• 대한약리학회지
• /
• 제17권1호
• /
• pp.17-25
• /
• 1981

No evidence has accumulated that lead compound is an essential component for biological function in animals. Lead is absorbed primarily through the epithelial mucosal cells in duodenum and the absorption can be enhanced by the substances which bind lead and increase its solubility. Iron, zinc and calcium ions, however, decrease the absorption of lead without affecting its solubility, probably by competing for shared absorptive receptors in the intestinal mucosa. Therefore, the absorption of lead is increased in iron deficient animals. Lead shows a strong affinity for ligands such as phosphate, cysteinyl and histidyl side chains of proteins, pterins and porphyrins. Hence lead can act on various active sites of enzymes, inhibiting the enzymes which has functional sulfhydryl groups. lead inhibits the activity of ${\delta}$-aminolevulinic acid dehydratase for the biosynthesis of hemoproteins and cytochrome, which catalyzed the synthesis of monopyrrole prophobilinogen from ${\delta}$-aminolevulinic acid. Accordingly lead decrease hepatic cytochrome p-450 content, resulting an inhibition of the activity of demethylase and hydroxylase in liver. Little informations are available on the effect of lead on digestive system although the catastrophic effects of lead intoxication are well documented. The present study was, therefore, attempted to investigate the effect of lead on pancreaticobiliary secretion in rats. Albino rats of both sexes weighing $170{\sim}230g$ were used for this study. The animals were divided into one control and three treated groups, i.e., control (physiologic saline 1.5ml/kg i.p.), lead acetate $(l0{\mu}mole/kg/day\;i.p.)$, $Pb(Ac)_2$ and EDTA$(each\;10{\mu}mole/kg/day\;i.p.)$, $Pb(Ac)_2$ and $FeSO_4(each\;l0{\mu}mole/kg/day\;hp)$. The pancreatico-biliary juice was collected under urethane anesthesia, and activities of amylase and lipase were determined by employing Sumner's and Cherry and Crandall's methods. The summarized results are follows. 1) In the experiment for acute toxicity of lead acetate, 20% of mortality was observed in rat treated with lead acetate as well as inhibition of the activity of amylase in the juice at the 3 rd day of the treatment. 2) No increases in body weight were observed in rats treated with lead acetate, while in control group the significant increases were observed. However, the body weights of animals were increased in the group lead acetate plus EDTA or $FeSO_4$. 3) Lead acetate decreased significantly the volume of pancreatico-biliary juice whereas additional treatment of EDTA and $FeSO_4$ prevented it. 4) Total activity of amylase was markedly reduced due to lead acetate treatment, but no change was showed following additional treatment with EDTA and $FeSO_4$. 5) No changes in the cholate and lipase output were observed in rats treated with lead acetate as compared with that of control rats. 6) Increase in bilirubin output in rats treated with lead acetate was shown on the 2nd and 3rd weeks treatment. 7) In the case of in vitro experiment, lead acetate also markedly inhibited release of amylase from pancreatic fragment. 8) Histologic finding indicated that acini vacuolation was induced in the pancreatic tissue of rat treated with lead acete. From the above results, it might be concluded that lead acetate decreases the volume of pancreatico-biliary secretion and inhibits the amylase activity, by acting directly on pancreatic cells.

