沉积物间隙水溶解态磷和铁（Ⅱ）高分辨同步分析方法的研究

沉积物具有高度的空间异质性,尤其在沉积物-水界面附近的微环境中,溶质在微小尺度上可能存在强烈的浓度梯度分布,需要借助高分辨的获取技术才能表征。本研究发展了一种沉积物微界面溶解态反应性磷（Dissolved Reactive Phosphorus,DRP）和溶解态铁（Ⅱ）的同步分析方法。利用分辨率为4 mm、平衡时间仅为2 d的微型间隙水平衡装置（Peeper装置）获取微量间隙水（～100μL·样品-1）,采用384微孔板微量比色法分别测定同一间隙水样品中的DRP和溶解态铁（Ⅱ）的质量浓度,单一指标所消耗的间隙水体积由5 mL减少到仅～40μL,检出限分别为0.009和0.017 mg·L-1,精密度为1%～7%,均与常规方法相近。将该分析方法应用到太湖两个湖区的沉积物中,同步获得的微界面溶解态磷和铁（Ⅱ）的分布较好地反映了两者的关系。     

夏、秋季长江口外海域沉积物-水界面溶解无机碳的交换通量

沉积物-海水界面是海洋中溶解无机碳(DIC)转移和储存的重要场所，长江口外海域拥有特定的沉积物-水界面交换的空间格局，研究其沉积物-水界面DIC的交换过程对于碳的循环和转化具有重要意义.本研究于2021年8月和2021年10月在长江口外海域采集沉积物样品及原位底层海水，通过实验室模拟培养法计算了该海域沉积物-水界面DIC的交换通量，并研究了沉积物间隙水-上覆水的DIC浓度差、温度、盐度和pH对DIC交换通量的影响.结果表明，夏季和秋季研究海域沉积物-水界面DIC交换通量平均值分别为(432.45±190.78)μmol·m^-2·h^-1和(223.05±110.39)μmol·m^-2·h^-1.夏季交换通量高于秋季，DIC扩散方向均由沉积物向上覆水释放，表明沉积物表现为DIC的“源”.此外，交换通量会随着DIC浓度差或温度升高而升高，随着盐度或pH升高而降低.     

铀胁迫对大豆与玉米幼苗细胞DNA损伤的彗星试验研究

以铀浓度为1000 μmol·L-1、800 μmol·L-1、600 μmol·L-1、400 μmol·L-1、200μmol·L-1和100μmol·L-1的6组铀溶液和对照组(0μmol·L-1)培养大豆和玉米幼苗,采用彗星试验研究铀胁迫对大豆和玉米幼苗细胞DNA的损伤情况.试验结果表明,铀浓度为1 000 μ...     

Mn对超富集植物青葙Cd毒害的缓解效应

为了探究Cd胁迫下青葙中Mn的生理作用,通过水培实验,研究在Cd暴露下(0、5和25 μmol·L-1 )施加Mn(5、100和1 000 μmol·L-1 )对青葙的干重、叶绿素含量、Cd含量和青葙根部不同区域实时Cd2+流速的影响.结果表明,提高Mn的供应水平可缓解Cd对青葙生长的抑制效应.在Cd浓度为5 μmol·L-1 ,施加1 000 μmol·L-1的Mn时,青葙的根、茎、叶干重和总干重分别增加了26.8% 、11.8% 、22.7%和21.19% .当Cd处理浓度为25 μmol·L-1时,1 000 μmol·L-1的Mn显著增加了青葙的叶绿素a和总叶绿素的含量(P＜0.05).相反地,Mn的添加显著减少了叶片中的丙二醛含量(P＜0.05).在Cd处理为5 μmol· L-1和25 μmol·L-1时,施加Mn使丙二醛含量降低了30% .这表明,Mn浓度的增加能够减少Cd对青葙的脂质过氧化伤害,保护叶绿素. Mn对青葙Cd积累的影响并不是严格的拮抗效应.在低Cd浓度(5 μmol·L-1 )处理组中,Mn的添加对青葙Cd累积无显著影响(P＞0.05).在高浓度处理时(25 μmol·L-1 Cd),1 000 μmol·L-1的Mn显著降低了青葙根、茎和叶的Cd含量(P＜0.05),较施加5 μmol·L-1 Mn处理分别降低了41.4% 、41.5%和23.3% .这可能与Mn2+抑制青葙根系对Cd2+的吸收有关.非损伤微测技术(NMT)分析结果显示,Mn2+的添加显著抑制了根表面Cd2+的内流速率.当加入50 μmol·L-1的Mn时,距根尖200 μm的Cd2+的内流速率下降了71.4% .上述结果表明,施加Mn有效地缓解了Cd对青葙的毒性效应.     

