放牧对草原群落主要植物种和功能群水分来源与水分利用效率的影响

水分是半干旱草原生态系统植物多样性和初级生产力的限制因素。近年来由于人为干扰和气候干旱，特别是过度放牧，导致半干旱地区草原严重退化，草地生产利用和生态服务功能日益衰减，自然灾害频繁发生。草原退化演替主要表现为不同植物种的消长和替代过程。在内蒙古草原，过度放牧导致多年生根茎禾草和丛生禾草被豆科灌木或具根茎和不定根的杂类草替代，丰富的多年生杂类草被一、二年生植物替代。目前，对于上述功能群之间的替代机制，以及草原退化的机理尚不十分清楚。本研究在中国科学院内蒙古草原生态系统定位研究站选取了79年围封的大针茅(Stipa grandis)样地、其外围的自由放牧样地及中德合作项目“ Matter Fluxes in grassland of Inner Mongolia as influenced by stocking rate (MAGIM) ”的传统平地放牧处理小区为研究对象，从植物-水分关系的角度，利用氢和碳稳定性同位素技术，研究主要植物种和功能群水分来源和水分利用效率对放牧的响应，进而揭示放牧干扰下草原退化的机理。本研究取得了如下主要研究结果和结论： 1. 在干旱年份，雨水仅湿润了大针茅草原0-20cm的表层土壤。土壤中保存的冬季降水贡献了植物可利用水分的30%，而在正常年份只有10%。干旱季节羊草(Leymus chinensis)和大针茅能够利用土壤60cm以下保存的多年降水，而糙隐子草(Cleistogenes squarrosa)和冰草(Agropyron cristatum)只能利用生长季的雨水。长期过度放牧使冰草和糙隐子草的相对生物量和相对多度均显著增加，而羊草的相对生物量和相对多度显著降低。这种由放牧引起的群落结构与组成的改变，降低了植被对冬季降水的利用，加剧了干旱对生态系统的影响。 2. 依据羊草草原群落植物的生活型和光合类型划分为：C4禾草、C4杂类草、C4灌木、C3禾草、C3杂类草、C3鳞茎类植物和C3灌木七个功能群，各功能群间的水分利用效率差异显著。不同功能群植物在对土壤水分的利用上存在着明显的生态位分离。C4禾草和C3鳞茎类植物主要利用表层水分，而C4灌木则利用深层土壤水分，C3其它功能群介于二者之间。在无放牧和低载畜率下，各功能群植物均主要吸收浅层土壤水分，功能群间竞争相对强烈。在较高载畜率下，C3禾草转为利用深层土壤水分，功能群间出现水分生态位的分离，部分地缓解了植物对土壤表层水分的竞争。沿着载畜率梯度，群落对浅层土壤水分的利用呈现出先增加，尔后下降的趋势。 3. 在放牧干扰下，羊草草原群落中主要植物种稳定性碳同位素值的变化范围为-13.100/00~-27.590/00。不同功能群植物间的水分利用效率有着显著的差异：C4禾草> C4杂类草> C4灌木> C3禾草、C3杂类草> C3鳞茎类植物> C3灌木。C3鳞茎类植物和C4杂类草的水分利用效率随载畜率增加而降低。C3和C4禾草的水分利用效率随载畜率的增加表现为先增加，尔后下降的趋势。群落水平的水分利用效率主要由占生物量90%的禾草的水分利用效率决定。随着载畜率增加，群落水分利用效率有逐渐降低的趋势。

Habitat use by wintering Ruddy Shelduck at Lashihai Lake, Lijiang, China

Habitat use by wintering Ruddy Shelduck (Tadorna ferruginea) in Lijiang Lashihai Lake of southwest China was studied from 1 November 1999 to 29 April 2000. We divided habitats into five types-deep water, shallow water, mudflat, grassland and farmland. Shallow water and grassland, with rich food and easily accessible water, were preferred by wintering Ruddy Shelducks, Farmland was preferred in mid-winter but avoided in early winter and late winter. Even in mid-winter, the feeding Ruddy Shelduck on farmland were not equally distributed in fields and preferred wet fields (just irrigated) and avoided dry fields. In dry fields, the distances to water sources had great impact on the feeding distribution. Mudflats were only selected in later winter, coinciding with the growth of water-weeds. Deep-water areas were always avoided. Prohibition of human disturbance and retaining shallow water areas and grassland are important measures to mitigate conflict between Ruddy Sheldruck and local people.

