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      강우시 비영농기와 영농기의 광역 논에서의 오염물질 유출 특성 = Pollutant runoff from a paddy field watershed during storms in the non-growing and growing seasons

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      https://www.riss.kr/link?id=T13262121

      • 저자
      • 발행사항

        청주 : 忠北大學校大學院, 2013

      • 학위논문사항

        학위논문(석사) -- 충북대학교대학원 , 지역건설공학과(원) , 2013. 8

      • 발행연도

        2013

      • 작성언어

        한국어

      • KDC

        539.1584 판사항(5)

      • 발행국(도시)

        충청북도

      • 형태사항

        viii, 52 p. : 삽화 ; 26 cm.

      • 일반주기명

        충북대학교 논문은 저작권에 의해 보호됩니다
        지도교수 :김진수
        참고문헌 : p.47-52

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      다국어 초록 (Multilingual Abstract) kakao i 다국어 번역

      The objective of this research was to investigate pollutant dynamics from a 26.2 ha rice field watershed during non-growing and growing seasons. Water samples were collected, and runoff water was measured at 1~6 hours intervals during six storm events of the year 2011~2012 .
      The water samples were analyzed for total nitrogen (TN), nitrate-nitrogen (NO3-N), total phosphorous (TP), phosphate-phosphorous (PO4-P), suspended solid (SS) and chemical oxygen demand (COD).
      Mean flow-weighted concentrations of pollutants were 10.2 mg/L for TN, 6.9 mg/L for NO3-N, 0.50 mg/L for TP, 0.35 mg/L for PO4-P, 64.4 mg/L for SS and 29.4 mg/L for COD in the non-growing season and 1.7 mg/L for TN, 1.2 mg/L for NO3-N, 0.16 mg/L for TP, 0.07 mg/L for PO4-P, 59.0 mg/L for SS and 11.5 mg/L for COD in the mid-growing season.
      The mean flow-weighted concentrations of pollutants except for SS in the non-growing season were higher than those in the mid-growing season. The mean flow-weighted concentration of SS in the non-growing season was almost the same as that in the mid-growing season. This may be because rice plant residues on the topsoil in the non-growing season act as surface mulch, and therefore prevent soil erosion.
      The average ratio of NO3-N to TN in the non-growing season was 68.0%, similar to 70.0% in the mid-growing season. However, the average ratios of PO4-P to TP in the non-growing season was 70.0%, much higher than 44.0% in the mid-growing season. The high average ratios of PO4-P to TP in the non-growing season may be due to mineralization and desorption of P caused by low soil water content.
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      The objective of this research was to investigate pollutant dynamics from a 26.2 ha rice field watershed during non-growing and growing seasons. Water samples were collected, and runoff water was measured at 1~6 hours intervals during six storm even...

      The objective of this research was to investigate pollutant dynamics from a 26.2 ha rice field watershed during non-growing and growing seasons. Water samples were collected, and runoff water was measured at 1~6 hours intervals during six storm events of the year 2011~2012 .
      The water samples were analyzed for total nitrogen (TN), nitrate-nitrogen (NO3-N), total phosphorous (TP), phosphate-phosphorous (PO4-P), suspended solid (SS) and chemical oxygen demand (COD).
      Mean flow-weighted concentrations of pollutants were 10.2 mg/L for TN, 6.9 mg/L for NO3-N, 0.50 mg/L for TP, 0.35 mg/L for PO4-P, 64.4 mg/L for SS and 29.4 mg/L for COD in the non-growing season and 1.7 mg/L for TN, 1.2 mg/L for NO3-N, 0.16 mg/L for TP, 0.07 mg/L for PO4-P, 59.0 mg/L for SS and 11.5 mg/L for COD in the mid-growing season.
      The mean flow-weighted concentrations of pollutants except for SS in the non-growing season were higher than those in the mid-growing season. The mean flow-weighted concentration of SS in the non-growing season was almost the same as that in the mid-growing season. This may be because rice plant residues on the topsoil in the non-growing season act as surface mulch, and therefore prevent soil erosion.
      The average ratio of NO3-N to TN in the non-growing season was 68.0%, similar to 70.0% in the mid-growing season. However, the average ratios of PO4-P to TP in the non-growing season was 70.0%, much higher than 44.0% in the mid-growing season. The high average ratios of PO4-P to TP in the non-growing season may be due to mineralization and desorption of P caused by low soil water content.

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      목차 (Table of Contents)

      • Ⅰ. 서 론 1
      • Ⅱ. 연 구 사 3
      • Ⅲ. 조사지구 및 연구방법 8
      • Ⅰ. 서 론 1
      • Ⅱ. 연 구 사 3
      • Ⅲ. 조사지구 및 연구방법 8
      • 3.1 조사지구 8
      • 3.1.1 개요 8
      • 3.1.2 기상 11
      • 3.1.3 배수로 13
      • 3.1.4 논의 작물과 수분 상태 14
      • 3.2 연구방법 15
      • 3.2.1 조사시기 15
      • 3.2.2 토양 15
      • 3.2.3 시비시기 및 시비량 17
      • 3.2.4 유속 17
      • 3.2.5 강우량 19
      • 3.2.6 수질 19
      • Ⅳ. 결과 및 고찰 20
      • 4.1 토성과 시비 20
      • 4.1.1 토성 20
      • 4.1.2 시비시기 및 시비량 22
      • 4.2 강수량 24
      • 4.2.1 비영농기 24
      • 4.2.2 영농기 25
      • 4.3 강우사상 개요 26
      • 4.4 강우 오염물질 농도 27
      • 4.5 시기별 강우시 오염물질 농도변화 특성 28
      • 4.5.1 N 농도 28
      • 4.5.2 P 농도 30
      • 4.5.3 SS 농도 32
      • 4.5.4 COD 농도 34
      • 4.6 오염물질 유량가중 평균농도 36
      • 4.7 유출량과 부하량 38
      • 4.7.1 부하량 38
      • 4.7.2 유출량-부하량 관계 39
      • 4.8 오염물질 평균농도의 비 43
      • 4.8.1 NO3-N/TN의 비 43
      • 4.8.2 PO4-P/TP의 비 44
      • Ⅴ. 결 론 45
      • Ⅵ. 참고문헌 47
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