Enhanced denitrification and organics removal in hybrid wetland columns: comparative experiments

This study investigated three lab-scale hybrid wetland systems with traditional (gravel) and alternative substrates (wood mulch and zeolite) for removing organic, inorganic pollutants and coliforms from a synthetic wastewater, in order to investigate the efficiency of alternative substrates, and monitor the stability of system performance. The hybrid systems were operated under controlled variations of hydraulic load (q, 0.3-0.9 m³/m² d), influent ammoniacal nitrogen (NH₄-N, 22.0-80.0 mg/L), total nitrogen (TN, 24.0-84.0 mg/L) and biodegradable organics concentration (BOD₅, 14.5-102.0 mg/L). Overall, mulch and zeolite showed promising prospect as wetland substrates, as both media enhanced the removal of nitrogen and organics. Average NH₄-N, TN and BOD₅ removal percentages were over 99%, 72% and 97%, respectively, across all three systems, indicating stable removal performances regardless of variable operating conditions. Higher Escherichia coli removal efficiencies (99.9%) were observed across the three systems, probably due to dominancy of aerobic conditions in vertical wetland columns of the hybrid systems.     

Factors determining the occupation of Marsh Harrier Circus aeruginosus breeding grounds in a Mediterranean environment

Capsule Wetland occupation by breeding Marsh Harriers is influenced by wetland and vegetation area, distance to other wetlands where conspecifics are present and also by the characteristics and conditions of the vegetation such as predominant species and its height at the start of the breeding period.

Aims To determine factors influencing the probability of wetland occupation by Marsh Harrier in relation to wetland dimensions, vegetation and hydric conditions, and to determine the effect of the predominant helophyte species in the wetlands and its physical characteristics.

Methods Three hundred and thirty-two wetlands were monitored during a breeding season in NW Spain, a Mediterranean area that hosts 10% of the total number of breeding pairs of Marsh Harriers in Spain. The probability of wetland occupation for breeding in terms of wetland size and proximity, vegetation characteristics, human disturbance and also hydrological variables, was analysed using logistic regression.

Results One hundred and sixty-five pairs were located in 131 wetlands. Variables affecting occupation include vegetation composition and characteristics, wetland dimensions and distance to other occupied wetlands. Wetlands with the highest probability of being occupied were larger, with greater areas of marsh vegetation, taller vegetation, rush and reed communities as the predominant species and which were closer to another wetland occupied by Marsh Harriers.

Conclusions The dimensions and predominant species of helophyte vegetation, and size and location determine the occupation of wetlands as breeding grounds by Marsh Harrier. Changes in the natural supply of water and nutrients due to the implementation of intensive irrigation farming are likely modifying flora in wetlands and affecting the distribution and population size of Marsh Harriers in this region of Spain.     

龙凤湿地与珰奈湿地底泥细菌古菌多样性及其对环境因子的响应

【背景】城市湿地和天然湿地受到人为扰动影响的程度显著不同。【目的】研究2种不同类型湿地底泥微生物多样性及种类的差异。【方法】采集冬夏两季城市湿地(龙凤湿地)和天然湿地(珰奈湿地)的底泥样品,使用16S rRNA基因测序技术测定底泥中细菌和古菌群落结构,分析2种湿地底泥的细菌、古菌差异及环境因素与微生物的相关性。【结果】龙凤湿地底泥中的硫杆菌属(Thiobacillus)、芽孢杆菌属(Bacillus)和鞘氨醇单胞菌属(Sphingomonas)丰度显著高于珰奈湿地(P<0.05);Methanoregula在珰奈湿地底泥中的丰度高于龙凤湿地;冬季厌氧绳菌属(Anaerolinea)和甲烷八叠球菌属(Methanosarcina)在珰奈湿地底泥中的丰度显著高于龙凤湿地(P<0.05)。【结论】龙凤湿地与珰奈湿地的差异主要影响湿地底泥中参与元素循环的细菌和产甲烷古菌的丰度,人为干扰和低温会降低湿地中微生物的多样性,pH、盐分和碱性磷酸酶是显著影响微生物多样性的环境因素。     

