域小型水库数量多分布广,具有重要的生态经济效益,探明小型水库水质对环境变量的响应规律对于提升水库水质具有非常重要的意义.基于长江上游36个小型水库枯水期水质数据,运用相关分析和冗余分析等研究方法,将环境变量划分为景观配置指标、景观组成指标和水库特征指标这三大类,探明其对水质指标变化的影响.结果表明：(1)旱地是NO^-₃-N、TN和TP的主要来源;居民点是TP物质的主要来源;水田、林地和荒草地对水库N、P的截留和净化具有正向作用;(2)旱地最大斑块指数与水库TN和NO^-₃-N浓度显著正相关,水田散布与并列指数、林地散布与并列指数与水库NO^-₃-N和TN浓度显著负相关;旱地斑块密度与TP物质含量显著正相关;林地最大斑块指数与TP含量显著负相关;(3)水库库容、水库平均深度和水库形状指数对水库水质提升具有显著的正向作用;(4)水库环境变量中,景观配置指标对水库水质指标变化的解释率最高(24%),其次是水库特征指标(11%),最后为景观组成指标(9%).流域...     

我国循环经济的发展模式

循环经济发展模式主要是指循环经济的产业发展模式和区域发展模式。根据我国循环经济的内涵、国际做法和国内相关实践探索经验,我国循环经济的产业发展模式涉及生产和消费两个重点领域和四个重点产业。四个重点产业是生态工业、生态农业、绿色服务业和废弃物再利用、资源化及无害化处置产业。循环经济区域发展模式是在区域基础设施体系和生态系统支撑下的两个重点领域和四个重点产业的有机组合和共生。是区域可持续发展的核心组成部分。区域基础设施体系也是应用循环经济原理的重要领域。以资源能源离效和环境影响最小为特征。在目前的实践中。我国出现了三种将发展循环经济作为推动区域可持续发展的助推器而引发的区域社会经济发展战略转型模式：东部发达地区的自发转型模式、辽宁资源型地区的转型模式和西部地区典型的跨越发展转型模式。     

基于生态市建设的生态可持续发展研究——以常州市为例

以常州市为例,探讨了基于生态市建设的生态可持续发展的内涵,提出“生态保育区-生态提升区-生态新建区”的生态建设分区模式和市域生态防护网架是构建区域生态安全格局的基本框架和促进区域生态可持续发展的调控途径。     

生态示范区建设的模式及其实践的几点思考

就生态示范区建设的重要性、生态示范区建设模式进行探讨,分析了生态示范区建设模式的成功范例,最后提出创建生态示范区的建议。     

大落差原油管道投产油顶水过程研究

为了探究隔离球在大落差原油管段投产过程中的影响作用,以某大落差“U”型起伏原油管线为实际案例（其最大高差达1 490 m）,基于OLGA多相流瞬态模拟方法,对大落差原油管段油顶水过程进行仿真研究。分析隔离球对原油顶水过程中的混油影响,同时对不同输量、管内积液量条件下隔离球在大落差管段中的运动特性进行研究,得到了清管器的平均运行速度、管中压力、持液率的变化趋势以及清管过程中的段塞行为等。结果表明:当输量为900~2 500 m3/h时,隔离球的加入能够降低混油量84.2%~93.7%;同时,还能减少投产过程中由于油品轻质组分汽化所产生的气体,并将更多管内气体带走,减少管中段塞流,提高原油投产效率,为工程实际投产过程提供有效依据。     

Na_2CO_3/H_2O_2“稳定”的CO_2的型体研究(Ⅱ)——“稳定性二氧化氯”溶液的UV吸收光谱、纸层析特性、微观结构和离子色谱分析

本文对以稳定剂H_2O_2和Na_2CO_3与ClO_2制备的所谓"稳定性二氧化氯"溶液的UV吸收光谱、纸层析特性、微观结构及离子色谱进行了分析,并与纯NaClO_2及ClO_2溶液做了对比.结果表明,“稳定性二氧化氯” 与NaClO_2在UV吸收光谱、层析比移值、微观结构、离子色谱这几方面都具有很好或极其相似的一致性 表明“稳定性二氧化氮’与NaClO_2溶液中氯氧化物存在型体的一致性.因此,认为“稳定性二氧化氯“溶液中ClO_2是以亚氯酸盐ClO_2~-的型体存在的.     

Seasonal variation of total dissolved arsenic and arsenic speciation in a polluted surface waterway

Seasonal differences in the dissolved arsenic concentration and speciation in a contaminated urban waterway in northwest England have been determined using a coupled ion chromatography-inductively coupled plasma-mass spectrometry (IC-ICP-MS) technique. Waters sampled in the vicinity of an industrial works during relatively dry conditions in April 2000 were found to contain total arsenic concentrations (As) of up to 132 g L^–1, more than an order magnitude greater than the 4 g L^–1 maximum found in December 2000. The difference in As between the April and December sampling periods is speculated to be largely due to the irregular anthropogenic supply of arsenic to the watercourse. For both sampling periods, the dissolved arsenic was exclusively inorganic in nature and had an As(V)/As ratio of between 0.6 and 0.8. Analysis of samples taken downstream of the industrial site, after the confluence with a relatively As-poor stream, revealed that As(III), As(V) and As concentrations were lower than would be expected from conservative mixing. The As(V)/As ratio was also observed to decrease markedly. The loss of arsenic from solution is thought to be due to adsorption on the iron oxyhydroxide-rich sediment observed to coat the riverbed downstream of the confluence. The reduction in the As(V)/As ratio is believed to be due to the more rapid adsorption of As(V) compared to that of As(III). Deviations from conservative behaviour were more marked during the relatively dry April 2000 sampling period and suggest the increased importance of adsorption processes controlling arsenic availability during this time.     