• Applied Microscopy
• /
• 제30권4호
• /
• pp.357-365
• /
• 2000

포유류 장생 상피세포의 하나인 파네스세포(Paneth cell)는 여러 가지 금속류를 함유하고 있으며, 생체가 과잉의 이들 금속류에 노출되거나 부족할 때에 장 내강을 통해 제거하거나 흡수함으로써 금속류의 항상성에 기여한다고 알려져 있다. 이번 연구는 이러한 연구보고에 근거하여 금속류중에서 zinc를 실험적으로 과량투여한 후 파네스세포내 zinc의 분포에 어떤 변화가 초래되는 지를 광학 및 전자현미경적 autometallography(AMG)로 관찰함으로써 파네스세포의 zinc와 관련된 세포생물학적 기능을 규명하고자 하였다. Wistar 랫드에 체중 당 20mg의 zinc chloride를 생리식염수 5ml에 녹여 복강주사한 후 2시간에 이르러 0.1 M phosphate buffer(PB)에 녹인 0.5% sodium sulphide-3% glutaraldehyde 흔합액으로 관류고정하였다. 회장(ileum)의 일부를 Dry Ice나 $CO_2$ gas로 얼린 후 cryostat을 이용하여 $20{\mu}m$ 두께의 조직절편을 만들어 및 단계의 AMG법을 시행하였다. 이와는 별도로 EM용으로 선택된 회장절편은 일련의 전자현미경 표본제작과정을 거쳐, 100nm두께의 thin section을 만들어 uranyl-lead 이중염 색 추 전자현미경으로 관찰하였다. Zinc를 투여한 동물에서 관찰된 소견은 생리식염수만을 투여한 대조군의 것과 비교할 때 큰 차이를 보였다. 우선 대조군에서는 파네스세포의 꼭대기(apex)부위에서 낱알모양을 띤 AMG양성반응 구조물(AMG grain)들이 분비과립과 사이토졸(cytosol)에서 관찰되었고, 세포사이공간에서도 적은 양의 grain이 분포하고 있었다. 반면 zinc를 투여한 랫드의 파네스세포에서는 AMG 입자가 이상의 부위에서 훨씬 많은 양의 grain이 분포해 있었으며, 특히 분비과립에서는 가장 높은 농도로 관찰되었다. 더욱이 대조군에서 관찰되지 많았던 장샘의 분비관(Lieberkuhn crypt)및 고유판 혈관의 내에서도 많은 grain이 관찰되었다. 이상의 결과를 요약하면 과량의 zinc에 노출된 생체는 혈관을 경유하여, 파네스세포의 분비과립을 매개로 하여, 장관의 내강쪽으로 과잉의 zinc 를 피내고 있는 모습을 보인다. 따라서 연구자는 파네스세포가 생체내 zinc의 양을 조절하는데 중요한 역할이 있을 것으로 본다.

• 한국결정성장학회지
• /
• 제16권2호
• /
• pp.88-93
• /
• 2006

유해한 중금속을 다량 함유하는 EAF(electric arc furnace) 더스트를 세라믹 원료로 재활용하기 위해서 EAF 더스트, EAF 더스트-점토에 대해서 pH와 혼합비에 따른 중금속 용출농도의 변화를 분석하였다. 소성과정 중에서 발생하는 중금속의 휘발량을 소지 내의 중금속 이온의 총량을 측정하여 평가하였으며 TCLP(toxicity characteristic leaching procedure)분석을 통해 중금속 이온의 안정화 정도를 평가하였다. EAF 더스트-점토 슬러리의 pH를 10으로 조절하였을 경우에 습식혼합 여액중의 중금속 이온의 농도가 가장 낮은 값을 가졌다. pH 10의 슬러리에 대해서 혼합비와 소성온도에 따른 소지내 중금속 이온의 총량을 측정한 결과 소성온도와 EAF 더스트의 함량이 증가할수록 중금속의 휘발이 증가하였으며, 점토의 혼합비가 증가할수록 중금속 이온의 휘발이 억제되었다. TCLP 분석결과 점토의 혼합비와 소성온도가 증가할수록 중금속의 용출은 감소하였으며 중금속의 용출농도는 기준치 이하로 안정화되었음을 확인할 수 있었다.

• 한국지하수토양환경학회:학술대회논문집
• /
• 한국지하수토양환경학회 2004년도 총회 및 춘계학술발표회
• /
• pp.472-472
• /
• 2004