WETLANDS AS ACCRETING SYSTEMS: NUTRIENT CYCLING IN WETLANDS

SUMMARY

The major concepts involved in nutrient cycling in wetlands are discussed using phosphorus and nitrogen as examples. The differences in nutrient cycling patterns between hydrologically contrasting wetlands, and the significance of fluctuating water levels in wetlands, are stressed. In South Africa, some research into nutrient cycling in submerged aquatic macrophyte communities has been undertaken, but very little information is available on these processes in wetlands dominated by emergent vegetation forms. Generally, the information available on nutrient cycling processes in South African wetlands is of limited applicability to the assessment of nutrient cycling in whole wetland systems. Therefore, rational wetland management strategies require further research on nutrient cycling.     

东北湿地沉积物中T4型噬菌体g23基因的多样性

【目的】揭示我国东北典型湿地沉积物中T4型噬菌体g23基因的多样性,明确湿地环境T4型噬菌体群落分布特征,为噬菌体生态学研究提供数据支撑。【方法】采用简并性引物MZIA1bis和MZIA6对采自东北6个地点不同类型湿地沉积物土壤DNA进行PCR扩增,采用克隆测序方法,解析沉积物中T4型噬菌体g23基因组成,通过UniFrac分析T4型噬菌体群落结构在湿地沉积物中与其他环境中的差异。【结果】在东北湿地沉积物中共得到262条不同的g23基因序列,构建的系统进化树分析表明,我国东北湿地沉积物T4型噬菌体g23基因分布与海洋、湖泊及稻田生态系统中g23基因亲缘关系较近,而与东北旱地黑土g23基因分布较远;以g23基因群集表征的T4型噬菌体群落在不同地点湿地中分异明显。【结论】东北湿地生态系统T4型噬菌体群落结构复杂多样,存在着一些未知的噬菌体类群。     

纳帕海高原湿地噬藻体g20基因系统发育多样性分析

【背景】噬藻体是感染蓝藻的病毒,是水生系统的重要组成部分。它们对宿主种群死亡率有重要影响,是控制蓝藻水华生消的潜在因子,对蓝藻群落结构的调控具有重要意义。大量研究揭示了海洋和淡水环境中噬藻体的高度多样性,但目前对高原湿地中噬藻体的多样性知之甚少。【目的】阐明我国纳帕海高原湿地噬藻体g20基因的遗传多样性,为进一步开展高原湿地微生物资源及其生态功能研究提供理论基础。【方法】采集雨季的水体样品,以衣壳蛋白基因g20为标记基因,利用特异性引物Cps1和Cps8对其进行PCR扩增,得到26条不同的g20基因有效序列,并将其与其他生境中g20基因序列进行主坐标分析和系统发育分析。【结果】与其他海洋和淡水的噬藻体序列相比,纳帕海高原湿地中噬藻体的序列与其他稻田序列更为相近;但也存在部分序列单独聚簇,这可能为纳帕海高原湿地中独有的噬藻体类型。【结论】表明该地区的噬藻体较丰富,并具有一定的独特性。     

Characterization of Neutrophilic Fe(II)-Oxidizing Bacteria Isolated from the Rhizosphere of Wetland Plants and Description of Ferritrophicum radicicola gen. nov. sp. nov., and Sideroxydans paludicola sp. nov.

Iron deposits (Fe plaque) on wetland plant roots contain abundant microbial populations, including Fe(II)-oxidizing bacteria (FeOB) that have not been cultured previously. In this study, 4 strains of Fe plaque-associated FeOB were isolated from 4 species of wetland plants. All 4 isolates grew in tight association with Fe-oxides, but did not form any identifiable Fe-oxide structures. All strains were obligate lithotrophic Fe(II)-oxidizers that were microaerobic, and were unable to use other inorganic or organic energy sources. One strain, BrT, was shown to fix ¹⁴ CO ₂ at a rate consistent with its requirement for total cell carbon. The doubling times for the strains varied between 9.5 and 15.8 hours. The fatty acid methyl ester (FAME) profiles of 2 strains, BrT and CCJ, revealed that 16:0, 15:1 isoG, and 14:0 were dominant fatty acids. Phylogenetic analysis of the 16S rRNA gene indicated that all the strains were Betaproteobacteria. Two of the strains, BrT and Br-1 belong to a new species, Sideroxydans paludicola; a third strain, LD-1, is related to Sideroxydans lithotrophicus, a recently described species of FeOB. The fourth isolate, Ferritrophicum radicicola, represented a new genus in a new order of Betaproteobacteria, the Ferritrophicales. There are no other cultured isolates in this order. A small subunit rRNA gene-based, cultivation-independent analysis of Typha latifolia collected from a wetland revealed terminal restriction fragment profiles (tRFLP) consistent with the presence of these bacteria in the rhizosphere. These novel organisms likely play an important role in Fe(II) oxidation kinetics and Fe cycling within many terrestrial and freshwater environments.     