Grazing as a measure against grass encroachment in Dutch dry dune grassland: effects on vegetation and soil

A grazing experiment was started in 1984 and 1989 respectively, in two parts of a dune grassland in the nature reserve ‘Zwanenwater’, North Holland; a third part with similar geology and topography was used as a control area and not grazed. An evaluation of the effects of grazing on vegetation patterns, species composition, vegetation structure and humus form was made with the help of vegetation maps from 1986 and 1992 as well as field surveys. Dense tall-grass communities dominated byAmmophila arenaria increased over the period 1986–1992 in the grazed areas, and especially in the non-grazed area (increase in area to 20%, 22% and 50%, respectively). Open communities decreased in the grazed areas, but are still prevalent, while in the ungrazed area they virtually disappeared, with the result that the present percentage areas are 53%, 38% and 17%. Field survey data were classified by TWINSPAN producing four vegetation types. These occur more or less equally in grazed and ungrazed areas, albeit with different percentage areas: (1) open vegetation dominated byCorynephorus canescens; (2) open vegetation characteized, byKoeleria macrantha; (3) heathland dominated byEmpetrum nigrum; and (4) tall-grass communities dominated byAmmophila arenaria. Within a vegetation type, species composition was only marginally affected by grazing regime. Within the open communities the number of species, vegetation height, vegetation cover and soil organic horizons were not affected by grazing. In the tall-grass communities the number of species was significantly larger and the height of the vegetation significantly lower in the area grazed since 1984. In the heathland community the number of species and cover of the moss layer were significantly higher in the 1984 area and ectorganic and endorganic horizons significantly thicker in the ungrazed area. It is suggested that these effects are the result of an increased availability of light, but possibly also of a decreased stock of organic matter and nutrients, due to a decreased input of litter and accelerated rates of decomposition.     

鼓翅皱膝蝗生态学特性研究

在甘肃省夏河县对鼓翅皱膝蝗的种群结构、数量变动、空间格局及动脉进行了系统研究。鼓翅皱膝蝗1a发生1代，以卵在土中越冬，翌年5月中旬开始孵化出土，6月上旬达到出土高峰，此期蝗虫种群仅由1龄和2龄蝗蝻组成，其中1龄蝗蝻占81.8％，2龄蝗蝻占18.2％，成虫于7月上旬开始羽化，8月上旬达到羽化高峰，此期的成虫数量达61.3％，而蝗蝻仅占38.7％，蝗蝻期约为72d，成虫寿命54d左右，每雌平均产卵32.6粒。鼓翅皱膝蝗在草地上属聚集分布，蝗蝻发生期种群的空间动态主要表现出扩散趋势，但初孵化出土时有短暂的聚集行为。取食量随龄期增大而增大，每头鼓翅皱膝蝗取食牧草量蝗蝻期平均为1.5g，成早期约为5.8g，成早期的食量是蝗蝻期的3.7倍。表3参12     

Scenarios of major terrestrial ecosystems in China

The spatial pattern and mean-center shift of major terrestrial ecosystems, termed Holdridge Life Zones (HLZ), during the periods from 1961 to 1990 (T1), from 2010 to 2039 (T2), from 2040 to 2069 (T3) and from 2070 to 2099 (T4) were analyzed by combining the zonal patterns of climatic change in China and the climatic change scenarios of HadCM2 and HadCM3. The results showed that nival area would decrease rapidly with temperature increase in the future. HadCM2 and HadCM3 predicted that the nival areas might disappear in 552 years and 204 years, respectively. Using both HadCM2 and HadCM3, the five HLZ types with the largest areal extent are nival zone, cool temperate moist forest, warm temperate moist forest, subtropical moist forest and boreal wet forest, which collectively account for more than 50% of China's land mass. Among these five HLZ types, nival zone, warm temperate moist forest and boreal wet forest would decrease continuously, whereas subtropical moist forest and cool temperate forest would increase continuously during the four periods. HLZ diversity and patch connectivity would increase continuously in the 21st century. The shift distances of mean centers of HLZ types simulated using HadCM3 were markedly greater than those simulated using HadCM2, in general. The results from both HadCM2 and HadCM3 showed that boreal wet forest, subtropical moist forest, tropical dry forest, warm temperate moist forest and subtropical wet forest had bigger shift ranges, indicating that these HLZ types are more sensitive to the climatic change scenarios of HadCM2 and HadCM3.