农村生活污水处理实用技术新进展

对高效藻类塘、一体化氧化沟、蚯蚓生态滤池和土壤毛细管渗滤净化系统四种实用工艺的特点和效果进行了介绍和分析，以供决策者参考。     

伪装遮障材料耐老化性能与机理分析

目的 研究伪装遮障材料在实用期的老化机理,获悉伪装遮障材料失效的主要环境因素。方法 通过分析伪装遮障材料在自然环境和实验室单因素环境中的性能变化,得出影响伪装遮障材料老化失效的主要因素。采用扫描电子显微镜、红外光谱仪、X射线光电子能谱仪表征材料的微观形貌、化学结构和化学成分变化,解释伪装遮障材料的老化机理。结果 获得了在不同自然环境、实验室单因素环境下,伪装遮障材料颜色外观和力学性能的变化规律,得到了伪装遮障材料在老化过程中发生的微观形貌、化学结构和化学成分变化。结论 伪装遮障材料在西双版纳自然环境下的老化程度最大,在济南自然环境下的老化程度最小。光照是导致伪装遮障材料颜色外观及力学性能降低的主要因素。老化过程中,主要是材料表面的聚氨酯发生老化、脱落,导致材料的力学性能下降。伪装遮障材料破坏时,纤维有2种失效形式,一种是纤维脱黏、直接断裂;另一种是纤维脱黏,拔出,或者拔出过程中断裂。     

贵州百花湖消落区土壤磷赋存形态初步研究

应用磷形态标准测试程序(SMT)对百花湖(水库)消落区土壤磷赋存形态进行了分级测定,分析了各形态磷之间与样品理化性质如有机质、pH、总氮和含水率的相关性。结果表明,百花湖消落区1区全磷含量平均为1239.9mg/kg,2区为1097.4mg/kg,3区为1041.5mg/kg;各形态磷中有机磷占全磷的百分比1区为58.7%,2区为55.1%,3区降至54.7%;消落带土壤中的磷以有机磷为主,无机磷为辅。铁铝结合态磷则是无机磷的主要组分,其中1区为77.1%,2区为66.7%,3区为61.4%;全磷、有机磷和铁铝结合态磷含量的总体变化趋势为1区>2区>3区;而钙结合态磷含量却呈现出3区>2区>1区。有机磷与全磷显著性相关,是土壤中磷素增加的主要因素;无机磷与铁铝结合态磷和钙结合态磷显著性相关,二者的增加和减少对无机磷的含量具有显著影响;全磷与有机质、酸碱性显著相关;有机磷与有机质,钙结合态磷与酸碱性之间均呈现出显著性相关,表明土壤的有机质和酸碱性影响磷的含量和分布。     

黑龙江省平水期地表水总磷构成的研究

通过对黑龙江省平水期地表水总磷监测结果分析,探讨地表水总磷的构成、成因;提出了从源头治理地表水总磷污染建议。     

三峡水库消落带土壤与优势植物淹水后对土-水系统汞形态的影响

三峡库区消落带落干期植被生长茂盛,蓄水后消落带被淹没,土壤-植物系统在长时间淹水情况下,随着体系内物理化学性质的改变,汞形态也会发生变化,从而对库区水生生态系统中汞含量以及形态带来一定的影响.为此,本研究选取三峡库区4种优势植物室内栽培,再进行室内模拟淹水试验,研究淹水后土壤、水体中甲基汞(Me Hg)以及其他形态汞的变化.结果表明,淹水过程中植物的存在有利于土壤Me Hg的生成,同时对上覆水不同形态汞浓度影响显著.狗牙根作为消落带优势种,由于其体内总汞及甲基汞含量较高,淹水后对土壤以及上覆水系统中甲基汞以及其他汞形态的影响最为明显.淹水第90 d,狗牙根+土+江水(B1)处理土壤Me Hg的含量最高,为(1 135.86±113.84)ng·kg~(-1),是不加植物的对照处理土+江水(CK2)中土壤Me Hg含量的2倍左右;上覆水总甲基汞(TMe Hg)、溶解态甲基汞(DMe Hg)、总汞(THg)、溶解态汞(DHg)和活性汞(RHg)均呈峰值偏左的抛物线状变化,在第30 d时达到峰值,其中B1处理上覆水TMe Hg、THg和DHg最高,分别为(2.88±0.06)、(40.29±2.42)和(35.51±3.77)ng·L~(-1),三者中溶解态汞是其主要存在形式.因此可以推测三峡库区消落带植物淹水后将增加水库汞污染负荷.     