Numerous studies on urban groundwater have been carried out in many other countries. Urban groundwater shows a unique hydrologic system because of complex urban characteristics such as road pavement, sewers and public water supply systems. These urban facilities may change the characteristics of groundwater recharge but contaminate its quality as well. There have been several researches on urban groundwater in Seoul. Seoul has been industrialized very rapidly so that the city has large population. The recent population in Seoul amounts to more than ten millions, corresponding to a very high density of about 17, 000 people/km$^2$. Therefore, many factors affect the groundwater quality and quantity in Seoul. Nowadays, groundwater in Seoul is being extracted for construction, industrial use, and drinking and so on. There are 15, 714 wells in Seoul and its annual usage is 41, 425, 977m$^3$(in 2001). Therefore, systematic studies are needed to properly manage and use the groundwater in Seoul. The purposes of this study in progress are to identify geochemical characteristics of groundwater in Seoul and to determine the extent of groundwater contamination and its relationship with urban characteristics. For this study, groundwater was sampled from more than 400 preexisting wells that were randomly selected throughout the Seoul area. For all samples, major cations together with Si, Al, Fe, Pb, Hg For 200 samples among them, TCE, PCE, BTEX were also analyzed by GC. Our study shows that groundwater types of Seoul are distributed broadly from Ca-HCO$_3$ type to Ca-Cl＋NO$_3$ type. The latter type indicates anthropogenic contamination. Among cations, Ca is generally high in most samples. In some samples, Na and K are dominant. The dominant anions change widely from HCO$_3$ to Cl＋NO$_3$. The anion composition is considered to effectively indicate the contribution of distinct anthropogenic sources. In addition, major ions are positively proportional to total dissolved solid (TDS) except K and NO$_3$. Thus, we consider that TDS may be used as an effective indicator of the extent of pollution. However, the increase of TDS may result from increased water-rock interaction. To determine the extent of groundwater contamination, it is needed to figure out the baseline water quality in Seoul. Furthermore, detailed geochemical studies are required to find out pollution sources and their corresponding hydrochemical parameters.

• 한국지하수토양환경학회:학술대회논문집
• /
• 한국지하수토양환경학회 2004년도 임시총회 및 추계학술발표회
• /
• pp.119-120
• /
• 2004

Urban groundwater has a unique hydrologic system because of the complex surface and subsurface infrastructures such as deep foundation of many high buildings, subway systems, and sewers and public water supply systems. It generally has been considered that increased surface impermeability reduces the amount of groundwater recharge. On the other hand, leaks from sewers and public water supply systems may generate the large amounts of recharges. All of these urban facilities also may change the groundwater quality by the recharge of a myriad of contaminants. This study was performed to determine the factors controlling the recharge of deep groundwater in an urban area, based on the hydrogeochemical characteristics. The term ‘contamination’ in this study means any kind of inflow of shallow groundwater regardless of clean or contaminated. For this study, urban groundwater samples were collected from a total of 310 preexisting wells with the depth over 100 m. Random sampling method was used to select the wells for this study. Major cations together with Si, Al, Fe, Pb, Hg and Mn were analyzed by ICP-AES, and Cl, N $O_3$, N $H_4$, F, Br, S $O_4$and P $O_4$ were analyzed by IC. There are two groups of groundwater, based on hydrochemical characteristics. The first group is distributed broadly from Ca-HC $O_3$ type to Ca-C1+N $O_3$ type; the other group is the Na+K-HC $O_3$ type. The latter group is considered to represent the baseline quality of deep groundwater in the study area. Using the major ions data for the Na+K-HC $O_3$ type water, we evaluated the extent of groundwater contamination, assuming that if subtract the baseline composition from acquired data for a specific water, the remaining concentrations may indicate the degree of contamination. The remainder of each solute for each sample was simply averaged. The results showed that both Ca and HC $O_3$ represent the typical solutes which are quite enriched in urban groundwater. In particular, the P$CO_2$ values calculated using PHREEQC (version 2.8) showed a correlation with the concentrations of maior inorganic components (Na, Mg, Ca, N $O_3$, S $O_4$, etc.). The p$CO_2$ values for the first group waters widely ranged between about 10$^{-3.0}$ atm to 10$^{-1.0}$ atm and differed from those of the background water samples belonging to the Na+K-HC $O_3$ type (<10$^{-3.5}$ atm). Considering that the p$CO_2$ of soil water (near 10$^{-1.5}$ atm), this indicates that inflow of shallow water is very significant in deep groundwaters in the study area. Furthermore, the P$CO_2$ values can be used as an effective parameter to estimate the relative recharge of shallow water and thus the contamination susceptibility. The results of our present study suggest that down to considerable depth, urban groundwater in crystalline aquifer may be considerably affected by the recharge of shallow water (and pollutants) from an adjacent area. We also suggest that for such evaluation, careful examination of systematically collected hydrochemical data is requisite as an effective tool, in addition to hydrologic and hydrogeologic interpretation.ion.ion.