• 환경생물
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• 제22권2호
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• pp.247-258
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• 2004

Climatological, hydrological and planktonical research studies, measurements of primary production and photosynthetic efficiency from December 1976 to December 1978 have been carried out in two brackish lakes: Lake Etang de Berre and Lake Etang de Vaine located in the French Mediterranean coast, in the region of Carry-le-Rouet located on the north-west Mediterranean near Marseilles, and in fresh water inflows from 4 Rivers (Touloubre, Durance, Arc, Durancole) to Lake Etang de Berre. Physico-chemical parameters were measured for this study: water temperature, salinity, density, pH, alcalinity, dissolved oxygen (% saturation), phosphate, nitrate, nitrite, silicate etc. Diverse biological parameters were also studied: photosynthetic pigments, phaeopigments, specific composition and biomass of phytoplankton, primary pelagic production etc. Climatical factors were studied: air-temperature, solar-radiation, evaporation, direction (including strength) of winds, precipitation and freshwater volume of the four rivers. The changes in Lake ‘Etang de Berre’ ecosystem depend on the quality of the water in the Durance River, and on the effects of seawater near the entrance of the Caronte Canal. The water quality of the lake varies horizontally and vertically as a result of atmospheric phenomena, maritime currents and tides. The distribution of water temperatures is generally heterogeneous. Southeasterly winds and the Northeasterly Mistral wind are important in the origins of circulated and mixed water masses. These winds are both frequent and strong. They have, as a result, a great effect on the water environment of Lake Etang de Berre. In theory, the annual precipitation in this region is well over eight times the water mass of the lake. The water of the Durance River flows into Lake Etang de Berre through the EDF Canal, amounting to 90% of the precipitation. However, reduction of rainfall in dry seasons has a serious effect on the hydrological characteristics of the lake. The temperature in the winter is partially caused by the low temperature of fresh water, particularly that of the Durance River. The hydrological season of fresh and brackish water is about one month ahead of the hydrological season of sea water in its vicinity. The salinity of Lake Etang de Berre runs approximately 3$\textperthousand$, except at lower levels and near the entrance to the Caronte Canal. However, when the volume of the Durance River water is reduced in the summer and fall, the salinity rises to 15$\textperthousand$. In the lake, the ratio of fresh water to sea water is six to one (6:1). The large quantities of seston conveyed by rivers, particularly the Durance diversion, strongly reduce the transparency in the brackish waters. Although the amount of sunshine is also notable, transparency is slight because of the large amount of seston, carried chiefly by Tripton in the fresh water of the Durance River. Therefore, photosynthesis generally occurs only in the surface layer. The transparency progressively increases from freshwater to open seawater, as mineral particles sink to the bottom (about 1.7kg $m^{-2}a^{-1}$ on the average in brackish lakes). The concentration of dissolved oxygen and the rate of oxygen saturation in seawater (Carry-le-Rouet) ranged from 5.0 to 6.0 $m\ell$ㆍ.$1^{-1}$, and from 95 to 105%, respectively. The amount of dissolved oxygen in Etang de Berre oscillated between 2.9 and 268.3%. The monographs of phosphate, nitrate, nitrite and silicate were published as a part of a study on the ecology of phytoplankton in these environments. Horizontal and vertical distributions of these nutriments were studied in detail. The recent diversion of the Durance River into Lake Etang de Berre has effected a fundamental change in this formerly marine environment, which has had a great impact in its plankton populations. A total of 182 taxa were identified, including 111 Bacillariophyceae, 44 Chlorophyceae, and 15 Cyanophyceae. The most abundant species are small freshwater algae, mainly Chlorophyceae. The average density is about $10^{8}$ cells $1^{-1}$ in Lake Etang de Berre, and about double that amount in Lake Etang de Vaine. Differences in phytoplankton abundance and composition at the various stations or at various depths are slight. Cell biovolume V (equivalent to true biomass), plasma volume VP (‘useful’ biomass) and, simultaneously. the cell surface area S and S/V ratio through the measurement of cell dimensions were computed as the parameters of phytoplankton productivity and metabolism. Pigment concentrations are generally very high on account of phytoplankton blooms by Cyanophyceae, Chlorophyceae and Cryptophyceae. On the other hand, in freshwaters and marine waters, pigment concentrations are comparatively low and stable, showing slight annual variation. The variations of ATP concentration were closely related to those of chlorophyll a and phytoplankton blooms only in marine waters. The carbon uptake rates ranged between 38 and 1091 mg$Cm^{-2}d^{-1}$, with an average surface value of 256 mg; water-column carbon-uptake rates ranged between 240 and 2310 mg$Cm^{-2}d^{-1}$, with an average of 810, representing 290 mg$Cm^{-2}$, per year 45 000 tons per year of photosynthetized carbon for the whole lake. Gross photosynthetic production measured by the method of Ryther was studied over a 2-year period. The values obtained from marine water(Carry-le-Rouet) ranged from 23 to 2 337 mg$Cm^{-2}d^{-1}$, with a weighted average of 319, representing about 110 gCm$^{-2}$ per year. The values in brakish water (Etang de Berre) ranged from 14 to 1778 mg$Cm^{-2}d^{-1}$, with a weighted average of 682, representing 250 mg$Cm^{-2}$ per year and 38 400 tons per year of photosynthesized carbon for the whole lake.

