土壤原位覆盖对底泥的修复作用研究

在高度厌氧底泥和富营养化水体构成的模拟生态系统中，采用土壤和硅藻土进行原位覆盖，研究了覆盖技术对水．沉积物界面微环境的改善作用和不同覆盖材料对苦草生长的影响。这2种底质覆盖后，表层底泥氧化还原电位（Eh）分别提高了48．37％和46．77％，底层水体的溶解氧消耗降低，水体中的总氮（TN）和总磷（TP）含量降低；与对照箱体的苦草死亡相比，经过土壤和硅藻土覆盖的箱体中苦草正常萌发、定植和生长；硅藻土箱体苦草的生物量、叶绿素和根茎比均高于土壤覆盖箱体。因此，原位覆盖能有效改善底层水体和表层底泥的氧化还原环境，隔绝污染底泥和延缓营养盐释放，为沉水植物种子萌发和幼苗生长提供有利的生境条件。     

Efficiency of active barriers attaching biofilm as sediment capping to eliminate the internal nitrogen in eutrophic lake and canal

Three active barrier materials (zeolite, ceramicite and light porous media) were applied for preventing nitrogen (N) release from eutrophic lake sediments. Long term experiment of two di erent lake sediments were carried out and the e ect of zeolite dose was evaluated. The results indicated that about 90%–100% of total N in overlying water was eliminated by using zeolite. While the N removal e ciency by ceramic was lower than that by zeolite, and light porous media present the lowest e ciency of 59%. Long term sediment incubation experiments indicated that two eutrophic sediments were both e ective in preventing N release in spite of di erent release characteristics. Bio-zeolite capping technology was able to e ectively inhibit the release of N from the sediment, and the zeolite dose was independently from N removal.     

Red soil for sediment capping to control the internal nutrient release under flow conditions

Nitrogen (N) and phosphorus (P) released from the sediment to the surface water is a major source of water quality impairment. Therefore, inhibiting sediment nutrient release seems necessary. In this study, red soil (RS) was employed to control the nutrients released from a black-odorous river sediment under flow conditions. The N and P that were released were effectively controlled by RS capping. Continuous-flow incubations showed that the reduction efficiencies of total N (TN), ammonium (NH ₄ ⁺ -N), total P (TP) and soluble reactive P (SRP) of the overlying water by RS capping were 77%, 63%, 77% and 92%, respectively, and nitrification and denitrification occurred concurrently in the RS system. An increase in the water velocity coincided with a decrease in the nutrient release rate as a result of intensive water aeration.

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原位掩蔽对底泥汞释放的抑制效果及中试评估

为解决贵州省百花湖底泥中的汞污染问题,研究了原位掩蔽对底泥中汞释放的抑制效果. 选择沸石、高岭土和赤铁矿为掩蔽材料,通过模拟试验,确定原位掩蔽的最佳覆盖厚度为2.0 cm,此时沸石、高岭土和赤铁矿对底泥汞释放的控制率分别为47.1%、64.9%和62.3%,说明最佳掩蔽材料为高岭土. 以高岭土为掩蔽材料的情况下,试验实施7 d后,水体扰动对控制率的影响不足6.7%. 中试区位于百花湖重度污染区,面积约为22 000 m2,采用驳船少量多次撒布高岭土原位掩蔽汞污染底泥,控制覆盖厚度为2.0~3.0 cm,按月连续监测6次. 结果显示,高岭土对汞污染底泥的控制率达到47.1%. 模拟试验及中试效果显示,高岭土原位掩蔽可有效抑制底泥中汞的释放,并且较薄的覆盖厚度可降低工程成本和对湖底生态系统的影响.      

覆盖法控制城市河涌底泥磷释放研究

建立了一套包含有城市河涌底泥、覆盖材料及上覆水的小试装置,采用粉煤灰、水泥、沸石、河砂、玻璃珠等不同物质作为覆盖材料,在厌氧条件下,覆盖材料对城市河涌底泥磷释放的控制效果进行了研究.结果表明,在培养温度为25℃,覆盖材料用量为6.0kg·m-2时,玻璃珠、河砂、沸石、粉煤灰、水泥对PO43-释放的抑制率分别为40.0%、46.7%、60.0%、75.6%、88 9%;覆盖材料对PO43-的抑制作用可归结为覆盖材料的覆盖效应、化学效应和吸附效应;覆盖材料对PO43-释放的抑制率均随着温度的升高而降低;覆盖材料用量对PO43-抑制率影响较大,对于水泥、粉煤灰、沸石、河砂,要达到约50%的PO43-释放抑制率,其用量分别为2.0、2.0、6.0、10.0 kg·m-2,选用粉煤灰作为覆盖材料较合适;从重金属毒理学方面讲,覆盖材料不会对底泥及区域土壤造成影响.     