青海湖3种类型高寒湿地甲烷氧化菌群落特征

【背景】甲烷氧化菌在维持湿地生态系统碳平衡方面发挥着重要作用,青海湖高寒湿地具有十分重要的生态地位,但目前有关该地区甲烷氧化菌的研究相对较少。【目的】探究不同类型高寒湿地土壤甲烷氧化菌的群落特征与驱动因素。【方法】以青海湖流域内的小泊湖沼泽湿地、鸟岛湖滨湿地、瓦颜山河源湿地为研究对象,通过高通量测序技术对土壤甲烷氧化菌进行检测。【结果】3种不同类型高寒湿地土壤甲烷氧化菌的优势菌门均为变形菌门(Proteobacteria)。鸟岛湖滨湿地与瓦颜山河源湿地的甲烷氧化菌α多样性存在显著差异(P<0.05),而小泊湖沼泽湿地与二者的甲烷氧化菌α多样性的差异不显著(P>0.05)。LEfSe分析表明,不同类型高寒湿地共存在40个差异菌群,尤以瓦颜山河源湿地差异菌群数量最多,从门到属水平均存在显著差异。冗余分析(redundancy analysis,RDA)表明,甲烷氧化菌菌群变化的主要驱动因子为土壤温度、土壤水分、电导率。【结论】整体而言,青海湖3种类型高寒湿地土壤理化性质及甲烷氧化菌群落多样性均存在差异,且部分菌群的相对丰度具有显著性差异(P<0.05)。     

黄河三角洲原生演替中土壤微生物群落结构分析

[目的] 黄河三角洲区域具有重要的湿地生态系统。碱蓬、野大豆和芦苇是该地区典型的盐生植物。本研究针对碱蓬、野大豆和芦苇混生植物的根际土壤微生物群落组成和功能基因进行了分析比较。[方法] 对碱蓬,野大豆-芦苇混生植物的根际微生物菌群和光滩土壤菌群进行了宏基因组测序,使用COG和KEGG数据库对微生物菌群的功能进行了注释和比较。[结果] 本研究结果表明,变形菌门是3个取样点的主要菌门,其在碱蓬、野大豆-芦苇根际土壤中的相对含量比光滩土壤分别多28.8%和10.6%。此外,拟杆菌门、放线菌门和芽单胞菌门是3个取样点中的优势物种。中华根瘤菌属是野大豆-芦苇混生植物根际土壤的最主要的属。对功能基因进行分析表明,光滩土壤中的功能基因的数量多于碱蓬根际土壤和野大豆-芦苇混生植物根际土壤的功能基因数。在这3个位点中,氨基酸代谢、碳水化合物代谢和能量代谢,以及无机离子转运和代谢的基因最多。[结论] 本研究为发掘有价值的微生物资源和海岸带盐碱土壤修复提供了一定的理论基础。     

