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포천지역 계류 (부소천)의 수질과 부착조류 생물량에 온배수와 수소이온농도 (pH) 영향
Effects of Thermal Wastewater Effluent and Hydrogen Ion Potential (pH) on Water Quality and Periphyton Biomass in a Small Stream (Buso) of Pocheon Area, Korea 원문보기

생태와 환경 = Korean journal of ecology and environment, v.50 no.1, 2017년, pp.96 - 115  

전경혜 (건국대학교 환경보건과학과) ,  엄현수 (건국대학교 환경보건과학과) ,  정진호 (고려대학교 환경생태공학부) ,  황순진 (건국대학교 환경보건과학과) ,  신재기 (한국수자원공사 낙동강남부권관리단)

초록
AI-Helper 아이콘AI-Helper

온배수와 산성화는 오래 전부터 전 세계를 통해 육수학과 수생태학에서 많은 관심을 갖게 한 분야이었다. 그러나 우리나라는 아직까지 초보적이거나 접근 조차 미진한 실정에 있다. 본 연구는 2015년 12월부터 2016년 9월까지 경기도 포천에 위치한 계류(부소천)의 최상류 구간 5개 지점(BSU (상류), HSW (온천폐수 방류구), BSD1~3 (하류))에서 수질환경과 부착조류 생태계에 온배수와 산성비의 시공간적 영향을 파악하고자 매월 조사하였다. 조사기간 동안 수온의 범위(평균값)는 $1.7{\sim}28.8^{\circ}C$($15.0^{\circ}C$)이었다. 특히 HSW의 범위와 평균값은 17.5 (1월)~$28.8^{\circ}C$(9월), $24.2{\pm}3.7^{\circ}C$로서 고온을 유지하였고, 다른 지점에 비해 월등히 높았다. 온배수는 하천수의 수온 증가와 영양염 펄스로서 작용하였으며, 그 영향은 갈수기와 저온기 (12월~3월)에 우세하였다. 그리고 온도의 영향권은 유하 거리에 따라 멀지 않았으나, P N 영양염은 다소 원거리까지 미칠 수 있는 잠재력을 갖고 있었다. pH는 5.1~8.4 (6.9)이었다. 수중 pH 감소의 원인은 계절적으로 강설과 산성비의 습윤 산성강하물에 있었고, 그 영향은 부착 규조류 중 호산성 종조성(Eunotia pectinalis, Tabellaria flocculosa)의 생물학적 분포에서 간헐적(3월과 8월)으로 확인되었다. 부소천의 수질과 부착조류 생태계는 열 오염, 부영양화 및 산성화에 의한 역동적인 상태이었고, 계류, 온배수 및 대기오염과 같은 지리 지역적 특성에 기반한 인위적 영향이 지배적이었다.

Abstract ▼ AI-Helper 아이콘AI-Helper

Understanding effects of thermal pollution and acidification has long been a concern of aquatic ecologists, but it remains largely unknown in Korea. This study was performed to elucidate the effects of thermal wastewater effluent (TWE) and acid rain on water quality and attached algae in a small mou...

주제어

#acidification   #acid rain   #hot-spring wastewater   #periphyton   #stream   #thermal pollution   #water quality  

질의응답

핵심어 질문 논문에서 추출한 답변
계류성 소하천의 특징은 무엇인가? 경기도 포천지역에 위치한 부소천은 산지에서 발원하는 원류성 계류 (溪流)로서 남북공유하천 임진강의 제1지류인 한탄강(댐) 상류에 유입되는 지천이다(MOLIT, 2012). 계류성 소하천은 본래 산림구역에 인접하여 오염원과 인위적 교란이 거의 없는 청정지역에 속하며, 수온이 비교적 차고 연중 유수환경이 유지되어 1차 생산자 중 식물플랑크톤보다 부착조류 생태계가 우세하다(Shin and Cho, 1998; Kim, 2004a). 부착조류는 서식지로서 하천을 이용하는 가장 성공적인 생물군이며(Stevenson et al.
부소천이란 무엇인가? 경기도 포천지역에 위치한 부소천은 산지에서 발원하는 원류성 계류 (溪流)로서 남북공유하천 임진강의 제1지류인 한탄강(댐) 상류에 유입되는 지천이다(MOLIT, 2012). 계류성 소하천은 본래 산림구역에 인접하여 오염원과 인위적 교란이 거의 없는 청정지역에 속하며, 수온이 비교적 차고 연중 유수환경이 유지되어 1차 생산자 중 식물플랑크톤보다 부착조류 생태계가 우세하다(Shin and Cho, 1998; Kim, 2004a).
수중 수소이온농도의 증감 변화를 일으키는 요인에는 무엇이 있는가? 0)을 기준으로 이산화탄소(Free CO2)-중탄산염(HCO3-)-탄산염(CO32-) 관계에서 무기탄소 종의 상대비율을 파악하는 데 유용하다 (Wetzel, 2001). 일반적으로, pH는 수온, 광합성 (식물), 호흡 (동물) 및 분해 (미생물)작용 그리고 오염도 (예, 생활계, 산업계(광산 포함)의 하·폐수 또는 산림, 토양의 부식질)에 따른 수중 CO2 양에 의해 하루 중 또는 경시적인 증감 변화가 일어난다(Wetzel, 2001; Park, 2010). 이 외에 인간 생활권에서 산업화, 도시화 및 현대화에 따른 대기오염 기원 산성강하물의 영향이 날로 가중되고 있는 실정에 있으며, 그 형태는 습성 (예, 눈과 비)과 건성 (예, 미세먼지 (PM))으로 구분된다(NIER, 2004).
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