水系沉积物重金属分析前处理方法

建立了水系沉积物中6种重金属分析的前处理方法,研究了样品粒径、消解前处理对测定结果的影响,对方法适用性作出评价,并对实际样品进行测定。结果表明:通过Hg元素含量的测定,粒径为0.147 mm的沉积物粒径可满足分析要求;采用微波-硝酸-盐酸-氢氟酸消解、ICP-MS法,对5种不同类型沉积物标准样品的6种重金属的测定结果显示,该方法精密度好、准确度高。利用建立的方法测定广西某河流湖库沉积物样品,6种元素测定结果 RSD为1.57%~11.1%,加标回收率大于74.4%。     

蓝藻越冬期湖湾沉积物磷吸附特征和释放风险

越冬过程是蓝藻暴发的前置阶段,该时期沉积物内源磷是蓝藻水华发生的主要磷源之一.在调查藻型湖湾蓝藻越冬两个时期(休眠期和复苏期)水质和沉积物污染物指标的基础上,进一步分析了水平和垂直方向上沉积物磷吸附特征,阐明沉积物磷释放风险及微生物群落结构变化.结果表明,研究区域两个时期湖湾基本为中度富营养水平,并且水质和沉积物氮磷污...     

易分解碳输入模式对沉积物共代谢效应的影响

通过构建室内微宇宙系统,运用稳定碳同位素示踪法,解析混合处理组中各有机组分代谢释放的CO2含量,探讨相对易分解碳源的输入对湖泊沉积物有机碳矿化过程的影响.结果表明:添加相对易分解碳源的处理组中,CO2排放量明显升高,较对照组分别提高了45.49％(单次添加组)、52.61％(重复添加组)和57.65％(连续添加组),分...     

华东某铀矿区周边河流表层沉积物的天然放射性评价

利用高纯锗γ能谱分析仪测量中国华东某铀矿区附近河流沉积物的放射性核素比活度,计算γ辐射吸收剂量率(D)、有效镭浓度(Ra_(eq))、外照射指数(H_(ex))、内照射指数(H_(in))、年有效剂量当量(AEDE(室内和室外))和年性腺剂量当量(AGDE)等放射性参数,并开展沉积物的放射性危害评估,最后通过Pearson线性系数确定放射性核素比活度之间的相关性。结果表明,河流沉积物中放射性核素~(238)U、~(226)Ra、~(232)Th和40K的平均比活度分别为51.55、37.32、57.63和756.86 Bq·kg~(-1),除~(226)Ra外,其他放射性核素的比活度均高于中国平均值;距离污染区较远或存在河流稀释作用的区域,沉积物的天然放射性核素处于正常水平,作为建筑材料使用时比活度不存在超标;放射性核素~(238)U、~(226)Ra和~(232)Th之间存在显著相关性。     

玉米秸秆生物炭对沉积物中BDE-47生态毒性的影响

生物炭对于污染沉积物的原位修复具有很大的潜力,但关于生物炭对沉积物中有机污染物生态毒性影响的研究则较少报道。为评价生物炭对沉积物中BDE-47生态毒性的影响,以底栖动物铜锈环棱螺为测试生物,采用28 d慢性沉积物生物测试研究了不同添加比例的玉米秸秆生物炭(CSB)与BDE-47联合作用对BDE-47生物积累、肝胰脏细胞DNA损伤以及氧化胁迫生物标志物的影响。结果表明,在慢性暴露情况下,CSB对铜锈环棱螺不具有毒性;CSB通过显著降低沉积物间隙水中BDE-47的浓度而降低其在铜锈环棱螺体内的生物积累。在实验浓度范围内(1%～7%),CSB添加比例越高,降低BDE-47生物积累的效果越显著。不同添加比例的CSB均可以显著降低BDE-47对铜锈环棱螺DNA损伤的毒性,较高比例(4%和7%)CSB的效果更为显著,但BDE-47的氧化胁迫毒性不随CSB添加比例的升高而下降。因此,从降低BDE-47生态毒性的角度考虑,沉积物中CSB的合适添加比例为4%左右。     

Determination activity of radionuclides in marine sediment by gamma spectrometer with anti cosmic shielding

In this work, the activities of radionuclides in a marine sediment sample have been determined. The gamma spectrometer comprises an N type coaxial HPGe detector with active shielding to reduce cosmic background. The mass activities of radionuclides have been derived and found to be around a few Bq kg⁻¹ to several hundreds Bq kg⁻¹ with relative uncertainties in this paper quoted corresponding to the combined standard uncertainties (k = 1).     