Further reading in geomicrobiology

In the wetland rhizosphere, high densities of lithotrophic Fe(II)-oxidizing bacteria (FeOB) and a favorable environment (i.e., high Fe(II) availability and microaerobic conditions) suggest that these organisms are actively contributing to the formation of Fe plaque on plant roots. We manipulated the presence/absence of an Fe(II)-oxidizing bacterium (Sideroxydans paludicola, strain BrT) in axenic hydroponic microcosms containing the roots of intact Juncus effusus (soft rush) plants to determine if FeOB affected total rates of rhizosphere Fe(II) oxidation and Fe plaque accumulation. Our experimental data highlight the importance of both FeOB and plants in influencing short-term rates of rhizosphere Fe oxidation. Over time scales ca. 1 wk, the FeOB increased Fe(II) oxidation rates by 1.3 to 1.7 times relative to FeOB-free microcosms. Across multiple experimental trials, Fe(II) oxidation rates were significantly correlated with root biomass, reflecting the importance of radial O ₂ loss in supporting rhizosphere Fe(II) oxidation. Rates of root Fe(III) plaque accumulation (time scales: 3 to 6 wk) were ～ 70 to 83% lower than expected based on the short-term Fe(II) oxidation rates and were unaffected by the presence/absence of FeOB. Decreasing rates of Fe(II) oxidation and Fe(III) plaque accumulation with increasing time scales indicate changes in rates of Fe(II) diffusion and radial O ₂ loss, shifts in the location of Fe oxide accumulation, or temporal changes in the microbial community within the microcosms. The microcosms used herein replicated many of the environmental characteristics of wetland systems and allowed us to demonstrate that FeOB can stimulate rates of Fe(II) oxidation in the wetland rhizosphere, a finding that has implications for the biogeochemical cycling of carbon, metals, and nutrients in wetland ecosystems.     

The freshwater tidal wetland Liberty Island,CA was both a source and sink of inorganic and organic material to the San Francisco Estuary

It is hypothesized that perennial freshwater tidal wetland habitat exports inorganic and organic material needed to support the estuarine food web and to create favorable habitat for aquatic organisms in San Francisco Estuary. It is also hypothesized that most of the material flux in this river-dominated region is controlled by river flow. The production and export of material by Liberty Island were measured and compared using discrete monthly and continuous (15 min) measurements of a suite of inorganic and organic materials and flow between 2004 and 2005. Seasonal material flux was estimated from monthly discrete data for inorganic nutrients, suspended solids and salts, organic carbon and nitrogen and phytoplankton and zooplankton group carbon and chlorophyll a and pheophytin pigment. Estimates of material flux from monthly values were compared with measured daily material flux values for chlorophyll a concentration, salt and suspended solids obtained from continuous measurements (15 min) using YSI water quality sondes. Phytoplankton carbon produced within the wetland was estimated by in situ primary productivity. Most inorganic and organic materials were exported from the wetland on an annual basis, but the magnitude and direction varied seasonally. Dissolved inorganic nutrients such as nitrate, soluble phosphorus, total phosphorus and silica as well as total suspended solids were exported in the summer while total and dissolved organic carbon were exported in the winter. Salts like chloride and bromide were exported in the fall. Chlorophyll a and pheophytin were exported in the fall and associated with diatom and cyanobacteria carbon. Mesozooplankton carbon was dominated by calanoid copepods and exported most of the year except summer. Continuous sampling revealed high hourly and daily variation in chlorophyll a, salt and total suspended solids flux due to high frequency changes in concentration and tidal flow. In fact, tidal flow rather than river discharge was responsible for 90% or more of the material flux of the wetland. These studies indicate that freshwater tidal wetlands can be a source of inorganic and organic material but the export of material is highly variable spatially and temporally, varies most closely with tidal flow and requires high frequency measurements of both tidal flow and material concentration for accurate estimates.     

