浙中典型富硒土壤区土壤硒含量的影响因素探讨

通过对浙江省中部典型富硒土壤区的系统调查研究,总结了影响土壤硒含量的主要因素.结果表明,地质背景对土壤硒含量有控制作用,汤溪组、之江组和金华组分布区的土壤硒含量明显高于其他地质背景区.研究同时发现,土地利用方式对土壤硒的迁移富集有不可忽视的影响,旱地土壤比水田土壤更易富集硒元素.由于土壤有机质对硒的吸附与固定作用,致使其成为影响硒含量的重要因素之一.除此之外,研究认为土壤质地也是影响土壤硒含量的重要因素,土壤中黏粒含量越多,越黏重,硒含量往往较高.     

水体悬浮颗粒物对斜生栅藻生理生化及光合活性的影响

通过研究不同浓度(30、40、50、60、70 mg·L-1)和不同粒径(0～75μm、75 ～ 96μm、96 ～150 μm、150～ 250 μm)水体悬浮颗粒物对斜生栅藻(Scenedesmus obliquus)叶绿素a含量、抗氧化系酶活性、脂质过氧化物丙二醛(MDA)含量、可溶性蛋白含量及光合参数变化的影响,探讨了水体悬浮颗粒物对斜生栅藻生理生化及光合活性影响的机制.结果表明,预处理与未处理悬浮颗粒物在一定浓度范围内会促进藻类生长,超过各自临界浓度(预处理为40 mg·L-1、未处理为50 mg·L-1)后,随着颗粒物浓度的增加会对藻类生长产生抑制现象未经处理的相同浓度不同粒径颗粒物对斜生栅藻都表现出抑制作用,0～75μm粒径组颗粒物作用下藻体内超氧化物歧化酶(SOD)、过氧化氢酶(CAT)、MDA和可溶性蛋白质含量等均显著区别于其他粒径组的作用(p＜0.05).经过预处理的相同浓度不同粒径颗粒物中,96～150μm粒径组对藻类的生长抑制较其他粒径组明显,且小粒径组颗粒物对藻类体内SOD、CAT、MDA和可溶性蛋白质含量等影响较大.受不同浓度悬浮颗粒物胁迫的斜生栅藻相对电子传递速率随着时间延长在一定程度上降低,但这种抑制作用在藻细胞的耐受范围,藻细胞可以通过自身调节将电子传递速率恢复到正常水平甚至更高以抵抗逆境环境.     

太湖梅梁湾和月亮湾春夏两季沉积物扰动下BAPP的转化规律

采用室内模拟试验研究了沉积物扰动下上覆水中可被生物利用颗粒态磷(BAPP)的变化规律,并分析了BAPP与悬浮物中内源磷间的内在联系.试验用沉积物分别于春季和夏季采自太湖梅梁湾和月亮湾.结果表明,沉积物扰动降低了上覆水中生物有效磷(BAP)含量,降至初始状态的40%左右.BAPP也明显降低,其占BAP的百分比稳定在50%左右,梅梁湾春季除外.扰动状态下颗粒态磷(PP)生物有效性显著降低,第12h时,BAPP占PP的百分比仅为10%左右;这与悬浮物中NH₄Cl-P和Fe/Al-P的降低明显相关,但其与 (AAP+NH₄Cl-P)占Tot-P的百分比相关性更好[r=0.565(n=48)].这暗示,沉积物扰动可能延缓了水体富营养化发展进程.     

黄河三角洲碱蓬湿地土壤有机碳及其组分分布特征

应用物理分组方法研究了黄河三角洲典型碱蓬湿地土壤有机碳及其组分分布特征.结果表明,研究区土壤重组有机碳是土壤有机碳的主要组成部分,土壤重组有机碳含量、土壤颗粒有机碳含量与土壤总有机碳含量都显著正相关.研究区土壤轻组组分比例和含量范围分别在0.008%～0.15%和0.10～0.40 g·kg-1,颗粒有机碳分配比例范围为8.83%～30.58%,说明黄河三角洲碱蓬湿地土壤有机碳中非保护性组分较低,碳库相对稳定.     

Removal and transformation of organic matters in domestic wastewater during lab-scale chemically enhanced primary treatment and a trickling filter treatment

To find a simple and economical way for treating the domestic wastewater in small counties and towns, a process combining chemically enhanced primary treatment and a trickling filter (CEPT-TF, representing the physical and biological effects) was constructed and operated in laboratory conditions. The characteristic behaviors of dissolved organic matter in raw wastewater and effluents were examined during steady-state operation. Experimental results showed that the process of CEPT and TF in series was beneficial for the removal of hydrophobic and hydrophilic organics. Specially, the hydrophobic and aromatic materials could be preferentially removed in the CEPT unit, and the hydrophilic fraction in the TF. Structural changes of the organic fractions during the operation of the different units were also characterized via spectrum analysis.     