纳滤和生物活性炭去除微污染原不中阿特拉津

除草剂阿特拉津的大量生产和广泛使用形成了对饮用水源的严重污染，目前在世界范围内的地表水和地下水中均检出一定浓度的阿特拉津，这对人类健康构成严重威胁。本文研究了采用纳滤技术和生物活性炭技术去除微污染原水中阿特拉津的可行性，对上述两种技术的去除效率、作用机理和影响因素进行了研究，并探讨了它们在未来饮用水深度处理中的优势和不足。本论文获得了以下一些具有重要意义的研究结果：（1）除天然有机物外，原水中无机离子在膜表面或孔径内吸附，引起膜有效孔径减小，使纳滤膜对农药截留率提高并降低水通量；在所研究的两个系列四种纳滤膜中，UTC-20截留阿特拉津达90％，截留其他有机物＞95％，对硝酸盐截留率＞70％，是迄今报道的对硝酸盐去除效率最高的纳滤膜，适于去除原水中阿特拉津和硝酸盐的双重污染；由于水合作用，纳滤膜对分子量相似有机物的截留率与有机物的油水分配系数（LogP）呈显著线性负相关，这一研究结果丰富了对有机物疏水性影响纳滤膜截留性能的认识。（2）筛选到一株能够以阿特拉津为惟一碳源生长的菌株-SYSA，经生理生化特性鉴定和1 6SrRNA基因序列分析，该菌为阴沟肠杆菌（Enterobacter cloacae）。这是首次报道肠杆菌属微生物可降解阿特拉津。对SYSA菌的生物学特性研究表明，SYSA菌可耐”受阿特拉津浓度100mg／L；pH7-8，30℃时，在以阿特拉津（20mg／L）惟一碳源的培养基上经146h培养，降解率为87％，该菌代时为2．gld，生长速率为（R）0.344dsel。（3）将SYsA菌接入活性炭柱，形成生物活性炭去除水中微量阿特拉津。研究结果表明空床接触时间为40min、温度为16℃±4℃、溶解氧为4.3-4.6mg／L时，120天后未接菌对照柱去除率下降至30％，而降解菌柱的去除效率却仍保持在65％～75％，延长了炭的使用时间。DGGE图谱表明未接菌对照柱、土壤悬液柱和降解菌柱上均有自来水中的微生物，但降解菌柱上还是以SYSA菌为优势菌。上述研究结果为纳滤或生物活性炭技术用于处理微污染原水、井直接生产饮用水提供了科学依据。

Reduction in microcystin concentrations in large and shallow lakes: Water and sediment-interface contributions

Blooms of cyanobacteria, or blue-greens, are known to produce chemicals, such as microcystins, which can be toxic to aquatic and terrestrial organisms. Although previous studies have examined the fate of microcystins in freshwater lakes, primary elimination pathways and factors affecting degradation and loss have not been fully explained. The goal of the present study was to explore sources of algal toxins and investigate the distribution and biodegradation of microcystins in water and sediment through laboratory and field analyses. Water and sediment samples were collected monthly from several locations in Lake Taihu from February 2005 to January 2006. Samples were analyzed for the presence of microcystin. Water and sediment were also used in laboratory studies to determine microcystin degradation rates by spiking environmental samples with known concentrations of the chemical and observing concentration changes over time. Some water samples were found to efficiently degrade microcystins. Microcystin concentrations dropped faster in water collected immediately above lake sediment (overlying water). Degradation in sediments was higher than in water. Based on spatial distribution analyses of microcystin in Lake Taihu, higher concentrations (relative to water concentrations) of the chemical were found in lake sediments. These data suggest that sediments play a critical role in microcystin degradation in aquatic systems. The relatively low levels of microcystins found in the environment are most likely due to bacterial biodegradation. Sediments play a crucial role as a source (to the water column) of bio-degrading bacteria and as a carbon-rich environment for bacteria to proliferate and metabolize microcystin and other biogenic toxins produced by cyanobacteria. These, and other, data provide important information that may be applied to management strategies for improvement of water quality in lakes, reservoirs and other water bodies. (C) 2007 Elsevier Ltd. All rights reserved.