不同地质背景下土壤溶解有机碳含量的季节动态及其影响因子

为了解岩溶区和非岩溶区土壤溶解有机碳(DOC)含量及其季节动态是否存在差异,为今后相关研究提供研究依据,作者用0.5mol·L-1K2SO4浸提法分析测定了广西桂林市灵川县潮田乡毛村由泥盆系融县组灰岩(D3r)发育石灰土、砂页岩(D2l)发育红壤中溶解有机碳的含量及其季节动态变化,并分析了其与影响因子的相互关系。结果表明:石灰土中溶解有机碳的质量分数为:19.3675～143.2524mg·kg-1,红壤的为:221.1652～1016.602mg·kg-1,石灰土因其偏碱、高钙镁、高有机质含量的特性而使得DOC含量远低于非岩溶区红壤的含量;石灰土和酸性土DOC含量在秋季都达到最高值,在冬季或春季含量最低;在空间分布上都随土壤深度增加而降低。岩溶区及非岩溶区土壤DOC含量的季节动态变化可以划分为4个阶段:①9—10月高温少雨,植物凋落物增多,DOC含量在一年中最高;②11月-12月,气温迅速降低,微生物活性随之降低,DOC含量下降;③12月底—4月,前期(12月至次年2月)DOC浓度随土壤有机质含量的增加而增加;后期(3—4月)气温回升,降雨频繁,生物复苏,生物活动旺盛,土壤DOC含量迅速增加;④5—8月,高温多雨,DOC转化为CO2释放出来,部分DOC随雨水淋失,土壤中DOC总含量不高。     

西江水体中多环芳烃的分布特征及来源

为确定西江水体中多环芳烃(PAHs)的分布特征和来源,分别在洪水期(2003年8月)和枯水期(2003年11月)对西江水体进行了两次水柱采样,利用气相色谱-质谱(GC-MS)对样品中15种优控的PAHs进行定量分析,并运用分子比值法探寻多环芳烃的来源.结果表明,西江水体溶解相和颗粒相中PAHs的质量浓度分别为21.7～138 ng·L-1,和40.9～238 μg·kg-1.水体中PAHs的总质量浓度(溶解相及颗粒相),洪水季(43.9～116.9 ng·L-1)大于枯水季(25.2～34.1 ng·L-1).溶解相和颗粒相中PAHs质量浓度都表现相同的垂直变化即中层>下层>上层.从PAHs组成特点来看,溶解相以3环的PAHs为主,占总组分的80%;而颗粒相以3环、4环的PAHs为主,分别占总组分的48%和41%.西江水体PAHs的质量浓度,与欧洲其他一些低污染水域相比相对较高;而低于国内一些主要受污染河流.分子比值法表明,西江水体PAHs主要来源于高温燃烧排放.     

米氏凯伦藻对氮源的吸收利用特征

对不同氮源的吸收利用特征在一定程度上决定了藻类的生长策略和种群生物量,采用单因子实验,以NaH2PO4作为唯一磷源,固定初始磷浓度为0.65 μmol·L-1,选用硝酸钠、亚硝酸钠、氯化铵和尿素分别作为氮源进行批次培养,对比研究米氏凯伦藻(Karenia mikimotoi)在不同氮源不同氮磷浓度比(cN/cP)条件下的吸收利用特征.结果表明:当cN/cP为80时,米氏凯伦藻细胞数量增长明显,对硝酸钠、亚硝酸钠、氯化铵和尿素的吸收量分别为51.64 μmol·L-1、29.28 μmol·L-1、42.17μmol·L-1、41.42 μmol·L-1.4种氮源对米氏凯伦藻的营养价值存在差别,其由大至小的排列顺序依次为:硝酸钠,尿素,亚硝酸钠,氯化铵.     