三峡工程运用后洞庭湖水沙情势变化及其影响初步分析

采用原型资料分析、长河段一维数学模型计算等手段,分析和预测了三峡工程运用对洞庭湖水沙与冲淤影响,研究了三峡工程运用对洞庭湖出口水位的影响,在此基础上初步分析了三峡工程运用对湖区防洪与生态环境影响。研究成果表明：三峡水库运用后30 a末,荆江三口年均分流量和分沙量比多年平均值分别减少43%和73%,三口分流道的河床相应发生冲淤变化;三峡工程运用后,受荆江三口分流比减少影响,洞庭湖区泥沙淤积显著减少,对增强洞庭湖区调蓄功能、延长洞庭湖寿命有利;受三峡水库调度运用与长江干流河道冲刷影响,洞庭湖出口水位以下降为主,汛期水位的下降将对湖区防洪有利,而枯期水位的下降将对湖区水资源利用及生态环境带来一定不利影响。     

丝状菌对生物淋滤去除底泥中重金属的促进作用

利用氧化亚铁硫杆菌(Acidithiobacillus ferrooxidans,A.f)对采自株洲霞湾港底泥中的Cu、Cd、Pb和Zn 4种重金属进行生物淋滤实验,在实验中加入丝状菌考察其对重金属去除效果的影响。结果表明,丝状菌可以有效抑制低分子量有机酸对A.f的毒害作用,促进各种重金属的去除。当加入10%(体积比)的丝状菌后,生物淋滤过程中系统pH值在5 d内降低到2以下,Fe2+在4 d内完全氧化。经过10 d的处理,Cu、Cd、Pb和Zn 4种重金属的最高去除率分别达到76.3%、92.5%、52.6%和88.5%,与不加入丝状菌的处理相比,达到最大去除率所需的时间缩短1~2 d,4种重金属中,丝状菌的加入对Pb的去除促进作用最为明显,其去除率增加1倍左右。因此,在生物淋滤处理重金属-有机物复合污染底泥工艺中接入丝状菌对处理效果有很好的促进作用。     

Ecosystem Consequences of Contrasting Flow Regimes in an Urban Effects Stream Mesocosm Study1

Abstract: A stream mesocosm experiment was conducted to study the ecosystem‐wide effects of two replicated flow hydrograph treatments programmed in an attempt to compare a simulated predevelopment condition to the theoretical changes that new development brings, while accounting for engineering design criteria for urban stormwater management. Accordingly, the treatments (three replicates each) differed in base flow between events and in the rise to, fall from, and duration of peak flow during simulated storm hydrographs, which were triggered by real rain events occurring outside over a 96‐day period from summer to fall, 2005. Incident irradiance, initial substrate quality, and water quality were similar between treatments. Sampling was designed to study the interactions among the treatment flow dynamics, sediment transport processes, streambed nutrients, and biotic structure and function. What appeared most important to the overall structure and function of the mesocosm ecosystems beyond those changes resulting from natural seasonality were (1) the initial mass of fines that infiltrated into the gravel bed, which had a persistent effect on nitrogen biogeochemistry and (2) the subsequent fine sediment accumulation rate, which was unexpectedly similar between treatments, and affected the structure of the macroinvertebrate community equally as the experiment progressed. Invertebrate taxa preferring soft beds dominated when the gravel was comprised of 5‐10% fines. The dominant invertebrate algal grazer had vacated the channels when fines exceeded 15%, but this effect could not be separated from what appeared to be a seasonal decline in insect densities over the course of the study. Neither hydrograph treatment allowed for scour or other potential for flushing of fines. This demonstrated the potential importance of interactions between hydrology and fine sediment loading dynamics on stream ecosystems in the absence of flows that would act to mobilize gravel beds.     

Contribution of In‐Channel Processes to Sediment Yield of an Urbanizing Watershed1

Abstract: A study was conducted between September 2003 and September 2006 to obtain baseline sediment inventories and monitor sediment transport and storage along a 3.7 km length of the channel of Valley Creek within Valley Forge National Historical Park, Pennsylvania. Valley Creek is a tributary of the Schuylkill River and drains an urbanizing 60.6 km² watershed that currently has 18% impervious land cover. Numerous field methods were employed to measure the suspended sediment yield, longitudinal profile, cross‐sections, banklines, and particle size distribution of the streambed. Suspended sediment yield for the watershed was measured at a USGS gage located just upstream of the park boundary between July 2004 and July 2005, the period corresponding to field surveys of bank erosion and channel change. The estimated suspended sediment yield of 95.7 t/km²/year is representative of a year with unusually high discharge, including a storm event that produced a peak of 78 m³/s, the second highest discharge on record for the USGS gage. Based on the median annual streamflow for the 24 years of record at the USGS gage from 1983 to 2006, the median annual sediment yield is estimated to be closer to 34 t/km²/year, considerably lower than median and mean values for other sites within the region. The mass of silt, clay, and fine sand derived from bank erosion along the 3.7 km study reach during the field survey period accounts for an estimated 2,340 t, equivalent to about 43% of the suspended sediment load. The mass of fine sediment stored in the bed along the study reach was estimated at 1,500 t, with about 330 t of net erosion during the study period. Although bank erosion appears to be a potentially dominant source of sediment by comparison with annual suspended sediment load, bed sediment storage and potential for remobilization is of the same order of magnitude as the mass of sediment derived from bank erosion.