A study of climate change and anthropogenic impacts in West Africa

BACKGROUND, AIM AND SCOPE: During the last decades ecological conditions in West Africa have dramatically changed. Very evident is the climate change, which has resulted in a southward shift of the climate zones, e.g. a spread of the desert (Sahara) into the Sahelian zone. After the drought period of the early 1970s and 1980s, livestock density increased resulting in an intensification of grazing pressure. This anthropogenous phenomenon leads to similar landscape changes as those caused by the climate. Only very few investigations exist on vegetation dynamics, climate changes and land use changes for the Sudanian zone. The paper presents data on changes of precipitation, of land use, of the geographical range of species, and of the composition of the flora, which have to be regarded as proofs of the sahelisation of large areas of the Sudanian zone. MATERIALS AND METHODS: Area of investigation: Burkina Faso. Precipitation data analysis: precipitation data from 67 stations; time series analysis and geo-statistical spatial interpolation. Analysis of land use change: Landsat satellite MSS and ETM+ data, acquired for two different dates between 1972 and 2001 analyzed by the software ERDAS/IMAGINE version 8.6 and ArcView 3.2 with the Spatial Analyst extension. Intensive ground truthing (160 training areas). Inventory of the flora: based on the data of the Herbarium Senckenbergianum (FR) in Frankfurt, Germany, and of the herbarium of the university of Ouagadougou (OUA), Burkina Faso, as well as on various investigations on the vegetation of Burkina Faso carried out in the years 1990 to 2005 by the team of the senior author. Life form analysis of the flora: based on the inventory of permanent plots. RESULTS AND DISCUSSION: Precipitation: Remarkable latitudinal shift of isohyets towards the South translates to a general reduction of average rainfall in great parts of the country. The last decade (1990-1999) shows some improvement, however, the more humid conditions of the 1950's and 1960's are not yet established again. Landcover change: In the study region the extent of arable fields and young fallows increased during the last 30 years from 580 km(2) in 1972 to 2870 km(2) in 2001. This means an average land cover conversion rate of 0.9% per year for the 6 departments considered. Change of the distribution of Sahelian and Sudanian species: Several species, mentioned in older literature as strictly Sahelian, today also occur in the Sudanian zone. Parallel to the spread of former strictly Sahelian species into the Sudanian zone, some former Sahelo-Sudanian species have withdrawn from the Sahel. Changes of the life form spectra of the flora: Considering their life form spectra, the flora of heavily grazed and of protected areas in the Sudanian zone show great differences. On areas intensively grazed the percentage of therophytes is evidently higher than on protected areas. Just the opposite is true for the phanerophytes. Their percentage is higher on the protected area than on the grazed zones. At the first glance, it is obvious to link the changes in flora and vegetation with the climate changes that have occurred during the last five decades (decrease of annual precipitation). However, not only climatic conditions have changed, but also population has increased, the percentage of land intensively used for agriculture and pasturing has increased and the time for soil regeneration today is much shorter than it was some decades ago. Thus, the landscape of the Sudanian zone has become a more Sahelian character. A comparison of the flora of an intensively used area of the Sudanian zone with that of a protected area shows a remarkable change in the life form spectra. The spectrum of the intensively used area is almost identical with that of the typical Sahelian flora. This comparison shows that the anthropogenic influence plays a greater role in the sahelisation of the Sudanian zone than the climate change. CONCLUSION: Climate change and anthropogenic influence both, lead to a sahelisation of landscape and flora. Thus in many parts of the Sudanian zone of West Africa sahelisation phenomena will remain and even increase independently from the reestablishment of the more humid climate conditions of the 1950ies. RECOMMENDATIONS AND PERSPECTIVES: In order to maintain some parts of the characteristic Sudanian landscape with its characteristic flora and vegetation, the number and size of protected areas should be augmented. For all protected areas it has to be ensured, that protection is reality, i.e. respected an understood by local people, not only fiction. As long as the enlargement of intensively used areas continues the sahelisation of flora, vegetation and landscape will continue too.     