• Tuberculosis and Respiratory Diseases
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• 제55권1호
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• pp.69-87
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• 2003

배 경 : Gemifloxacin은 그람음성 및 그람양성 균주에 대해서 모두 좋은 활성을 가지고 있는 fluoroquinolone 항균제로서, 임상균주를 이용한 in vitro 시험에서 다른 대조 quinolone에 비하여 S. pneumnoniae의 penicillin 내성 균주에 대해서 활성이 높을 뿐만 아니라, 다른 quinolone 항균제에 내성을 나타내는 S. pneumoniae 임상 균주에 대해서도 좋은 활성을 유지하는 것으로 밝혀져 만성기관지염의 급성악화(AECB)시 사용하기 적절한 치료제로 여겨진다. 목 적 : 한국인에서 AECB를 치료하기 위한 LB20304(gemifloxacin) 160mg 또는 320rng 1일 1회 7일간 투여의 유효성과 안전성을 평가하고자 하였다. 방 법 : Gemifloxacin 100mg과 위약을 1일 1회 7일간 경구 투여한 환자 67명, gemifloxacin 320mg을 1일 1회 7일간 경구 투여한 환자 70명의 환자를 대상으로 무작위 배정, 이중맹검, 병행 치료군, 다기관, 2상 임상시험으로 실시하였다. 결 과 : 두 치료군의 인구통계학적 특징과 임상적 및 흡연 기왕력 등 기저 상태는 대등하였다. Per-protocol(PP) 환자군에서, 추적관찰 시점(days 14-21) 및 치료종료 시점(days 7-10)에서의 임상적 반응은 gemifloxacin 100mg군이 각각 84.2%, 96.5%, 320mg군이 각각88.7%, 96.4%로 두 군간에 유의한 사이가 없었고(각각 p=0.49, p=0.99), 추적관찰 시점 및 치료종료 시점의 미생물학적 반응도 gemifloxacin 160mg군이 각각 78.9%, 81.8%, 320mg군이 각각 84.2%, 86.4%로 두 군간에 유의한 차이가 없었다(각각 p=0.68, p=0.68) 본 임상시험에서 치료 전에 많이 배양된 병원균으로는 S. pneumoniae(12/52), H. influenzae(10/52), K. pneumoniae(6/52), M. catarrhalis(3/52) 로 K. pneumoniae가 비교적 많이 배양된 점을 제외하고는 기존에 알려진 AECB 시 배양되는 병원균의 분포와 큰 차이가 없었다. S. pneumoniae, H. influenzae, K. pneumoniae, M. catarrhalis 등 주요 병원 균에 대한 MIC는 전반적으로 다른 quinolone 항균제보다 gemifloxacin이 더 낮았고, 특히 S. pneumoniae(3 PRSP, 7 ERSP 포함)에 대한 gemifloxacin의 MIC(${\leq}0.03ug/ml$)는 다른 quinolone, beta-lactam, macrolide 항균제보다 월등히 낮아 gemifloxacin 이 AECB의 치료에 매우 유용한 항균제임을 보여주었다. 안전성 결과에서는 gemifloxacin 160mg 및 320mg 투여군 모두 시험약과의 관련성을 배제할 수 없거나 관련이 의심되는 중대한 이상반용은 관찰되지 않았고, 치료 중 및 치료 후 30일 기간동안, 이상반응을 최소한 하나 이상 보고한 환자가 gemifloxacin 160mg군은 26.9%, 320mg군은 31.4%이었다. 가장 흔히 보고된 이상반응은 간효소 수치의 증가로서, 발생 빈도는 160mg군에서 1/67명(1.5%), 320mg군에서 5/70명(7.1%) 이었다. 간효소 수치의 증가로 인해 탈락한 환자는 없었고, 중증도(severity)는 모두 경도(mild)였으며, 별다른 처치 없이 정상으로 회복되었다. 전반적인 이상반응의 profile에서 치료군간 주요한 차이는 없었다. 결 론 : 본 임상시험의 결과, 한국인에서 AECB를 치료하기 위한 gemifloxacin 160mg 또는 320mg 1일 1회 7일간의 투여는 임상적 및 미생물학적으로 매우 유효하고 안전하였다.