污染水体底泥治理技术研究进展

水体底泥污染,是世界范围内的一个环境问题,污染物通过大气沉降、废水排放、雨水淋溶与冲刷进入水体,最后沉积到底泥中并逐渐富集,底泥中主要的污染物有重金属、营养元素、难降解有机物.目前底泥的治理方法有原位修复和异位处置,原位修复主要有掩蔽技术、淋洗技术;异位处置主要有卫生填埋、堆肥法、干式热处理;生物修复技术是既可用于原位修复又可用于异位处置的一种方法,具有投资少、见效快且没有二次污染的优点,是一种具有广阔应用前景的技术.     

Damos: Twenty Years of Dredged Material Disposal Site Monitoring. Isn'st That Enough?

Since 1977, the US Army Corps of Engineers Disposal Area Monitoring System (DAMOS) has monitored New England's offshore dredged material disposal sites. DAMOS has shown that by using monitoring information to make management decisions, open water disposal of dredged sediments is possible with minimal environmental impact. Over the past two decades, DAMOS has answered many of the key questions about dredged material impacts. Yet the need for such a programme remains strong from both the technical and public interest perspectives. the programme continues to monitor projects that are extending our knowledge in the areas of deeper water capping, geotechnical behaviour of capping and capped materials, and biological response to contaminants. These investigations, along with the need for specific disposal site surveys, will continue to provide valuable technical information needed by the public, policy makers, and regulators to make critical decisions on dredged sediment management.     

底泥煤渣帽封与药剂投加联用原位稳定化技术对上覆水体及底泥pH-Eh-COD的影响

将底泥有机物原地稳定化处理技术中药剂投加法和帽封法结合，研究以煤渣为帽封材料，苏州河底泥中分别投加零价铁（Fe⁰）及硝酸钙的实验里各体系上覆水体及底泥的pH、氧化还原电位（Eh）、有机含量在60 d的变化情况。结果表明，煤渣帽封下，底泥中投加Fe⁰或硝酸钙后上覆水体pH均在8左右，Eh呈下降趋势，投加Fe⁰后对上覆水体COD的影响较硝酸钙小，但均不会对上覆水体水质产生持久、较大的影响。从底泥有机质的去除率上来看，Fe⁰-煤渣帽封体系在反应周期里有机质的去除率约55%，而硝酸钙-煤渣帽封体系底泥有机质的去除率在27%左右。以Fe⁰-煤渣帽封材料复合体系运用在底泥原地稳定化帽封技术中降解有机物更为合适。     

沸石与生物沸石薄层覆盖技术削减富营养化景观水体氮比较研究

以扬州古运河河水和表层沉积物为研究对象，实验室静态模拟实验比较研究了沸石与生物沸石（即附着高效异养硝化菌和好氧反硝化菌的沸石）薄层覆盖削减富营养化景观水体氮效果，考察了生物沸石薄层覆盖削减氮可行性，探讨了生物沸石薄层覆盖削减氮的机理和影响因素。实验结果表明，当实验历时21d时，2kg／m^2（2mm厚）的沸石和生物沸石覆盖对上覆水体TN的削减率分别为36．92％和60．41％，生物沸石比沸石对TN削减率提高了23．48％，高效菌的生物脱氮作用明显；21d后生物沸石覆盖对TN的削减率维持在60％～75％，但生物沸石相对于沸石削减氮的效果有降低趋势。实验后期碳源不足是影响高效菌生物脱氮的主要影响因素。可见，生物沸石薄层覆盖削减富营养化景观水体氮是可行的，但需要进一步研究强化高效反硝化细菌适应能力方法。     

灼烧净水污泥投加方式对磷吸附和磷形态的影响

以灼烧净水污泥为研究对象,探讨在其不同投加方式(混匀和覆盖)下,各底泥对外源磷的吸附效果以及间隙水和底泥中各形态磷的数量分布.结果表明,相比未灼烧净水污泥,灼烧净水污泥对磷的吸附能力显著改善,磷最大吸附量(Smax)提高了43.7%、底泥磷平衡浓度(EPC0)降低69.1%、磷饱和度(DPS)降低54.4%.混匀和覆盖对上覆水中磷消失的贡献率几乎一致,但明显高于对照实验.但如果考虑灼烧净水污泥与上覆水的接触几率,则混匀条件下,单位净水污泥对磷的吸附量为覆盖条件下的2.3倍.覆盖条件下,间隙水(1~2 cm)中溶解性磷酸盐浓度是混匀条件的33.17倍(平均值),这主要源于覆盖导致溶解氧渗透深度明显降低.混匀条件下,外源磷更易形成Ca-P,而覆盖条件下,易释放的NH_4Cl-P和Fe/Al-P占比更多,这暗示了混匀对底泥微环境的改造更有利于外源磷的吸附和内源磷的持留.