东海北部滨海湿地铁氧化细菌的分布及其对不同氧气穿透深度的响应

【目的】滨海湿地生态系统位于淡水与海水交互地带,含有高浓度Fe²⁺的地下水渗透到沉积物表层形成的湿地径流和周期性潮汐淹水形成的含氧-缺氧界面有利于铁氧化细菌介导的Fe²⁺的生物氧化过程发生。然而,目前缺乏对滨海湿地生态系统中铁氧化细菌类群的全面评估。【方法】以上海崇明西沙湿地公园及浙江舟山市朱家尖岛东沙沙滩两地共5处滨海湿地沉积物为研究对象,分析沉积物的氧气穿透深度等环境参数,并基于16S rRNA基因扩增子测序技术,全面解析不同滨海湿地生态系统中细菌与铁氧化细菌的群落组成与分布特征。【结果】与崇明西沙湿地相比,朱家尖岛东沙沙滩有更深的氧气穿透深度,达到10 mm以上。非度量多尺度分析(non-metric multidimensional scaling, NMDS)统计结果表明,细菌群落结构主要受到区域位置不同导致的环境条件差异的影响,而铁氧化细菌的群落结构则受到采样的区域位置和沉积物氧气穿透深度的共同影响。崇明西沙湿地和朱家尖岛东沙沙滩的优势细菌为蓝细菌门(Cyanobacteria)、γ-变形菌纲(Gammaproteobacteria)、拟杆菌门(Bacteroidetes)、α-变形菌纲(Alphaproteobacteria)和放线菌门(Actinobacteria);优势铁氧化细菌为嘉利翁氏菌属(Gallionella)、红细菌属(Rhodobacter)、Lepthothrix和Sideroxydans。【结论】通过对崇明西沙湿地和朱家尖岛东沙沙滩沉积物中栖息的铁氧化菌的调查发现,铁氧化细菌的群落组成与湿地沉积物类型导致的氧气穿透深度差异具有密切联系。     

Formation and growth of a heronry in a managed wetland in Doñana,southwest Spain

Capsule A newly created wetland has been beneficial for the breeding of five heron species and for the settlement and expansion of Glossy Ibises in the region.

Aim To determine whether created wetland would lead to the establishment of a heron and ibis breeding colony, and if so, to determine its effects on the distribution of these species in the wider region.

Methods Number of pairs breeding at the new wetland and in the region were estimated annually from 1996 to 2008. We investigated whether the growth of the new colony was explained by redistribution of breeding pairs within the region.

Results Purple Herons, Squacco Herons and Glossy Ibises colonised the new wetland in 1996. Black‐crowned Night Herons settled in 1998, while Cattle and Little Egrets were the last species to establish in the mixed colony in 2001. The population increase was particularly marked for Glossy Ibises (which had bred in Doñana only sporadically through the 20th century). Our findings suggest that simple redistribution of pairs does not explain the formation and growth of the new colony. Since the first year of establishment numbers of Glossy Ibises and Purple Herons have shown a significant growth trend at both the new colony and in Doñana.

Conclusion The creation and management of a new wetland has been successful for the conservation of heron and egret species and promoted the expansion of the Glossy Ibis population across the western Mediterranean region.     

Preliminary investigation of an integrated aquaculture–wetland ecosystem using tertiary-treated municipal wastewater in Los Angeles County, California

The objective of this study was to determine the feasibility of using a designed integrated aquaculture–wetland ecosystem (AWE) for experimental food production and inorganic nitrogen removal from tertiary-treated wastewater. The AWE connected polyculture aquaculture ponds with in-pond aquatic plant systems (water hyacinths, Eichhornia crassipes, and Chinese water spinach, Ipomea aquatica), a solar energy aeration system, and an artificial wetland. Ponds were stocked with hybrid tilapia (Oreochromis mossambicus×O. urolepis hornorum), common carp (Cyprinus carpio), mosquitofish (Gambusia affinis), and red swamp crayfish (Procambarus clarkii), and were flushed weekly with new wastewater at 20%. Fish were fed a 32% protein floating ration at 1% fish body weight per day, and wheat bran was added at 1 mg l⁻¹ when water conductivities exceeded 900 μmhos cm⁻¹. Plants were allowed to grow until they reached approximately 50% of the pond surface area, then maintained at this area by manual harvesting. Pond water quality (temperature, conductivity, pH, oxygen) was monitored twice daily, and weekly water samples were taken for analyses of inorganic nitrogen (ammonia and nitrate-N) in the ponds, wetland, and wetland discharge waters (n=30). Tilapia harvest from three ponds was 1134.5 kg. Fish standing crop biomass increased from 0.16 to 0.21 at stocking to 1.50–2.00 kg m⁻³ at harvest. Tilapia grew from an average stocking weight of 21 to 362–404 g at harvest but had poor survival (48–64%) due to heavy bird predation. Total food conversion ratios ranged 0.9–1.2. Approximately 70% of the tilapia were marketed live at $2.20 kg⁻¹. An estimated standing crop of 1.4 tons wet weight of Ipomea aquatica grew luxuriantly in one 200-m² polyculture pond which could be harvested sustainably at 20 kg week⁻¹. Water hyacinths removed approximately 90% of the ammonia and nitrate-N in wastewater, and the wetland removed an additional 7% (total removal was 97% of wastewater input concentrations). Overflow water exiting the wetland had less than 0.4 mg ammonia–nitrogen l⁻¹ and no detectable nitrate–nitrogen. The experimental AWE accomplished aquatic food production and almost complete removal of inorganic nitrogen from wastewater, functioning as a `quartenary' wastewater treatment/food production ecosystem. However, more rigorous experimentation is required to optimize fish- and plant-carrying capacities, nutrient cycles, and testing for bioaccumulation of metals in order for the AWE to be socially and economically relevant. The concept of using tertiary-treated wastewater for aquatic food production may be attractive in the peri-urban areas of many meagcities like Los Angeles, both for fish markets and to stem the growing discharges of wastewaters that are causing coastal pollution.     