Influence of dissolved organic matter character on mercury incorporation by planktonic organisms：An experimental study using oligotrophic water from Patagonian lakes

Ligands present in dissolved organic matter （DOM） form complexes with inorganic divalent mercury （Hg^2＋） affecting its bioavailability in pelagic food webs. This investigation addresses the influence of a natural gradient of DOM present in Patagonian lakes on the bioaccumulation of Hg^2＋ （the prevailing mercury species in the water column of these lakes） by the algae Cryptomonas erosa and the zooplankters Brachionus calyciflorus and Boeckella antiqua. Hg^2＋ accumulation was studied through laboratory experiments using natural water of four oligotrophic Patagonian lakes amended with^197Hg^2＋. The bioavailability of Hg^2＋ was affected by the concentration and character of DOM. The entrance of Hg^2＋ into pelagic food webs occurs mostly through passive and active accumulation. The incorporation of Hg^2＋ by Cryptomonas, up to 27% of the Hg^2＋ amended, was found to be rapid and dominated by passive adsorption, and was greatest when low molecular weight compounds with protein-like or small phenolic signatures prevailed in the DOM. Conversely, high molecular weight compounds with a humic or fulvic signature kept Hg^2＋ in the dissolved phase, resulting in the lowest Hg^2＋ accumulation in this algae. In Brachionus and Boeckella the direct incorporation of Hg from the aqueous phase was up to 3% of the Hg^2＋ amended. The dietary incorporation of Hg^2＋ by Boeckella exceeded the direct absorption of this metal in natural water, and was remarkably similar to the Hg^2＋ adsorbed in their prey. Overall, DOM concentration and character affected the adsorption of Hg^2＋ by algae through competitive binding, while the incorporation of Hg^2＋ into the zooplankton was dominated by trophic or dietary transfer.     

Electrochemical and spectroscopic characteristics of dissolved organic matter in a forest soil profile

Dissolved organic matter （DOM） represents one of the most mobile and reactive organic compounds in ecosystem and plays an important role in the fate and transport of soil organic pollutants, nutrient cycling and more importantly global climate change. Electrochemical methods were first employed to evaluate DOM redox properties, and spectroscopic approaches were utilized to obtain information concerning its composition and structure. DOM was extracted from a forest soil profile with five horizons. Differential pulse voltammetry indicated that there were more redox-active moieties in the DOM from upper horizons than in that from lower horizons. Cyclic voltammetry further showed that these moieties were reversible in electron transfer. Chronoamperometry was employed to quantify the electron transfer capacity of DOM, including electron acceptor capacity and electron donor capacity, both of which decreased sharply with increasing depth. FT-IR, UV-Vis and fluorescence spectra results suggested that DOM from the upper horizons was enriched with aromatic and humic structures while that from the lower horizons was rich in aliphatic carbon, which supported the findings obtained by electrochemical approaches. Electrochemical approaches combined with spectroscopic methods were applied to evaluate the characteristics of DOM extracted along a forest soil profile. The electrochemical properties of DOM, which can be rapidly and simply obtained, provide insight into the migration and transformation of DOM along a soil profile and will aid in better understanding of the biogeochemical role of DOM in natural environments.     

封闭式博物馆室内空气颗粒物离子成分特征

采用气体悬浮物粒子监测仪和NanoMoudi-Ⅱ125A型分级采样器对某封闭式博物馆进行颗粒物数浓度监测和颗粒物采样,测定了不同粒径段颗粒物中的主要离子组分。结果表明,监测期间粗颗粒物(粒径≥2.5μm)、细颗粒物(粒径在0.1~2.5μm之间)和超细颗粒物(粒径≤0.1μm)质量浓度分别为20.50~24.38μg/m3、23.39~24.08μg/m3和16.02~17.48μg/m3。颗粒物数浓度集中在粒径≤0.3μm范围,PM1数浓度占PM10数浓度的97%以上,游客扰动和清洁活动使粗颗粒物数浓度增加了8~172倍。SO42-、NO3-、NH4+峰值出现在0.32~0.56μm粒径段,Na+、Cl-分布较平均,K+峰值出现在0.32~0.56μm和3.2~5.6μm粒径段,Mg2+的峰值出现在3.2~5.6μm粒径段,Ca2+峰值出现在1.8~3.2μm粒径段;总有机酸根离子无明显峰值;乙酸根离子浓度为1.238μg/m3,高于甲酸根和乙二酸根。颗粒物的阳/阴离子比均值为2.83,说明阴离子测定可能有缺失,如碳酸盐等。颗粒物中水溶性离子浓度水平和粒径分布受游客影响不明显,受室外空气输送的影响较大。     

城市大气颗粒物背景值涵义及定值方法

城市大气颗粒物背景值的概念对防治城市大气颗粒物污染具有重要意义。城市大气颗粒物背景值不同于颗粒物本底值。本底值是指不受人类活动影响的自然条件下颗粒物的浓度值,而背景值是个相对值,其所在的环境条件有可能已经受到了环境污染。影响城市大气颗粒物背景值的因素主要包括两个方面:一是污染源,主要包括城市本地源排放和外来颗粒物,二是颗粒物扩散的天气和气象因素。将城市大气颗粒物的背景值定义为在一定时期内,由于城市本身的排放,城市大气环境中颗粒物的浓度水平。通过分析总结近年来人们对大气颗粒物垂直分布规律的研究,探讨了采用监测一定高度处大气颗粒物,结合气象因素确定城市环境空气中大气颗粒物背景值的方法。     

可吸入颗粒物污染与气象因子的关系

对闸北区空气自动监测站2009年SO2、NO2、PM10的浓度和气象参数变化特征进行研究,可吸入颗粒物的时间变化特征表明,总体上呈现冬春季高、夏秋季低;PM10与降水量、相对湿度、温度呈现一定的负相关性,但与风速的相关性随季节不同而不同,与气压略呈正相关性。对典型日和灰霾日PM10、SO2、NO2以及相应气象因子的特征进行了分析比较。