• 한국토양비료학회지
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• 제40권5호
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• pp.418-428
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• 2007

본 연구는 골재 부산물의 용토재로서 활용을 위한 기초 특성 분석으로서 전국 21개소의 골재 업체를 대상으로 골재 생산시 생하는 슬러지나 석분 등 골재 부산물의 화학성과 물리성 및 광물 조성을 알아 보는데 있다. 그 결과를 요약하면 다음과 같다. 1. 골재 부산물의 pH는 전라도 지역의 JH, DA 업체를 제외하고 모두 8.41~10.97 정도로 높았으며, EC는 평균 $167.9{\mu}S\;cm^{-1}$ 이고 전라도 지역은 대부분 $33.0{\sim}122.4{\mu}S\;cm^{-1}$ 정도로 상대적으로 낮은 수치를 보였으나, 경상도 지역은 $169.5{\sim}639.0{\mu}S\;cm^{-1}$ 정도로 상대적으로 높은 수치를 나타냈다. 2. 유기물 함량은 대부분 $2.9{\sim}5.0g\;kg^{-1}$ 이며, 강원도 지역의 GG 업체의 경우 $11.27g\;kg^{-1}$ 로 상대적으로 높았다. T-N의 경우, 0.01~0.11 % 정도이고 $NH_4{^+}-N$의 경우, 대부분 지역은 $14.0{\sim}67.2mg\;kg^{-1}$ 수준이었으나 전라도 지역은 $1.03{\sim}3.00mg\;kg^{-1}$ 수준을 보였다. $NO_3{^-}-N$의 경우, 대부분 지역은 $14.0{\sim}67.2mg\;kg^{-1}$ 수준이었으나 전라도 지역은 $1.0{\sim}3.2mg\;kg^{-1}$ 수준을 보였다. $P_2O_5$ 의 경우, 강원도의 $10.2mg\;kg^{-1}$ 에서 전라도 $24.8mg\;kg^{-1}$ 까지 비슷한 수준을 나타냈다. $Ca^{2+}$, $Mg^{2+}$, $K^+$ 및 $Na^+$ 의 각 평균은 $2.299cmol_c\;kg^{-1}$, $0.472cmol_c\;kg^{-1}$, $0.021cmol_c\;kg^{-1}$, $0.055cmol_c\;kg^{-1}$ 이며 $Ca^{2+}$의 경우, 최고값인 경상도 DE 업체의 $6.385cmol_c\;kg^{-1}$ 부터 최저값인 전라도 JH 업체의 $0.742cmol_c\;kg^{-1}$ 사이의 범위를 보였다. $Mg^{2+}$의 경우 최고값인 전라도 YS 업체의 $1.850cmol_c\;kg^{-1}$ 부터 최저값인 충청도 JK 업체의 $0.006cmol_c\;kg^{-1}$ 사이의 범위를 보였다. 양이온교환용량은 평균 $7.6cmol_c\;kg^{-1}$으로 경상도에서 $17.3cmol_c\;kg^{-1}$으로 가장 높았으며, 전라도에서 $2.2cmol_c\;kg^{-1}$ 으로 가장 낮았다. 3. 중금속 함량은 모든 항목에서 환경부에서 고시한 농경지 오염 우려 기준을 초과하지 않았다. Cd의 경우, 평균 $0.011mg\;kg^{-1}$ 이며 최저 값인 강원도 DM 업체의 $0.003mg\;kg^{-1}$ 에서부터 최고 값인 경상도 DH 업체의 $0.062mg\;kg^{-1}$ 사이의 값을 보였다. $Cr^{6+}$의 경우, 평균 $0.068mg\;kg^{-1}$ 이며 최저 값인 강원도 DM 업체와 SS 업체의 $0.037mg\;kg^{-1}$ 에서부터 최고 값인 경기도 KG 업체의 $0.169mg\;kg^{-1}$ 사이의 값을 보였다. Cu의 경우, 평균 $0.419mg\;kg^{-1}$ 이며 최저 값인 강원도 DM 업체와 SS 업체의 $0.000mg\;kg^{-1}$ 에서부터 최고 값인 충청도 SB 업체의 $1.072mg\;kg^{-1}$ 사이의 값을 보였다. Ni의 경우, 평균 $3.513mg\;kg^{-1}$ 이며 최저 값인 전라도 DA 업체의 $0.045mg\;kg^{-1}$ 에서부터 최고 값인 강원도 GG 업체의 $11.980mg\;kg^{-1}$ 사이의 값을 보였다. Zn의 경우, 평균 $0.588mg\;kg^{-1}$이며 최저 값인 경상도 SU 업체의 $0.014mg\;kg^{-1}$ 에서부터 최고 값인 충청도 SB 업체의 $1.086mg\;kg^{-1}$ 사이의 값을 보였다. Pb의 경우, 평균 $0.467mg\;kg^{-1}$이며 최저 값인 강원도 DM 업체의 $0.008mg\;kg^{-1}$ 에서부터 최고 값인 충청도 SB 업체의 $1.261mg\;kg^{-1}$ 사이의 값을 보였다. Fe의 경우, 평균 $33.815mg\;kg^{-1}$이며 최저 값인 경상도 SU 업체의 $0.805mg\;kg^{-1}$ 에서부터 최고 값인 경기도 KG 업체의 $106.400mg\;kg^{-1}$ 사이의 값을 보였다. Mn의 경우, 평균 $18.427mg\;kg^{-1}$이며 최저 값인 강원도 SS 업체의 $0.703mg\;kg^{-1}$ 에서부터 최고 값인 충청도 SB 업체의 $49.140mg\;kg^{-1}$ 사이의 값을 보였다. 4. 골재 부산물의 토성은 평균적으로 대부분 모래가 50 % 이하이며 미사가 50 % 이상인 미사질양토(SiL)인데 비해 전라도의 경우, 양토(L)였다. 유효수분은 평균 2.58 % 로 매우 낮은 수준이며, 액성한계의 경우, 최저 값인 전라도 JS 업체의 5.9 % 에서 최고 값인 경상도의 DH 업체의 39.1 % 사이의 값을 보이며 평균 24.4 %로 일반 밭 토양의 액성한계와 유사한 수치를 보였다. 대부분 시료에서 점착성 및 가소성 모두 그 성질이 약하거나 없는 C나 D 등급이었다. 5. 골재 부산물의 투수성은 경기도 KG 업체의 경우, $2.8{\times}10^{-6}m\;sec^{-1}$, 강원도 CC 업체의 경우, $0.4{\times}10^{-6}m\;sec^{-1}$, 그리고 전라도 KS 업체의 경우, $1.4{\times}10^{-6}m\;sec^{-1}$ 로 상당히 느린 투수성을 보여준다. 6. 골재 부산물의 X선 회절분석 결과, 석영(Quartz)과 단사녹니석(Clinochlore)이나 금운모(Phlogopite)가 주요 피크로 대부분 시료에서 화강암 또는 화강 편마암 지역의 광물 조성을 보였으며, 강원도 지역의 DM 업체에서 석회암을 모암으로 하는 방해석(Calcite)과 백운석(Dolomite)이 주요 피크였다. 7. 골재 부산물의 화학 조성 분석 결과(X선 형광분석), 대부분 시료는 원암을 화강암이나 화강편마암으로 하고 있기에 대표적인 원소는 $SiO_2$이며 그 다음으로 $Al_2O_3$가 대부분을 차지한다. 강원도의 SS, DM 업체의 $SiO_2$의 함량은 30 %이하로 낮은 반면에 CaO의 함량은 45 % 이상으로 높은 수치를 보여준다. 골재 부산물의 규반비는 1.70~3.42 이며, 이는 골재 부산물이 화학적 풍화 보다는 원암에서 기계적인 파쇄에 의한 단순 입자 크기의 축소로 보이며, 원암 가루, 즉 1차 광물로서 2차 광물이 거의 없기 때문이라 판단된다. 8. 골재 부산물의 시차 열분석 결과, 열변화 곡선이 안정적이며 주요 천이점이 $550^{\circ}C$에서 $610^{\circ}C$ 부근에 석영의 천이를 보이는 것과 열변화 곡선이 불안정적이며 여러 천이를 보이는 것으로 나뉘며, 골재 부산물의 경우는 흡 발열피크를 검토할 때 점토광물이 거의 없는 것으로 보인다.

