Chlorination Byproducts in Drinking Water Produced from Thermal Desalination in United Arab Emirates

Oil activities in the Arabian Gulf can potentially affect the quality of the intake water available for coastal desalination plants. This paper addresses such situation by investigating the quality of intake water and desalinated water produced by a desalination plant located near a coastal industrial complex in United Arab Emirates (UAE). Analyses of the organic compounds on the intake seawater reported non-detected levels in most samples for the three tested organic groups; namely Polyaromatic Hydrocarbons (PAHs), Phenols, and Polychlorinated Biphenyls (PCBs). Trihalomethanes (THMs) and Haloacetic Acids (HAAs) were also tracked in the intake sea water, throughout the desalination processes, and in the final produced drinking water, to evaluate the undertaken pre- and post chlorination practices. The levels of considered Chlorination Byproducts (CBPs) were mostly found below the permissible international limits with few exceptions showing tangible levels of bromoform in the intake seawater and in the final produced drinking water as well. Lab-controlled experiments on the final produced distillate showed little contribution of its blending with small percentage of seawater upon the formation of trihalomethane and in particular, bromoform. Such results indicate that the organic precursors originated in the seawater are responsible for bromoform formation in the final distillate.     

Analysis,accumulation and central effects of trihalomethanes. I. bromoform†

The paper presents the results obtained in a study on the effects of organic micropollutants on the central nervous system of the rat, used herein as a suitable model for neurotoxicologic work. Bromoform, a member of the trihalomethane (THM) family, was the pollutant selected since it becomes a characteristic marker in the Barcelona potable water supply.

Analytical data on the GC‐ECD separation of THMs from other volatile halocarbons is presented. A mixed packed column 10% SE‐30/PEG 20M (94:6) at 70°C provides an adequate separation. The distribution of bromoform in rat plasma and tissues showed an accumulation in brain, kidney and fat, increasing in this order and a rapid elimination after 30 min. The effect on the central aminergic metabolism is studied by HPLC. The increased metabolic activity detected could be attributed either to an increased nervous activity, stimulating the metabolism of serotonin, or to its greater degradation.     

四种金属离子对CHBr_3和小牛胸腺DNA间结合作用的影响

采用紫外光谱和荧光光谱法研究了CHBr3与离体小牛胸腺DNA(ctDNA)间的相互作用,以及Cu2+、Co2+、Cd2+、Mg2+4种金属离子单独或共存时对CHBr3与ctDNA结合的影响.结果表明:4种金属离子与CHBr3、ctDNA均能发生基态络合反应,络合物的生成导致体系的紫外吸收峰强度和形状改变,使ctDNA-溴化乙锭体系的荧光发生了不同程度的猝灭;向CHBr3-ctDNA-溴化乙锭体系中分别或同时加入4种金属离子后,Cu2+、Co2+、Cd2+可减弱两者之间的结合,减弱顺序为Cu2+Co2+Cd2+,Mg2+可加强两者之间的结合,4种金属离子同时加入后出现不同于4种金属离子单独加入时的中间类型.据此推断,CHBr3可能主要是通过嵌插作用与ctDNA碱基结合,金属离子对CHBr3与ctDNA结合的影响主要取决于金属离子与DNA的碱基和磷酸基团间结合的相对亲和比.     

Marine macroalgae in polar regions as natural sources for volatile organohalogens

Marine macroalgae species from the polar regions were investigated for their importance as natural sources of volatile halogenated compounds released into the biosphere. Several different halogenated C1 to C4 hydrocarbons were identified and their release rates determined. The compounds contained mainly bromine and iodine, and form was the dominant compound released. Although an annual atmospheric input of approximately 10(8)-10(10) g bromine and 10(7)-10(8) g iodine was calculated from the release rates, marine macroalgae are apparently not the major source on a global scale, as the release is up to four orders of magnitude lower than a presumed annual flow from the oceans. Despite this, macroalgae may be more important on a local scale due to their occurrence at a high biomass in the coastal regions. The present paper gives an overview about studies done on the release of volatile halocarbons by macroalgae from polar regions. Furthermore, the function of these compounds in the macroalgal metabolism is discussed.     

The natural production of organobromine compounds

Organobromine chemicals are produced naturally by an array of biological and other chemical processes in our environment. Some of these compounds are identical to man-made organobromine compounds, such as methyl bromide, bromoform, and bromophenols, but many others are entirely new moleclar entities, often possessing extraordinary and important biological properties. Although only a few natural organobromine compounds had been discovered up to 1968, this number as of early 1999 is more than 1,600, and new examples are being discovered continually. Organobromine compounds are produced naturally by marine creatures (sponges, corals, sea slugs, tunicates, sea fans) and seaweed, plants, fungi, lichen, algae, bacteria, microbes, and some mammals. Many of these organobromine compounds are used in chemical defense, to facilitate food gathering, or as hormones.