Re-assessment of phosphorus availability in fens with varying contents of iron and calcium

Aim

To further unravel P availability in mineral-rich fens, and test whether high Fe in the soil would lead to low P availability to the vegetation.

Methods

Mesotrophic fens were selected over gradients in Ca and Fe in central Sweden and the Netherlands, to study characteristics of vegetation, pore water and peat soil, including inorganic and organic forms of P, Fe and Al.

Results

Soil Fe was more important than region or soil Ca, and P availability to the vegetation increased from Fe-poor to Fe-rich fens. Contrary to expectations, precipitation of iron phosphates played a minor role in Fe-rich fens. Fe-rich fens were P-rich for three reasons: (1) high P sorption capacity, (2) relatively weak sorption to Fe-OM complexes and (3) high amounts of sorbed organic P, which probably consists of labile P. Also, nonmycorrhizal wetland plants probably especially take up weakly sorbed (organic) P. However, high P did not lead to high biomass or low plant diversity. Fe-rich fens were limited by other nutrients, and high P may help protect the vegetation against Fe-toxicity.

Conclusions

Fe-poor fens are P-poor, irrespective of Ca, and Fe-rich fens P-rich even under mesotrophic conditions. However, high P itself does not endanger Fe-rich fens.

     

Information content of chemical structures and some possible biological applications

The purpose of this paper is to calculate the amount of information contained in a chemical or biological structure, and to estimate the energy needed for obtaining an organization unit. The first problem is solved by applying H. J. Morowitz's reasoning (Bull. Math. Biophysics,17, 81–86, 1955) and, for the second one, calculations based upon bond formation heat are carried out.Information content theoretical physical entropy, real physical entropy, informational entropy or negentropy entropic information or neginformation, heat amount, as well as relationships between these system parameters, are defined and used. The investigation covers 63 chemical substances (inorganic and organic compounds). The numerical results should show that common organized systems happen to be between two extreme kinds of systems: highly disordered systems and ideally organized systems. Some speculative numerical applications are carried out regarding chlorophyllian photosynthesis and information amount accumulated through biological growth. It seems that Information Theory may predict some biocalorimetric results.     

The Water Quality Consequences of Restoring Wetland Hydrology to a Large Agricultural Watershed in the Southeastern Coastal Plain

To ameliorate local and coastal eutrophication, management agencies are increasingly turning to wetland restoration. A large portion of restoration is occurring in areas that were drained for agriculture. To recover wetland function these areas must be reflooded and disturbances to soils, including high nutrient content due to past fertilizer use, loss of organic matter and soil compaction, must be reversed. Here, we quantified nitrogen (N) and phosphorus (P) retention and transformation in a unique large-scale (440 ha) restored wetland in the North Carolina coastal plain, the Timberlake Restoration Project (TLRP). For 2 years following restoration, we quantified water and nutrient budgets for this former agricultural field. We anticipated that TLRP would export high concentrations of inorganic P immediately following reflooding, while retaining or transforming inorganic N. In the first 2 years after a return to the precipitation and wind-driven hydrology, TLRP retained or transformed 97% of NO₃–N, 32% of TDN, 25% of NH₄–N, and 53% of soluble reactive phosphorus (SRP) delivered from inflows and precipitation, while exporting 20% more dissolved organic nitrogen (DON), and 13% more total P (inorganic, organic, and particulate P) than inputs. Areal mass retention rates of N and P at TLRP were low compared to other restored wetlands; however, the site efficiently retained pulses of fertilizer NO₃–N derived from an upstream farm. This capacity for retaining N pulses indicates that the potential nutrient removal capacity of TLRP is much higher than measured annual rates. Our results illustrate the importance of considering both organic and inorganic forms of N and P when assessing the benefits of wetland restoration. We suggest that for wetland restoration to be an efficient tool in the amelioration of coastal eutrophication a better understanding of the coupled movement of the various forms of N and P is necessary.     