• 대한미생물학회지
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• 제21권1호
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• pp.151-161
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• 1986

In order to develop sensitive and sepcific assay methods for E. coli heat labile enterotoxin(LT) hybridoma cell lines secreting LT specific monoclonal antibody were obtained. LT was purified from cell lysate of E. coli O15H11. The steps included disruption of bacteria by French pressure, DEAE Sephacel ion exchange chromatography, Sephadex G200 gel filtration, and second DEAE Sephacel ion exchange chromatography, successively. Spleen cells from Balb/c mice immunized with the purified LT and $HGPRT^{(-)}$ plasmacytomas, $P3{\times}63Ag8.V653$ were mixed and fused by 50% (w/v) PEG. Hybrid cells were grown in 308 wells out of 360 wells, and 13 wells out of them secreted antibodies reacting to LT. Among these hybridoma cell 1G8-1D1 cell line was selected since it had produced high-titered monoclonal antibody continuously. By using culture supernatant and ascites from 1G8-1D1 cells the monoclonal antibody was characterized, and an assay system for detecting enterotoxigenic E. coli was established by double sandwich enzyme-linked immunosorbent assay (ELISA). The following results were obtained. 1. Antibody titers of culture supernatant and ascites from 1G8-1D1 hybridoma cells were 512, and 102, 400, respectively by GM1-ELISA and its immunoglobulin class was IgM. 2. The maximum absorption ratio of 1G8-1D1 cell culture supernatant to LT was 90% at $300\;{\mu}g/ml$ of LT concentration. LT concentration shown at 50% absorption ratio was $103.45{\mu}g$ and the absorption ratio was decreased with tile reduction of LT concentration. This result suggests that monoclonal antibody from 1G8-1D1 hybridoma cell bound with LT specifically. 3. The reactivities of 1G8-1D1 cell culture supernatant to LT and V. cholerae enterotoxin(CT) were 0.886 and 0.142(O.D. at 492nm) measured by the GM1-ELISA, indicating 1G8-1D1 monoclonal antibody reacted specifically with LT but not with CT. 4. The addition of 0.1ml of ascites to 0.6mg and 0.12mg of LT decreased the vascular permeability factor to 41% and 44% respectively, but it did not completely neutralize LT. 5. By double sandwich ELISA using monoclonal antibody, as little as 75ng of the purified LT per ml could be detected. 6. The results by assay of detecting LT in culture supernatants of 14 wild strains E. coli isolated from diarrhea patients by the double sandwich ELISA were almost the same level as those by reverse passive latex agglutination.

