渤海富营养化现状、机制及其与赤潮的时空耦合性

通过对历年调查与监测数据的整理,从污染物源强、渤海富营养化状况、赤潮发生的时空分布三个角度,分析了渤海近岸海域富营养化的"压力—状态—响应"耦合作用机制。根据文献及调查资料研究渤海营养要素的来源及通量,指出渤海污染物主要来自于陆源输入,并且以河流携带的营养盐输入为主。在对渤海近岸海域历年营养盐含量及富营养化水平分析的基础上,结合赤潮发生的时空变化特征,就富营养化对渤海赤潮的诱导作用与耦合关系进行初步讨论。     

巢湖藻类生物量季节性变化特征

在2008年对巢湖浮游藻类的生态分布进行了为期1 a的调查研究,并采用自制"藻类上浮/下沉捕集器"定量研究了水柱中藻类上浮和下沉速率的季节性变化.结果表明,蓝藻为巢湖主要的水华优势群落,但各个季节优势水华种群有所差别,春季鱼腥藻占优势,微囊藻次之;夏、秋两季微囊藻占绝对优势.5月开始,水柱中藻类生物量明显增加;8月份达到最大值,叶绿素含量全湖平均为146.37 mg.m-3.表层沉积物中藻类生物量在9.75～16.24 mg.kg-1之间,最小值出现在夏季,然后逐渐升高,最大值出现在冬季的11月.研究期间(5～10月),水柱中浮游藻类一直存在上浮和下沉现象,上浮速率在总体上呈先上升后下降的趋势,最大值出现在8月初,为0.036 8 mg.(m2.d)-1;下沉速率则呈现先缓慢上升后急剧下降的趋势,最大值出现在9月初,为0.032 1 mg.(m2.d)-1.多元逐步回归统计表明,温度是巢湖藻类生物量变化最为显著的影响因子,其次为总氮(TN)和总磷(TP).     

Alga-lysing bioreactor and dominant bacteria strain

Alga-lysing bacteria have been paid much attention to in recent years. In this study, the alga-lysing strain P05 which was isolated from an immobilizing biosystem was immobilized by coke and elastic filler, forming two biological reactors. The removal efficiencies of algae, NH4^＋-N and organic matter using the two reactors were studied. The results showed that strain P05 was an ideal algal-lysing bacteria strain because it was easy to be immobilized by coke and elastic filler which are of cheap, low biodegradability and the simple immobilization procedure. After 7 d filming, the biological film could be formed and the reactors were used to treat the eutrophic water. These two reactors were of stability and high effect with low cost and easy operation. The optimal hydraulic retention time （HRT） of each reactor was 4 h. The algae removal rates were 80.38% and 82.1% （in term of Chl-α） of coke reactor and filler reactor, respectively. And that of NH4^＋-N were 52.3% and 52.7%. The removal rates of CODMn were 39.03% and 39.64%. The strain P05 was identified as Bacillus sp. by PCR amplification of the 16S rRNA gene, BLAST analysis, and comparison with sequences in the GenBank nucleotide database.     

Topsoil organic carbon mineralization and CO2 evolution of three paddy soils from South China and the temperature dependence

Carbon mineralization and its response to climatic warming have been receiving global attention for the last decade. Although the virtual influence of temperature effect is still in great debate, little is known on the mineralization of organic carbon （SOC） of paddy soils of China under warming. SOC mineralization of three major types of China＇s paddy soils is studied through laboratory incubation for 114 d under soil moisture regime of 70% water holding capacity at 20℃ and 25℃ respectively. The carbon that mineralized as CO2 evolved was measured every day in the first 32 d and every two days in the following days. Carbon mineralized during the 114 d incubation ranged from 3.51 to 9.22 mg CO2-C/gC at 20℃ and from 4.24 to 11.35 mg CO2-C/gC at 25℃ respectively; and a mineralizable C pool in the range of 0.24 to 0.59 gC/kg, varying with different soils. The whole course of C mineralization in the 114 d incubation could be divided into three stages of varying rates, representing the three subpools of the total mineralizable C： very actively mineralized C at 1-23 d, actively tnineralized C at 24--74 d and a slowly mineralized pool with low and more or less stabilized C mineralization rate at 75-114 d. The calculated Q10 values ranged from 1.0 to 2.4, varying with the soil types and N status. Neither the total SOC pool nor the labile C pool could account for the total mineralization potential of the soils studied, despite a well correlation of labile C with the shortly and actively mineralized C, which were shown in sensitive response to soil warming. However, the portion of microbial C pool and the soil C/N ratio controlled the C mineralization and the temperature dependence. Therefore, C sequestration may not result in an increase of C mineralization proportionally. The relative control of C bioavailability and microbial metabolic activity on C mineralization with respect to stabilization of sequestered C in the paddy soils of China is to be further studied.     