基于CA的城市形态扩展多解模拟——以北京市东部平原区情景分析为例

构建了一个基于人工神经网络的约束型城市扩展CA模型。利用该模型,预测了北京市东部平原区在3种情景规划之下的未来50年的城市形态,为不同的城市发展模式之间的比较分析奠定基础。然后以2024年的北京东部平原区模拟城市形态为基准,从自然生态功效、社会服务功效、经济利益功效3个方面对3种规划模式进行了情景分析,从而系统的比较了3种规划模式的复合生态功效,为城市规划决策提供有力的支持。     

不同晶型纳米TiO_2在斑马鱼体内的富集与清除

为探讨纳米材料的慢性生物效应以及材料结构对生物富集的影响,开展了A-TiO2(锐钛型纳米TiO2)和R-TiO2(金红石型纳米TiO2)在斑马鱼(Danio rerio)体内的长期富集和清除试验.采用半静态暴露试验,试验周期为46 d(暴露阶段28 d,清除阶段18 d),每种晶型设置2个处理组(ρ分别为4.0和10.0 mg/L),测定各时间点斑马鱼体内不同晶型纳米TiO2含量(以w计);以暴露阶段的BAF(生物富集系数)以及清除阶段的排出速率常数、总量清除率为终点,比较斑马鱼对2种晶型纳米TiO2的富集、清除的异同.结果表明:在暴露阶段,A-TiO2在斑马鱼体内的富集量显著高于R-TiO2,10.0 mg/L处理组斑马鱼体内富集量均显著高于4.0 mg/L处理组;4.0和10.0 mg/L的A-TiO2处理组的BAF分别为76.7和105.4 L/kg,略高于R-TiO2(41.6和36.1 L/kg),二者在斑马鱼体内均不具有生物蓄积性.在清除阶段,斑马鱼体内的2种晶型的纳米TiO2均可被排出,清除阶段的清除率为88.0%~100%;斑马鱼体内2种晶型纳米TiO2富集量的下降均符合一阶指数衰减方程,排出速率常数在0.26~1.01 d-1之间.     

Leaching-induced migration and compositional form change of Cu,Zn, and Cd from sludge to loess

Land utilization of sewage sludge has become one of the major issues in environmental mitigation in China. This is particularly important in the Loess Plateau of Northwest China. Sludge enriched with organic matter and nutrients might effectively help to resolve the problems of silty loess soils as evidenced by porosity defect, structural alterations and absence of fertility. After sludge flows into the loess, irrigation water contains heavy metals that leach and migrate into sludge and consequently related human health risks may occur that raise concerns; and this situation needs to be rectified. The characteristics of the vertical migration and composition form change of Cu, Zn, and Cd from composted sludge to loess, and corresponding influencing factors, were investigated by performing a soil column simulation test under the leaching treatment of a one-year irrigation water capacity. Results demonstrated that: (1) composted sludge significantly improved loess fertility, and irrigation leaching transported only a small quantity of organic matter in sludge in the plough layer; (2) although some of the Cu, Zn, and Cd in composted sludge migrated to and concentrated in the middle and upper layers of the soil column during leaching, these metals were mostly retained in the plough layer; and (3) after the leaching treatment of the one-year irrigation water capacity, the compositions of Cu, Zn, and Cd (particularly Cu and Zn) in both plough layer and loess began to stabilize with low concentrations in the exudate. These findings confirmed the applicability of composted sludge in loess regions. This study provided a new insight into the sludge reuse in alkaline soils in arid and semi-arid region.