• 제목/요약/키워드: Clogging factor

검색결과 24건 처리시간 0.031초

미고결대수층에서 우물 굴착 및 개량에 의한 대수층의 수리특성 변화 (Change of Hydraulic Characteristics due to Well Drilling and Well Development in an Unconsolidated Aquifer)

  • 김병우;김규범;김건영
    • 지질공학
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    • 제22권1호
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    • pp.27-37
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    • 2012
  • 미고결대수층에서 우물 굴착 시 대수층 교란이 수리특성에 미치는 영향을 파악하기 위하여 우물굴착 이후의 우물개량 공법인 서지블록과 에어서징을 실시하였다. 그리고 우물 굴착 및 개량의 대수층 변화를 비교 분석하기, 위하여 단계 및 장기 양수시험을 수행하였다. 그 결과 우물 굴착 및 개량 이후의 단계양수시험에서 동일 양수율 $700m^3/day$에 대한 수위강하와 비교하였을 때 수위강하는 각각 26.01 m, 21.62 m로 4.39 m정도 감소되었다. 이때 우물특성을 파악하기 위한 우물 굴착 및 개량 이후의 스킨계수는 7.92에서 5.04로 감소되어 우물상태가 개선된 것으로 나타났다. 우물 굴착 및 개량 이후의 장기양수시험에서 양수정을 중심으로 주변 MW-2, 3, 4호정의 투수량계수 범위는 각각 $1.684{\times}10^{-3}{\sim}4.490{\times}10^{-3}m^2/sec$, $4.002{\times}10^{-3}{\sim}4.939{\times}10^{-3}m^2/sec$ 범위로 우물개량 이후의 수리전도도 값이 조금 증가되었으며, MW-1호정은 $1.018{\times}10^{-2}m^2/sec$에서 $6.988{\times}10^{-3}m^2/sec$로 감소되었다. 이는 서징하는 동안 대수층의 공기 차단 및 폐색의 잠재적인 요인으로 인하여 MW-1호정 주변 대수층의 투수성이 미세하게 감소되는 효과로 나타났다. 따라서 미고결대수층에서 우물 굴착 시 미세입자가 양수정 주변의 수리특성에 영향을 미칠 수 있음을 반드시 유의해야 한다.

하수처리수를 이용한 인공수로에서 사상성 부착조류의 성장에 영향을 미치는 요인들 (Factors to Affect the Growth of Filamentous Periphytic Algae in the Artificial Channels using Treated Wastewater)

  • 박구성;김호섭;공동수;신재기;황순진
    • 생태와환경
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    • 제39권1호통권115호
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    • pp.100-109
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    • 2006
  • 본 연구는 영양염이 풍부한 하수처리수를 이용한 인공수로에서 사상성 부착조류의 성장에 미치는 요인들(유속. 부착기질, 인 농도)을 평가하였다. 실험은 하수처리수를 이용한 현장 인공수로와 실내 순환수로에서 부착조류의 성장실험을 수행하였고, 서로 다른 인 농도에서의 사상성 부착조류 종간의 성장률과 인 흡수율을 비교하였다. 조절된 유속조건(5 ${\sim}$ 15 cm $s^{-1}$)에서 사상성 부착조류의 순생산성은 유속이 빠를수록 높았으나 최대의 순생산성은 10 cm $s^{-1}$ 유속에서 나타났다. 현장 인공수로와 실내순환수로 실험 간에 사상성부착조류의 최대성장은 기질에 따라 다르게 나타났다. 부유물질이 충분히 제거되지 않았던 현장 인공수로 실험에서는 망목이 20 mm인 철망에서, 실내순환수로 실험에서 사상성 부착조류의 성장은 자연섬유망에서 높게 나타났다. 0.05 ${\sim}$ l.0 mg P $L^{-1}$로 조절된 인 농도범위에서 3종의 사상성 부착조류 성장률은 인 농도가 높아짐에 따라 증가하였으나, 각 종들은 인 농도에서 따라 차별적인 성장을 나타냈다. 또한 영양염 농도가 매우 높은 환경에서 사상성 부착조류 생물량의 발달이 크면 클수록 높은 유속이 사상체의 탈리를 유발하여 조류의 성장을 감소시키는 제한요인으로 작용할 수 있음이 제시되었다. 탈리된 사상체는 연결된 하천, 저수지, 하류의 수질과 생태계를 악화시킬 수 있기 때문에 하천 수질관리에 있어 중요한 요인으로 고려한 필요성이 크다.

