第五章 結果與討論
6.2 建議
1. 本研究使用 QUAL2K 作為水質模擬模式,為美國環保署所發展之 軟體,建構在 Excel 介面下,雖改善操作介面,但運算時間過長,
提高模擬次數將使整體模擬時間大幅增加,若改以 QUAL2E 或其 他水質模擬軟體,可減少模擬時間。
2. 研究僅針對河川水資源調配及河川水質管理作探討,而未考慮成本 效益等因素,未來能整合其他因素考量,將可使系統更趨完善。
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網路部份:
水文水資源資料管理供應系統,http://gweb.wra.gov.tw/wrweb/
行政院環保署環境資料庫,http://gweb.wra.gov.tw/wrweb/
經濟部水利署,http://www.wra.gov.tw/default.asp 美國環境保護署,http://www.epa.gov/
附錄
附表1 續 荖濃溪流量馬可夫鏈轉換矩陣
附表1 續 荖濃溪流量馬可夫鏈轉換矩陣
附表1 續 荖濃溪流量馬可夫鏈轉換矩
十月
Q100 Q90 Q80 Q70 Q60 Q50 Q40 Q30 Q20 Q10 Q0
Q90 100.0% 0.0% 0.0% 0.0% 0.0% 0.0% 0.0% 0.0% 0.0% 0.0%
Q80 0.0% 0.0% 0.0% 0.0% 0.0% 0.0% 0.0% 0.0% 0.0% 0.0%
Q70 0.0% 0.0% 0.0% 100.0% 40.0% 16.7% 0.0% 0.0% 0.0% 0.0%
Q60 0.0% 0.0% 0.0% 0.0% 60.0% 58.3% 16.7% 0.0% 0.0% 0.0%
Q50 0.0% 0.0% 0.0% 0.0% 0.0% 0.0% 33.3% 22.2% 33.3% 0.0%
Q40 0.0% 0.0% 0.0% 0.0% 0.0% 8.3% 50.0% 66.7% 33.3% 0.0%
Q30 0.0% 0.0% 0.0% 0.0% 0.0% 8.3% 0.0% 11.1% 11.1% 0.0%
Q20 0.0% 0.0% 0.0% 0.0% 0.0% 8.3% 0.0% 0.0% 11.1% 0.0%
Q10 0.0% 0.0% 0.0% 0.0% 0.0% 0.0% 0.0% 0.0% 11.1% 0.0%
十一月
Q0 0.0% 0.0% 0.0% 0.0% 0.0% 0.0% 0.0% 0.0% 0.0% 0.0%
Q100 十一月
Q90 100.0% 0.0% 0.0% 0.0% 0.0% 0.0% 0.0% 0.0% 0.0% 0.0%
Q80 0.0% 0.0% 80.0% 58.3% 0.0% 0.0% 0.0% 0.0% 0.0% 0.0%
Q70 0.0% 0.0% 20.0% 41.7% 66.7% 6.3% 33.3% 0.0% 0.0% 0.0%
Q60 0.0% 0.0% 0.0% 0.0% 33.3% 56.3% 0.0% 50.0% 0.0% 0.0%
Q50 0.0% 0.0% 0.0% 0.0% 0.0% 31.3% 66.7% 50.0% 100.0% 0.0%
Q40 0.0% 0.0% 0.0% 0.0% 0.0% 0.0% 0.0% 0.0% 0.0% 0.0%
Q30 0.0% 0.0% 0.0% 0.0% 0.0% 0.0% 0.0% 0.0% 0.0% 0.0%
Q20 0.0% 0.0% 0.0% 0.0% 0.0% 0.0% 0.0% 0.0% 0.0% 0.0%
Q10 0.0% 0.0% 0.0% 0.0% 0.0% 6.3% 0.0% 0.0% 0.0% 0.0%
十二月
Q0 0.0% 0.0% 0.0% 0.0% 0.0% 0.0% 0.0% 0.0% 0.0% 0.0%
附表2 隘寮溪流量馬可夫鏈轉換矩陣
附表2 續 隘寮溪流量馬可夫鏈轉換矩陣
附表2 續 隘寮溪流量馬可夫鏈轉換矩陣
附表2 續 隘寮溪流量馬可夫鏈轉換矩
十月
Q100 Q90 Q80 Q70 Q60 Q50 Q40 Q30 Q20 Q10 Q0
Q90 0.0% 0.0% 0.0% 66.7% 0.0% 0.0% 0.0% 0.0% 0.0% 0.0%
Q80 0.0% 0.0% 0.0% 33.3% 0.0% 25.0% 0.0% 0.0% 0.0% 0.0%
Q70 0.0% 0.0% 100.0% 0.0% 66.7% 25.0% 0.0% 14.3% 0.0% 0.0%
Q60 0.0% 0.0% 0.0% 0.0% 0.0% 12.5% 16.7% 0.0% 20.0% 0.0%
Q50 0.0% 0.0% 0.0% 0.0% 0.0% 25.0% 16.7% 0.0% 0.0% 0.0%