• Restorative Dentistry and Endodontics
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• 제28권1호
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• pp.89-99
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• 2003

The purpose of this study was to investigate the bonding of resin- based root canal sealer, AH26 when the sealer was applied as a thin layer between dentine and gutta-percha surface. In this study forty non-caries extracted human molars and resin-based root canal sealer(AH 26, DeTrey/Dentsply, Germany) were used. Disks of gutta-percha, 6mm in diameter.6mm thick (Diadent/Dentsply, Korea) for thermoplastic obturation were used and dentin surfaces were treated with 2% NaOCl(Group 1) or 2%NaOCl+17% EDTA(Group 3). Disks of gutta-Percha, 6mm in diameter.6mm thick (Diadent/Dentsply, Korea) for conventional obturation were used and dentin surface were treated with 2% NaOCl(Group 2) or 2%NaOCl+17% EDTA(Group 4). Enamel was removed by a horizontal section 1mm below the deepest portion of the central occlusal groove by using a watercooled low speed diamond saw. A second horizontal section was done around cementoenamel junction. Exposed dentin surface was cut to approximately $8{\times}8{\;}mm$ rectangular shape and was ground against 320, 400, 600 grade silicon carbide abrasive paper serially. After grinding, the dentine surface were soaked in a solution of 2% NaOCl for 30 minutes and twenty of specimens were treated with 17% EDTA solution for 1 minute. The treated specimens were washed and dried, Root canal sealer, AH26 was prepared according to the manufacture's instructions The Gutta-percha and dentin surface were coated with a thin layer of the freshly mixed seal or. The specimens were left overnight at room temperature. After their initial set, they were transferred to an incubator at $37$^{\circ}C$ for 72 h. After 72 hours, resin blocks were made. The resin block was serially sectioned vertically into stick of $1{\cdot}1mm$. Twenty sticks were prepared from each group. After that, tensile bond strength f3r each stick was measured with Microtensile Tester Failure patterns of the specimens at the interface between gutta-percha and dentin were observed under the SEM(x1000) and Stereomicroscope (LEICA M42O, Meyer Inst., TX U.S.A) at 1.25 x25 magnification. The results were statistically analysed by using a One-way ANOVA and Tukey's test. The results were as follows; 1. Tensile bond strengths($mean{\pm}SD$) were expressed with ascending order as follows: Group 1, $3.09{\pm}$ 1.05Mpa : Group 2, $6.23{\pm}1.16MPa$ : Group 3, $7.12{\pm}1.07MPa$ : Group 4, $10.32{\pm}2.06MPa$. 2. Tensile bond strengths of the group 2 and 4 used disks of gutta-percha for conventional obturation were significantly higher than that of the group 1 and 3 used fir thermoplastic obturation. (p < 0.05). 3. Tensile bond strengths of the group 3 and 4 treated with 2% NaOC1+17% EDTA were significantly higher than that of the group 1 and 2 treated with 2% NaOCl. (p < 0.05). 4. In analysis of failure patterns at the interface between sealer and gutta-percha, there were observed 49 (61%)cases of adhesive failure patterns and 31 (39%) cases of mixed failures patterns.

• 한국자기학회지
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• 제13권6호
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• pp.237-242
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• 2003