模拟太阳光下冰相中壬基酚的光解

本文采用模拟太阳光对比研究了HONO和H2O2体系冰相中壬基酚的降解.考察了模拟太阳光作用下冰相中壬基酚的光转化规律,讨论了壬基酚初始浓度、pH、光照时间对壬基酚去除率的影响.结果表明,初始浓度降低、光照时间延长、pH值升高,壬基酚直接光解时的去除率升高.初始浓度为0.025 mmol·L-1的壬基酚在冰相中直接光解12 h,去除率达36.7%.外加H2O2时,冰相中壬基酚光解受到一定的抑制,且H2O2剂量增加,壬基酚去除率下降.而HONO吸收UV解离出的·OH自由基,促进了冰相中壬基酚的光转化.     

地下环境中铁氧化物生物异化还原耦合降解硝基苯的影响因素研究

通过静态实验模拟地下水厌氧环境,研究了碳源、电子受体、初始微生物量和硝基苯浓度等因素对地下环境中微生物异化铁还原作用耦合降解硝基苯的影响。实验选取乙酸铵、葡萄糖、柠檬酸铵为碳源,针铁矿、赤铁矿为电子受体,进行异化铁还原协同耦合降解硝基苯。结果表明：乙酸铵为碳源时硝基苯的降解率最高为78.5%;针铁矿作电子受体时硝基苯降解效果比赤铁矿好,且0.3 mg·L-1效果最好;微生物量对耦合体系中硝基苯降解率有影响但并不显著,最适宜的初始微生物量为4×108cells·mL-1;硝基苯质量浓度在50～150 mg·L-1时,硝基苯浓度与降解率呈负相关,其中对50 mg·L-1的初始硝基苯质量浓度降解效果最好。因此,碳源和电子受体对地下环境中微生物异化铁还原作用耦合降解硝基苯具有重要的影响。     

城市污水中典型卤代苯酚分布及其光降解行为研究

卤代苯酚(HPs)是一类广泛存在于水体中的污染物,其在污水处理厂出水中的存在及迁移转化会产生一定的健康和生态风险。探究卤代苯酚在环境中的转化行为非常重要。光降解反应是酚类物质在水体中迁移转化的重要途径,实际水体中的有机质等对卤代苯酚的光降解会产生一定的影响。对大连市区6家污水处理厂出水中卤代苯酚的污染状况进行了调查,结果显示在所有出水中总HPs的浓度范围为77.2~168.6 ng·L-1。在所有检出的卤代苯酚中,五氯酚和2,6-二氯酚浓度较高,且检出频率均为100%,检出浓度范围分别为10.8~166.7 ng·L-1和0.1~72.2 ng·L-1。在模拟太阳光照射条件下,选取2种氯酚和2种溴酚研究它们在污水样品与纯水中光降解行为,从卤原子取代的程度和种类两方面对不同卤代苯酚光降解的规律进行类比,分析了其光降解特性。此外,对比分析了不同污水厂出水的对同种卤代苯酚降解速率的影响,发现出水的p H值、溶解性有机质等因素,都可能影响卤代苯酚的光降解。     

Automatic potentiometric determination of dissolved oxygen

Commercially available automatic titration systems were tested in 1988 for potentiometric titration of liberated iodine by the Winkler method of oxygen determination. The potentiometric equivalence point was also compared to the manual starch end point. Finally the automatic method was used in order to estimate belowhalocline respiration in the Kattegat, Sweden. Standard deviations of 0.007 ml O₂ l^–1 or 0.1 to 0.3% coefficients of variation (% standard deviation of the mean) were achieved when titrating 25 ml from replicate 60-ml oxygen bottles using the automatic method, or 50 ml manually. The precision for replicate titrations of 50-ml aliquots of 0.001N KIO₃ was <0.05% (0.002 ml 0.01N Na₂S₂O₃) for the automatic method. Titration time for 25-ml aliquots was 2 to 4 min, somewhat longer than for manual titrations (1 to 1.5 min). However, during titration the operator is free to perform other tasks. It is not possible to use automatic sample changers, due to rapid iodine volatilization. The equipment can be handled by relatively unskilled analysts and is suitable for use on board research vessels or in field stations [weight for a Mettler^TM titrator (Mettler Instrumente AG, Greifensee, Switzerland) <10 kg, volume <0.1 m³]. Below-halocline oxygen consumption in the SE Kattegat ranged from 0 to 6 ml O₂ m^–3 h^–1 (mean values for September and October 1988=1.69 and 0.66 ml O₂ m^–3 h^–1, respectively, with 95% confidence limits of ca. ±0.6 ml O₂ m^–3 h^–1).     

