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    농업용 저수지 소하천의 통계학적 수질변화 특성 = Statistical Study of the Long-term Changes in Water Quality Parameters of the Small Streams in Agricultural Reservoir

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    https://www.riss.kr/link?id=A40124583

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    The results of investigation for the long-term changes in water quality of the small streams in agricultural reservoir indicate that nitrogen is determined mainly by the agricultural activities while phosphorus and suspended solids are affected by the soil particles moved by irrigation return flow or/and rainfall discharge. However, nitrogen is related with factors of the flow more than suspended solids concentration but rather tends to decrease with the abundant stream flows caused by rainfalls. As the use of land for rice paddy in the watershed increases, more nitrogen loss was also observed. It was found that about 50% of the total phosphorus and nitrogen exists in dissolved form. There is a possibility to develop tools which can be used to predict dissolved forms of the nutrient by TDS values easily and reliably measured by electrical conductivity. Coefficient of determination(R²) between TDS and phosphorus concentration was higher than the nitrogen concentration. Especially, the more rice paddy area, the higher correlation coefficient. In addition, TDS was inversely correlated with flow(or depth) due to the dilution effect of rainfall water, so that multiple rating curves from flow depth to approximate TDS and then nutrients could be useful. Most of the water quality parameters were found to have a log-normal probability distribution.
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    The results of investigation for the long-term changes in water quality of the small streams in agricultural reservoir indicate that nitrogen is determined mainly by the agricultural activities while phosphorus and suspended solids are affected by the...

    The results of investigation for the long-term changes in water quality of the small streams in agricultural reservoir indicate that nitrogen is determined mainly by the agricultural activities while phosphorus and suspended solids are affected by the soil particles moved by irrigation return flow or/and rainfall discharge. However, nitrogen is related with factors of the flow more than suspended solids concentration but rather tends to decrease with the abundant stream flows caused by rainfalls. As the use of land for rice paddy in the watershed increases, more nitrogen loss was also observed. It was found that about 50% of the total phosphorus and nitrogen exists in dissolved form. There is a possibility to develop tools which can be used to predict dissolved forms of the nutrient by TDS values easily and reliably measured by electrical conductivity. Coefficient of determination(R²) between TDS and phosphorus concentration was higher than the nitrogen concentration. Especially, the more rice paddy area, the higher correlation coefficient. In addition, TDS was inversely correlated with flow(or depth) due to the dilution effect of rainfall water, so that multiple rating curves from flow depth to approximate TDS and then nutrients could be useful. Most of the water quality parameters were found to have a log-normal probability distribution.

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    유사연구자 (20) 활용도상위20명

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    학술지 이력

    학술지 이력
    연월일 이력구분 이력상세 등재구분
    2027 평가 재인증평가 신청대상 (재인증)
    2021-01-01 등재 등재학술지 유지 (재인증) KCI등재
    2018-01-01 등재 등재학술지 유지 (등재유지) KCI등재
    2015-01-01 등재 등재학술지 유지 (등재유지) KCI등재
    2012-01-01 학술지명변경 한글명 : 수질보전 한국물환경학회지 -> 한국물환경학회지
    외국어명 : 미등록 -> Journal of Korean Society on Water Environment
    KCI등재
    2011-12-27 학회명변경 영문명 : Korean Society on Water Quality -> Korean Society on Water Environment KCI등재
    2011-01-01 등재 등재학술지 유지 (등재유지) KCI등재
    2009-07-22 학회명변경 영문명 : Journal Of Korean Society On Water Qulity -> Korean Society on Water Quality KCI등재
    2009-01-01 등재 등재학술지 유지 (등재유지) KCI등재
    2007-01-01 등재 등재학술지 유지 (등재유지) KCI등재
    2004-01-01 등재 등재학술지 선정 (등재후보2차) KCI등재
    2003-01-01 등재 등재후보 1차 PASS (등재후보1차) KCI등재후보
    2001-07-01 등재 등재후보학술지 선정 (신규평가) KCI등재후보
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    학술지 인용정보

    학술지 인용정보
    기준연도 WOS-KCI 통합IF(2년) KCIF(2년) KCIF(3년)
    2016 0.51 0.51 0.46
    KCIF(4년) KCIF(5년) 중심성지수(3년) 즉시성지수
    0.43 0.39 0.613 0.15
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