刘家峡水库水环境质量生物学评价研究

2008年黄河丰水期和2009年黄河枯水期,对研究区6处标志性区域进行随机采样,采用活体观察和固定染色法鉴定藻类种类,直接计数法统计藻类数量,共鉴定到藻类114种(包括22个未定名物种),隶属于9门11纲17目34科55属。其中,硅藻门47种,占41.22%,以无壳缝目为优势类群;绿藻门24种,占21.05%,为次优势类群;蓝藻门,金藻门,裸藻门为常见类群;隐藻门、甲藻门和黄藻门均为罕见类群。利用藻类群落结构特征、优势种类、藻类污染指数和污生指数等指标对刘家峡水库水质进行评价,结果表明:刘家峡水库水质在1#、2#样区较清洁,3#、4#样区为轻-中度污染,5#、6#样区为重度污染,与采用粪大肠肝菌、DO指标评价结果具有良好一致性。     

滇池蓝藻快速热解液化制取生物油的初步研究

文章采用实验室规模的固定床反应器作为实验平台,对蓝藻快速热解液化制取生物油的可行性进行了探讨,并对影响液化性能的诸多因素,如热解温度(300～700℃)、载气流量(0～400 mL/min)、原料粒径(d＜0.08 nn,0.15＜d＜0.25 mm,0.25＜d＜0.38 mm,0.38＜d＜3.35 mm,d＞3....     

地表水中藻类代谢对pH和含氧量影响分析

藻类代谢对地表水中含氧量和pH均产生影响。藻类光合作用放出氧气,导致地表水中的含氧量增加。藻类光合作用吸收二氧化碳,影响地表水中碳酸及碳酸盐的平衡,导致地表水中pH偏向碱性。地表水中存在的弱酸及弱酸盐也会影响地表水中pH的变化。在同样的光合作用条件下,如果地表水中碳酸及碳酸盐浓度高,则pH变化小;如果地表水中碳酸及碳酸盐浓度低,则pH变化大。     

明矾石在水体微藻去除中的应用研究

以温州市某大学校区内富营养化水体为研究对象,采用本地明矾石对含藻水体进行混凝除藻、除浊实验研究,分别进行投加量、搅拌强度、搅拌时间、静置时间及pH值对微藻去除效率的影响研究,以获得处理工艺的最佳条件,为恢复河流水体生态自净功能提供理论基础.试验中对投加明矾石前后,水体中浊度、总磷、氨氮和总氮进行了测定,结果表明：明矾石最佳投加量为0.35 g/L,最佳搅拌方式为200 rpm搅拌4 min;最佳静置时间为25 min;在碱性或中性水体的处理效果尤佳.     

周期性的温度扰动对藻类群落结构演替的影响

为了研究水库生境扰动对藻类水华的作用机制,以中度扰动理论为基础,结合藻类群落生境选择学说和藻类生态功能组,开展了不同温度扰动周期、相同扰动幅度下藻类多样性变化特性和群落结构演替特征的室内控制实验.结果表明:1适度的扰动会促进藻类的生长且增加其多样性.中度扰动组Δ22℃/48 h藻类生物量最大,但多样性最高,不存在绝对占优藻种,而高频次扰动组Δ22℃/24 h生物多样性较小,但可降低藻类生物量.2温度的周期性变化对浮游藻类群落的演替有明显的影响,优势种也呈现一定的差异性.藻类优势功能组演替基本规律为:X_1(小球藻)→J(栅藻)→S_1(席藻)或X_2(衣藻),群落结构呈现出C/CR型藻类先行占优向R型演替的趋势.高温扰动频繁时,R型藻类(S_1)明显占优;无扰动或低扰动时,群落结构组成特点以C/R策略为主.适度的扰动组Δ22℃/48 h形成了多种生长策略的藻类共存的格局,且耐受高温胁迫的S策略藻类(L_0)开始出现.     

长期暴露下纳米二氧化钛对典型淡水藻体砷累积与生物转化的影响

以铜绿微囊藻(Microcystis aeruginosa)和斜生栅藻(Scenedesmus obliquus)为研究对象,通过室内培养实验,研究了长期暴露下纳米二氧化钛(nano-TiO_2)对五价砷[As(Ⅴ)]在典型淡水藻体中累积与生物转化的影响.结果表明不同藻类对无机砷的吸收和转化能力差异很大.长期暴露下斜生栅藻累积的砷(As,以DW计,下同)高达(819.66±11.25)μg·g-1,比铜绿微囊藻累积的As[(355.95±8.31)μg·g-1]高2倍多.Nano-TiO_2可增加藻体对As的吸收累积,降低了培养基中As的含量.同时,nano-TiO_2可增加藻体对As(Ⅴ)的生化转化;其中,铜绿微囊藻中有机砷以二甲基砷(DMA)为主,而斜生栅藻中有机砷以一甲基砷(MMA)为主.另外,长期暴露下nano-TiO_2处理的铜绿微囊藻和斜生栅藻向培养基释放的甲基砷小于对照组,表明长期暴露中的nano-TiO_2不能促进藻体内甲基砷的释放.研究结果可促进nano-TiO_2与As相互作用时生态风险的理解.