土壤溶解性有机质的生态环境效应

土壤生态环境是一个复杂的多介质多界面体系。现有的研究表明，DOM作为环境中重要的天然配位体和吸着载体，是一种非常活跃的化学物质，它将土壤中的矿物质、有机质与生物成分联系在一起，通过物理或化学作用改变金属与外源性化合物的环境行为，促进温室气体的排放，调节土壤养分流失，指示土壤质量，并对成土过程、微生物的生长代谢过程、土壤有机质分解和转化过程有着重要作用，已经成为土壤科学、生态科学和环境科学交叉领域的研究热点。文章系统地评述了DOM的组成特点及其环境效应，同时介绍了未来的研究方向及一些有待于进一步研究的问题。     

Exudation of dissolved organic carbon by brown algae

The release via exudation of dissolved organic carbon by Ascophyllum nodosum (L.) Le Jol. was investigated under laboratory conditions. In contrast to results previously reported by Sieburth (1969), continuous release of organic matter was found with only 1 specimen out of 21 tested either in stagnant sea water or in sea water flowing through the system. The holdfast of the plants was found to release relatively large amounts of organic material; however, this release lasted only for short periods, and was most probably due to damage caused by removing the plants from their substrate. The possible reasons for the failure to detect exudation are discussed. With Fucus vesiculosus L., no reliable results could be obtained, most probably due to particulate matter sloughing off the plants during the washings and during the experiments under conditions of photosynthesis.     

Availability of dissolved free glucose to heterotrophic microorganisms

In 5 different aquatic biotopes, widely differing in salinity as well as in degree of eutrophication and pollution, the concentration of dissolved free glucose was measured employing ion exchange chromatography of sugar borate complexes. The concentrations of glucose ranged from 4.99 to 9.63 g C 1^-1. No correlation between the amounts of glucose and the trophic character of the biotope was evident. The parameter K_t+S_n (sum of the transport constant and the natural concentration of glucose) was determined using a microbiological method. Instead of being larger, the K_t+S_n values were smaller than the concentrations obtained chemically. The range was between 0.62 and 2.72 g glucose- C 1^-1. Expressed as percentages the K_t+S_n values were between 6.4 and 30.5% of the concentrations of glucose alone. No gross errors of the microbiological and chemical methods seem to be responsible for these large discrepancies, since internal standardization gave excellent results. Two reasons might account for the discrepancy: (1) Not all of the dissoved free glucose (existing as truly free, absorbed or complexed free glucose) is available to the heterotrophic microorganisms. (2) During the relatively short duration of the experiments, the added ¹⁴C-labelled glucose may not be proportionally distributed between the different fractions of the dissolved free glucose. Instead, the fraction of the truly free glucose might be higher specifically labelled than the absorbed and complexed ones. This would lead to an over-representation of the presumably small fraction of the truly free form. It is concluded that using the concentration of the dissolved free substance obtained by chemical analysis to calculate the flux might be misleading.Publication No. 282 of the Joint Research Program at the Kiel University (Sonderforschungsbereich 95 der Deutschen Forschungsgemeinschaft)     

焦化废水中溶解性有机物组分的特征分析

焦化废水是典型的具有复杂有机质的工业废水,其复杂的有机构成制约了水处理的水质达标,且可能对排入水体构成危害.为了探明其溶解性有机物的组成,采用XAD-8大孔树脂将焦化废水中的溶解性有机物分为亲水性组分(HIS)、疏水酸性组分(HOA)、疏水碱性组分(HOB)和疏水中性组分(HON),分析了各组分的溶解性有机物(DOC)、紫外-可见光谱、色度,并采用GC/MS对各组分中有机物进行定性分析.结果表明,焦化废水中的有机物主要为HIS和HOA组分,其DOC含量分别占总DOC的44.3%和32.4%;焦化废水在200—250 nm和300—400 nm范围内有特征吸收峰,且吸收光强度顺序为HIS>HOA>HON>HOB;焦化废水的色度主要由HOA和HON构成,其在525 nm和436 nm处的吸光度分别占焦化废水吸光度的42.9%(HON)、42.1%(HON)和21.4%(HOA)、15.8%(HOA);焦化废水中亲水性物质主要是苯胺、苯酚、喹啉、异喹啉,疏水酸性物质中主要是各种甲基取代的酚类物质,疏水碱性物质主要是各种胺类和含氮杂环化合物,疏水中性物质主要是吲哚及其衍生物.     