Non-destructive approaches for assessing biofouling of household reverse osmosis membranes

Abstract

This study determined economic non-destructive methods to assess biofouling in point of use reverse osmosis (RO) membrane treatment systems. Three parallel household RO membrane units were operated under controlled feed water conditions to promote biofouling, inorganic fouling and a combination of both. Operational and biological parameters were monitored throughout the systems’ lifespan. Membrane autopsies assessed the degree and type of fouling. Statistical models determined statistically relevant parameters for fouling types that were validated with membrane autopsies. Permeate flow rates decreased differently with biofouling vs inorganic fouling. Large increases in permeate conductivity were noted in membranes suffering from biofouling and not in inorganically fouled membranes. The concentration of cell clumps from detached biofilm in the retentate increased in membranes experiencing biofouling and no increase was seen for inorganically fouled membranes. A combination of these methods could be used to conveniently assess the types of fouling experienced by RO systems.     

滇西北高原纳帕海湿地土壤氮矿化特征

采用树脂芯原位培育法,研究了纳帕海沼泽、沼泽化草甸和草甸土壤氮的矿化特征。结果表明,铵态氮（NH₄⁺-N）为沼泽、沼泽化草甸土壤中无机氮的主要存在形式,分别占无机氮含量的96.76%和75.24%,而硝态氮（NO₃^--N）为草甸土壤中无机氮的主要存在形式,占无机氮含量的58.77%。植物生长期内,纳帕海湿地土壤的净氮矿化速率表现为沼泽化草甸 > 草甸 > 沼泽,表明干湿交替的土壤环境更利于土壤氮矿化作用的进行,土壤中氮素有效性和维持植物可利用氮素的能力更强。整个生长季,沼泽和草甸土壤氮矿化为硝化作用,而沼泽化草甸土壤氮矿化为氨化作用。土壤硝态氮含量、有机质含量、碳氮比和含水量均对纳帕海沼泽、沼泽化草甸和草甸土壤的氮矿化产生显著影响。     

从宏基因组推测扎龙湿地未培养甲烷古菌Rice Cluster II的代谢途径与可能的盐碱适应性

【背景】湿地是重要的甲烷排放源,因为其中栖息着各种产甲烷古菌。已知未培养甲烷古菌Rice Cluster Ⅱ (RCⅡ)类群广泛分布于低温酸性和北方泥炭藓湿地、淡水湿地及草本沼泽等环境,但它们在低温盐碱湿地中的分布及代谢途径尚未知。【目的】分析扎龙盐碱湿地未培养甲烷古菌RCⅡ类群的多样性、推测产甲烷代谢途径及其潜在的盐碱适应机制。【方法】16S rRNA基因扩增子测序分析扎龙湿地土壤中甲烷古菌群组成;构建16S rRNA基因克隆文库分析扎龙湿地土壤RCⅡ的多样性;宏基因组分析推测RCⅡ古菌编码的产甲烷途径及与耐盐碱相关物质的合成基因。【结果】16SrRNA基因高通量测序发现未培养甲烷古菌的RCⅡ类群占扎龙盐碱湿地总甲烷古菌的13.280%±0.019%;系统发育学分析表明该湿地的RCⅡ由3个分支组成;宏基因组分析组装了2个优势的未培养RCⅡ的基因组,均含完整的氢还原二氧化碳产甲烷途径的基因,并编码海藻糖的转运与合成基因。【结论】扎龙盐碱湿地土壤富含未培养RCⅡ甲烷古菌,推测它们通过氢还原二氧化碳产甲烷,利用细胞内高的海藻糖适应盐碱环境。