Sediment sources and the flood record from Wanghu lake, in the middle reaches of the Yangtze River

A sediment core was collected from the centre of Wanghu Lake, in the Middle Reaches of the Yangtze River. The recent part of the core was dated using a combination of Pb-210 and spheroidal carbonaceous particle (SCP) techniques. Extrapolating this chronology dated the laminated section of the core, between 723 and 881 mm, to the first half of the 18th century and this section was selected for detailed study. The thicknesses of the laminae were measured using reflecting and polarizing microscopes whilst geochemistry was determined by an electron probe. The thickness of the dark layers was found to be positively correlated with titanium concentrations, and negatively correlated with aluminium and potassium concentrations. The thickness of the light layers was found to be negatively correlated with the concentrations of titanium. It is concluded that the dark layers were deposited from the Fushui River, a tributary of the Yangtze River, under periods of normal flow whilst the light Layers were mainly deposited from the Yangtze River itself during flood periods. Documentary evidence for floods occurring in the take catchment corresponded with thick laminations of high titanium concentration. Further, two of the three thickest, light laminations with low titanium concentrations were found to be synchronous with recorded flood dates of the main Yangtze River in its Middle Reaches, but one was synchronous with a local drought. These data suggest that the Lake sediment provides an archive of the relative water levels of the Yangtze and Wanghu including floods of both the main Yangtze River and the local hydrological regime. (c) 2006 Elsevier B.V. All rights reserved.

Discharges and sediments as sources of extracellular alkaline phosphatase in a shallow Chinese eutrophic lake

Total alkaline phosphatase activity (APA) and soluble reactive phosphorus (SRP) concentrations were measured in municipal wastewater, and a shallow Chinese freshwater lake receiving it. Activities of Dissolved alkaline phosphatase ( ADAP) in overlying and interstitial water were also analyzed monthly at three sites for several years. The lake was enriched with SRP and alkaline phosphatase by discharge of the wastewater, indicating that the inclusion of APA for estimating water pollution was reasonable. Annual data showed that APA in coarser fraction was significantly higher at the site receiving more wastewaters, both in surface and overlying water, suggesting that resuspension of enzyme most likely occurred in the basin heavily discharged. ADAP was an order of magnitude higher in the wastewater than those in lake waters, and was generally higher in interstitial water, a feature more striking at the site receiving more discharges. Besides, it was irrespectively inhibited by Na2WO4, L-cysteine and EDTA-Na, but stimulated by Cu2+, Zn2+, CTAB and Triton X-100 in interstitial, overlying and surface waters. This similarity of responding patterns to the stressors indicated an analogy between dissolved alkaline phosphatase in water column and that in interstitial water, supporting the hypothesis that the polluted sediments act as source of dissolved alkaline phosphatase in eutrophic lakes.

Spatial variability in water quality and surface sediment diatom assemblages in a complex lake basin,lake of the woods,ontario,canada

Lake of the Woods (LOW) is an international waterbody spanning the Canadian provinces of Ontario and Manitoba, and the U.S. state of Minnesota. In recent years, there has been a perception that water quality has deteriorated in northern regions of the lake, with all increase in the frequency and intensity of toxin-producing cyanobacterial blooms. However, given the lack of long-term data these trends are difficult to verify. As a first step, we examine spatial and seasonal patterns in water quality in this highly complex lake on the Canadian Shield. Further, we examine surface sediment diatom assemblages across multiple sites to determine if they track within-take differences in environmental conditions. Our results show that there are significant spatial patterns in water quality in LOW. Principal Component Analysis divides the lake into three geographic zones based primarily on algal nutrients (i.e., total phosphorus, TP), with the highest concentrations at sites proximal to Rainy River. This variation is closely tracked by sedimentary diatom assemblages, with [TP] explaining 43% of the variation in diatom assemblages across sites. The close correlation between water quality and the surface sediment diatom record indicate that paleoecological models could be used to provide data on the relative importance of natural and anthropogenic sources of nutrients to the lake.