Q40 0.0% 0.0% 0.0% 0.0% 0.0% 12.5% 50.0% 71.4% 50.0% 60.0%
Q30 0.0% 0.0% 0.0% 0.0% 33.3% 0.0% 16.7% 0.0% 20.0% 0.0%
Q20 0.0% 0.0% 0.0% 0.0% 0.0% 0.0% 0.0% 14.3% 10.0% 20.0%
Q10 0.0% 0.0% 0.0% 0.0% 0.0% 0.0% 0.0% 0.0% 0.0% 20.0%
十一月
Q0 0.0% 0.0% 0.0% 0.0% 0.0% 0.0% 0.0% 0.0% 0.0% 0.0%
Q100 十一月
Q90 50.0% 66.7% 28.6% 25.0% 0.0% 0.0% 0.0% 0.0% 0.0% 0.0%
Q80 0.0% 33.3% 14.3% 0.0% 0.0% 0.0% 0.0% 0.0% 0.0% 0.0%
Q70 50.0% 0.0% 57.1% 50.0% 33.3% 17.6% 25.0% 33.3% 0.0% 0.0%
Q60 0.0% 0.0% 0.0% 25.0% 0.0% 5.9% 0.0% 0.0% 0.0% 0.0%
Q50 0.0% 0.0% 0.0% 0.0% 66.7% 70.6% 25.0% 0.0% 0.0% 0.0%
Q40 0.0% 0.0% 0.0% 0.0% 0.0% 5.9% 25.0% 33.3% 0.0% 0.0%
Q30 0.0% 0.0% 0.0% 0.0% 0.0% 0.0% 25.0% 0.0% 100.0% 0.0%
Q20 0.0% 0.0% 0.0% 0.0% 0.0% 0.0% 0.0% 0.0% 0.0% 0.0%
Q10 0.0% 0.0% 0.0% 0.0% 0.0% 0.0% 0.0% 33.3% 0.0% 0.0%
十二月
Q0 0.0% 0.0% 0.0% 0.0% 0.0% 0.0% 0.0% 0.0% 0.0% 0.0%
附表3 旗山溪流量馬可夫鏈轉換矩陣
附表3 續 旗山溪流量馬可夫鏈轉換矩陣
附表3 續 旗山溪流量馬可夫鏈轉換矩陣
附表3 續 旗山溪流量馬可夫鏈轉換矩陣
十月
Q100 Q90 Q80 Q70 Q60 Q50 Q40 Q30 Q20 Q10 Q0
Q90 0.0% 0.0% 0.0% 0.0% 0.0% 0.0% 0.0% 0.0% 0.0% 0.0%
Q80 0.0% 0.0% 0.0% 0.0% 0.0% 0.0% 0.0% 0.0% 0.0% 0.0%
Q70 0.0% 0.0% 0.0% 0.0% 0.0% 0.0% 0.0% 0.0% 0.0% 0.0%
Q60 0.0% 0.0% 0.0% 100.0% 0.0% 50.0% 0.0% 0.0% 50.0% 0.0%
Q50 0.0% 0.0% 0.0% 0.0% 0.0% 50.0% 100.0% 100.0% 0.0% 0.0%
Q40 0.0% 0.0% 0.0% 0.0% 100.0% 0.0% 0.0% 0.0% 50.0% 0.0%
Q30 0.0% 0.0% 0.0% 0.0% 0.0% 0.0% 0.0% 0.0% 0.0% 0.0%
Q20 0.0% 0.0% 0.0% 0.0% 0.0% 0.0% 0.0% 0.0% 0.0% 0.0%
Q10 0.0% 0.0% 0.0% 0.0% 0.0% 0.0% 0.0% 0.0% 0.0% 0.0%
十一月
Q0 0.0% 0.0% 0.0% 0.0% 0.0% 0.0% 0.0% 0.0% 0.0% 0.0%
Q100 十一月
Q90 0.0% 0.0% 0.0% 0.0% 25.0% 0.0% 0.0% 0.0% 0.0% 0.0%
Q80 0.0% 0.0% 0.0% 100.0% 0.0% 0.0% 0.0% 0.0% 0.0% 0.0%
Q70 0.0% 0.0% 0.0% 0.0% 25.0% 0.0% 0.0% 0.0% 0.0% 0.0%
Q60 0.0% 0.0% 0.0% 0.0% 50.0% 0.0% 0.0% 0.0% 0.0% 0.0%
Q50 0.0% 0.0% 0.0% 0.0% 0.0% 100.0% 0.0% 0.0% 0.0% 0.0%
Q40 0.0% 0.0% 0.0% 0.0% 0.0% 0.0% 0.0% 0.0% 0.0% 0.0%
Q30 0.0% 0.0% 0.0% 0.0% 0.0% 0.0% 0.0% 0.0% 0.0% 0.0%
Q20 0.0% 0.0% 0.0% 0.0% 0.0% 0.0% 0.0% 0.0% 0.0% 0.0%
Q10 0.0% 0.0% 0.0% 0.0% 0.0% 0.0% 0.0% 0.0% 0.0% 0.0%
十二月
Q0 0.0% 0.0% 0.0% 0.0% 0.0% 0.0% 0.0% 0.0% 0.0% 0.0%