Mathematical models of dissolved oxygen concentration in fresh water

An adequate reserve of dissolved oxygen in a receiving stream is extremely important for protecting aquatic plants and animals, and for conserving our water resources. This paper briefly describes the environmental engineering significance of the stream self-purification, the current stream quality standards on dissolved oxygen concentration, and the solubility of dissolved oxygen in water. Special emphasis is placed on the modelling of the biological reactions and the dissolved oxygen saturation concentration in fresh water. The model can be used for calculating the dissolved oxygen saturation concentration, in turn, for determining the dissolved oxygen deficits, the critical dissolved oxygen concentration, and the allowable dissolved oxygen drop in a stream into which the waste water is discharged.     

Release of dissolved organic matter by some marine macrophytes

The amount of photoassimilated carbon released as dissolved organic carbon was investigated for 5 species of benthic marine macrophytes (Thalassia testudinum, Diplanthera wrightii, Acanthophora spicifera, Chondria dasyphylla, and Dictyota dichotoma) and 1 species of pelagic marine macrophyte (Sargassum natans). Release rates ranged between 0.006 and 0.053 mg C g^-1 h^-1. Percent release values ranged from 1.1 to 3.8%. Spermatophytes had slightly lower percent release values than algae. Investigations performed on the ability of release products to be utilized by heterotrophic organisms showed that 20 to 30% of the released organic carbon was assimilated within a 2-h period.     

NMR spectroscopy of dissolved organic matter: a review

Environmental Chemistry Letters - The presence of liquid water makes our planet habitable. Water in soils, sediments, lakes, rivers and the ocean forms the largest habitat for life on Earth. During...     

Pretreatment for dissolved organic nitrogen testing by gas stripping

ABSTRACT

Total dissolved nitrogen (TDN), including dissolved inorganic nitrogen (DIN) and dissolved organic nitrogen (DON), is of significant importance in aquatic systems due to its roles in numerous environmental processes, such as nutrients for agriculture activities, sources for lake and estuary eutrophication, and one of the major factors contributing to disinfection byproduct formation. The distribution and impact of DIN on these processes are relatively well-understood; however, information on DON is extremely limited, as there is no direct method for its quantification. DON is conventionally determined by subtracting DIN from TDN. However, significant errors may be introduced if DIN is the predominant species in samples with high concentrations of TDN. In order to deal with this challenge, pretreatment method for nitrogen gas stripping was investigated using 56 water samples collected from various ecosystems. The results indicated that after nitrogen gas stripping pretreatment, removal % of ammonia nitrogen (NH₃–N) was more than 87.5%, and the ratios of removal of NH₃–N/removal of TDN (β) were over 86.5% for most of 56 samples with high [NH₃–N], indicating a high efficiency for removal of NH₃–N, and that NH₃–N was the predominant nitrogen species removed for the samples with high [NH₃–N]. Therefore, nitrogen gas stripping is an appropriate pretreatment method for DON testing when NH₃–N is the dominant inorganic nitrogen species.     

淡水水体溶解有机氮对有毒藻种的生物有效性

溶解有机氮(Dissolved organic nitrogen,DON)是多数天然水体中溶解氮的主要组成部分。天然水体DON是许多微生命体包括有毒藻种的氮营养源,在供水安全以及水体富营养化等方面的生态环境效应不容忽视。文章系统地介绍了淡水水体DON含量与来源、生物有效性与估算方法,以及对有毒藻种生长的影响。DON的来源是影响水体中DON含量动态特征的关键因素。DON来源包括陆地径流,植物碎屑,土壤淋溶液,沉积物释放,大气沉降,藻类、大型植物、细菌与细胞死亡或自我分解,微型及大型浮游动物捕食和排泄、分泌物释放等。研究表明约有12%～72%的DON可迅速被生物所利用,具显著差异,究其原因可能是其来源组成、化学本质(分子质量与极性)、测试生物组成、是否有细菌作用等因素造成的。不同藻种具有不同氮源利用能力,DON对藻类生长具有直接或间接的作用,并可能影响藻类群落结构(有毒藻类成为优势种)。考虑到水环境保护与饮用水安全供水的重要性,未来研究应重视淡水水体DON生物有效性与其化学本质的揭示,尤其是对有毒藻种。