멀티도어코트하우스제도: 기원, 확장과 사례분석 (The Multi-door Courthouse: Origin, Extension, and Case Studies)

  • 정용균
    • 한국중재학회지:중재연구
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    • 제28권2호
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    • pp.3-43
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    • 2018
  • The emergence of a multi-door courthouse is related with a couple of reasons as follows: First, a multi-door courthouse was originally initiated by the United States government that increasingly became impatient with the pace and cost of protracted litigation clogging the courts. Second, dockets of courts are overcrowded with legal suits, making it difficult for judges to handle those legal suits in time and causing delays in responding to citizens' complaints. Third, litigation is not suitable for the disputant that has an ongoing relationship with the other party. In this case, even if winning is achieved in the short run, it may not be all that was hoped for in the long run. Fourth, international organizations such as the World Bank, UNDP, and Asia Development Bank urge to provide an increased access to women, residents, and the poor in local communities. The generic model of a multi-door courthouse consists of three stages: The first stage includes a center offering intake services, along with an array of dispute resolution services under one roof. At the second stage, the screening unit at the center would diagnose citizen disputes, then refer the disputants to the appropriate door for handling the case. At the third stage, the multi-door courthouse provides diverse kinds of dispute resolution programs such as mediation, arbitration, mediation-arbitration (med-arb), litigation, and early neutral evaluation. This study suggests the extended model of multi-door courthouse comprised of five layers: intake process, diagnosis and door-selection process, neutral-selection process, implementation process of dispute resolution, and process of training and education. One of the major characteristics of extended multi-door courthouse model is the detailed specification of individual department corresponding to each process within a multi-door courthouse. The intake department takes care of the intake process. The screening department plays the role of screening disputes, diagnosing the nature of disputes, and determining a suitable door to handle disputes. The human resources department manages experts through the construction and management of the data base of mediators, arbitrators, and judges. The administration bureau manages the implementation of each process of dispute resolution. The education and training department builds long-term planning to procure neutrals and experts dealing with various kinds of disputes within a multi-door courthouse. For this purpose, it is necessary to establish networks among courts, law schools, and associations of scholars in order to facilitate the supply of manpower in ADR neutrals, as well as judges in the long run. This study also provides six case studies of multi-door courthouses across continents in order to grasp the worldwide picture and wide spread phenomena of multi-door courthouse. For this purpose, the United States and Latin American countries including Argentina and Brazil, Middle Eastern countries, and Southeast Asian countries (such as Malaysia and Myanmar), Australia, and Nigeria were chosen. It was found that three kinds of patterns are discernible during the evolution of a multi-door courthouse model. First, the federal courts of the United States, land and environment court in Australia, and Lagos multi-door courthouse in Nigeria may maintain the prototype of a multi-door courthouse model. Second, the judicial systems in Latin American countries tend to show heterogenous patterns in terms of the adaptation of a multi-door courthouse model to their own environments. Some court systems of Latin American countries including those of Argentina and Brazil resemble the generic model of a multi-door courthouse, while other countries show their distinctive pattern of judicial system and ADR systems. Third, it was found that legal pluralism is prevalent in Middle Eastern countries and Southeast Asian countries. For example, Middle Eastern countries such as Saudi Arabia have developed various kinds of dispute resolution methods, such as sulh (mediation), tahkim (arbitration), and med-arb for many centuries, since they have been situated at the state of tribe or clan instead of nation. Accordingly, they have no unified code within the territory. In case of Southeast Asian countries such as Myanmar and Malaysia, they have preserved a strong tradition of customary laws such as Dhammthat in Burma, and Shriah and the Islamic law in Malaysia for a long time. On the other hand, they incorporated a common law system into a secular judicial system in Myanmar and Malaysia during the colonial period. Finally, this article proposes a couple of factors to strengthen or weaken a multi-door courthouse model. The first factor to strengthen a multi-door courthouse model is the maintenance of flexibility and core value of alternative dispute resolution. We also find that fund raising is important to build and maintain the multi-door courthouse model, reflecting the fact that there has been a competition surrounding the allocation of funds within the judicial system.

Earthquake impacts on hydrology: a case study from the Canterbury, New Zealand earthquakes of 2010 and 2011

  • Davie, Tim;Smith, Jeff;Scott, David;Ezzy, Tim;Cox, Simon;Rutter, Helen
    • 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.

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