Sulfonated poly(ether ether ketone)/clay-SO3H hybrid proton exchange membranes for direct methanol fuel cells Journal of Power Sources

A new type of sulfonated clay (clay-SO3H) was prepared by the ion exchange method with the sulfanilic acid as the surfactant agent. The grafted amount of sulfanilic acid in clay-SO3H was 51.8 mequiv. (100 g)(-1), which was measured by thermogravimetric analysis (TGA). Sulfonated poly(ether ether ketone) (SPEEK)/clay-SO3H hybrid membranes which composed of SPEEK and different weight contents of clay-SO3H, were prepared by a solution casting and evaporation method. For comparison, the SPEEK/clay hybrid membranes were produced with the same method.

Novel proton exchange membranes based on water resistant sulfonated poly[bis(benzimidazobenzisoquinolinones)]

Novel water resistant sulfonated poly[bis(benzimidazobenzisoquinolinones)] (SPBIBIs) were synthesized from 6,6'-disulfonic-4,4'-binaphthy]-1,1',8,8'-tetracarboxylic dianhydride (SBTDA) and various aromatic ether tetraamines. The resulting polymers with IEC in the range of 2.17-2.87 mequiv g(-1) have a combination of desired properties such as high solubility in common organic solvents, film-forming ability, and excellent thermal and mechanical properties. Flexible and tough membranes, obtained by casting from m-cresol solution, had tensile strength, elongation at break, and tensile modulus values in the range of 87.6-98.4 MPa, 35.8-52.8%, and 0.94-1.07 GPa. SPBIBI membranes with a high degree of sulfonation displayed high proton conductivity and a good resistance to water swelling as well. SPBIBI-b with IEC of 2.80 mequiv g(-1) displayed the conductivity of 1.74 x 10(-1) S cm(-1) at 100 degrees C, which was comparable to that of Nafion (R) 117 (1.78 x 10(-1) S cm(-1), at 100 degrees C).

Low-temperature synthesis of oil-soluble CdSe, CdS, and CdSe/CdS core - Shell nanocrystals by using various water-soluble anion precursors

Colloidal CdSe and CdS quantum dots were synthesized at low temperatures (60-90 degrees C) by a two-phase approach at a toluene-water interface. Oil-soluble cadmium myristate (Cd-MA) was used as cadmium source, and water-soluble Na2S, thiourea, NaHSe, Na2SeSO3, and selenourea were used as sulfur and selenium sources, respectively. When a cadmium precursor in toluene and a selenium precursor in water were mixed, CdSe nanocrystals were achieved at a toluene-water interface in the range of 1.2-3.2 nm in diameter. Moreover, we also synthesized highly luminescent CdSe/CdS core-shell quantum dots by a two-phase approach using poorly reactive thiourea as sulfur source in an autoclave at 140 degrees C or under normal pressure at 90 degrees C. Colloidal solutions of CdSe/CdS core-shell nanocrystals exhibit a photoluminescence quantum yield (PL QY) up to 42% relative to coumarin 6 at room temperature.

Preparation and evaluation of a proton exchange membrane based on oxidation and water stable sulfonated polyimides

A series of novel oxidation and water stable sulfonated polyimides (SPIs) were synthesized from 4,4'-binaphthyl-1,1',8,8'-tetracarboxylic dianhydride (BTDA), and wholly aromatic diamine 2,2'-bis(3-sulfobenzoyl) benzidine (2,2'-BSBB) for proton exchange membrane fuel cells. These polyimides could be cast into flexible and tough membranes from m-cresol solutions. The copolymer membranes exhibited excellent oxidative stability and mechanical properties due to their fully aromatic structure extending through the backbone and pendant groups. Moreover, all BTDA-based SPI membranes exhibited much better water stability than those based on the conventional 1,4,5,8-naphthalenecarboxylic dianhydride. The improved water stability of BTDA-based polyimides was attributed to its unique binaphthalimide structure. The SPI membranes with ion exchange capacity (IEC) of 1.36-1.90 mequiv g(-1) had proton conductivity in the range of 0.41 x 10(-1) to 1. 12 x 10(-1) S cm(-1) at 20 degrees C. The membrane with IEC value of 1.90 mequiv g(-1) displayed reasonably higher proton conductivity than Nafion((R)) 117 (0.9 x 10(-1) S cm(-1)) under the same test condition and the high conductivity of 0.184 S cm(-1) was obtained at 80 degrees C. Microscopic analyses revealed that well-dispersed hydrophilic domains contribute to better proton conducting properties. These results showed that the synthesized materials might have the potential to be applied as the proton exchange membranes for PEMFCs.