$Ti_{1-x}$$^{57}$ F $e_{x}$ $O_2$(0.0$\leq$x$\leq$0.7) 분말을 졸-겔법으로 제조하여 $^{57}$ Fe의 치환량에 따른 결정학적 및 자기적 성질을 연구하였다. X-선 회절 및 중성자 회절실험을 통하며 모든 시료가 anatase 구조를 갖는 순수한 단일상임을 확인할 수 있었다. 진동시료자화율측정기 (VSM)를 통한 자기모멘트의 측정 결과, $^{57}$ Fe의 치환량이 증가함에 따라 상온에서의 Fe 원자 당 자기모멘트 값이 급격히 감소하는 매우 독특한 현상을 관측할 수 있었다. x$\leq$0.01 치환량을 갖는 시료들은 분명한 강자성 거동을 보였으며, x$\geq$0.03 치환량을 갖는 시료들에 대해서는 상자성 형태의 자화곡선이 관측되었다. 이에 대하여 14 K 부터 400 K까지 Mossbauer 분광실험을 한 결과 x$\leq$0.01 치환량을 갖는 시료의 경우 Ti $O_2$내의 $^{57}$ Fe가 상온에서 강자성(sextet)과 상자성(doublet) 형태로 동시에 존재함을 확인할 수 있었고, x$\geq$0.03 치환량을 갖는 시료들에 대해선 오직 상자성 상만을 나타내는 날카로운 doublet만이 존재함을 확인할 수 있었다. 이는 Mossbauer와 VSM 두 결과가 잘 일치함을 보여주고 있고, 상온에서 강자성을 나타내기 위한 $^{57}$ Fe의 치환한계가 x=0.01과 0.03 사이에 있음을 말해 주고 있다. 또한, 상온에서 강자성 성질을 갖는 x$\leq$0.01 시료들로부터 얻은 자기 모멘트 값이 매우 작은 것은 치환된 $^{57}$ Fe의 강자성 상과 상자성 상이 동시에 기여하기 때문에 얻어진 결과로 해석될 수 있다.다.

• 한국수자원학회:학술대회논문집
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• 한국수자원학회 2011년도 학술발표회
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• pp.8-9
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• 2011

On 4 September 2010 an earthquake of magnitude 7.1 on the Richter scale occurred on the Canterbury Plains in the South Island of New Zealand. The Canterbury Plains are an area of extensive groundwater and spring fed surface water systems. Since the September earthquake there have been several thousand aftershocks (Fig. 1), the largest being a 6.3 magnitude quake which occurred close to the centre of Christchurch on 22February 2011. This second quake caused extensive damage to the city of Christchurch including the deaths of 189 people. Both of these quakes had marked hydrological impacts. Water is a vital natural resource for Canterburywith groundwater being extracted for potable supply and both ground and surface water being used extensively for agricultural and horticultural irrigation.The groundwater is of very high quality so that the city of Christchurch (population approx. 400,000) supplies untreated artesian water to the majority of households and businesses. Both earthquakes caused immediate hydrological effects, the most dramatic of which was the liquefaction of sediments and the release of shallow groundwater containing a fine grey silt-sand material. The liquefaction that occurred fitted within the empirical relationship between distance from epicentre and magnitude of quake described by Montgomery et al. (2003). . It appears that liquefaction resulted in development of discontinuities in confining layers. In some cases these appear to have been maintained by artesian pressure and continuing flow, and the springs are continuing to flow even now. In spring-fed streams there was an increase in flow that lasted for several days and in some cases flows remained high for several months afterwards although this could be linked to a very wet winter prior to the September earthquake. Analysis of the slope of baseflow recession for a spring-fed stream before and after the September earthquake shows no change, indicating no substantial change in the aquifer structure that feeds this stream.A complicating factor for consideration of river flows was that in some places the liquefaction of shallow sediments led to lateral spreading of river banks. The lateral spread lessened the channel cross section so water levels rose although the flow might not have risen accordingly. Groundwater level peaks moved both up and down, depending on the location of wells. Groundwater level changes for the two earthquakes were strongly related to the proximity to the epicentre. The February 2011 earthquake resulted in significantly larger groundwater level changes in eastern Christchurch than occurred in September 2010. In a well of similar distance from both epicentres the two events resulted in a similar sized increase in water level but the slightly slower rate of increase and the markedly slower recession recorded in the February event suggests that the well may have been partially blocked by sediment flowing into the well at depth. The effects of the February earthquake were more localised and in the area to the west of Christchurch it was the earlier earthquake that had greater impact. Many of the recorded responses have been compromised, or complicated, by damage or clogging and further inspections will need to be carried out to allow a more definitive interpretation. Nevertheless, it is reasonable to provisionally conclude that there is no clear evidence of significant change in aquifer pressures or properties. The different response of groundwater to earthquakes across the Canterbury Plains is the subject of a new research project about to start that uses the information to improve groundwater characterisation for the region. Montgomery D.R., Greenberg H.M., Smith D.T. (2003) Stream flow response to the Nisqually earthquake. Earth & Planetary Science Letters 209 19-28.