環境資源報告成果查詢系統

日月潭底泥岩芯調查與分析示範計畫

中文摘要 本計畫完成日月潭底部的聲納震測掃描,據此在日潭和月潭共擇定兩個站位,總計鑽採5支岩芯,累計總長度超過825 cm,符合計畫預期之標準。對每根岩芯均進行底泥描述及照相紀錄,並進行多感測元岩芯物理參數掃描、反射光譜量測及X光螢光掃描等非破壞性分析,並依環保署要求加做放射性定年分析工作,完成55個定年分析樣。最後本計畫針對成果提出岩芯作業標準規範,做為日後湖泊底泥採樣參考之標準作業流程。 本計畫所獲取岩芯均反應超過1934年日月潭建壩時間之深度,定年結果指出日潭岩芯具有較佳定年參考點。同時發現日潭Sun 2站位之沉積速率約為月潭Moon 1站位的3倍,顯示底泥主要供應源來自日潭東北方往月潭搬送。從岩芯射線、孔隙率、磁感率等物理參數資料發現日潭及月潭在建壩前、後底泥組成有明顯改變,反映蓄水後確造成有機物質的減少;X光螢光掃描發現部分重金屬元素組成有明顯變化,可能反應底泥源區產生改變:例如在1934年以前底泥Ni含量較高,反映來源以當時集水盆地為主,但建壩後Pb、Zn、Cr含量大幅增加,同時Ca含量也大幅變動,則反映來自較遠之源區。是否有來自濁水溪流域或潭周邊的污染源,未來也值得探討。此外,本次計畫成果發現1999年集集地震與掠過中部颱風帶來驚人雨量對地表的破壞,也顯著反映在底泥淤積上,因此水庫淤積量是未來另一個值得注意的問題。
中文關鍵字 日月潭、底泥、震測、重金屬、定年

基本資訊

專案計畫編號 EPA-104-GA13-03-A299 經費年度 104 計畫經費 3111.631 千元
專案開始日期 2015/11/30 專案結束日期 2016/09/29 專案主持人 李德貴
主辦單位 土污基管會 承辦人 鄭仲庭 執行單位 社團法人中華民國地質學會

成果下載

類型 檔名 檔案大小 說明
期末報告 日月潭結案報告(定稿)OK.pdf 18MB

The demonstrative project of investigating and analyzing the mud core in Sun-Moon Lake

英文摘要 This project completed first the works of sonar seismic scan before coring. Then two sites were chosen for getting cores in Sun-Moon Lake based on the seismic results, and 5 sediment cores which have a total recovered length over 825 cm have succeeded to be taken in accordance with the project’s objects. After, sediment descriptions, photos, non-destructive analysis of Multi-Sensor Core Logging, Color Reflectance Spectrum and X-ray Fluorescence scanning were carried out for each core. Besides, 55 samples were chosen for radioactive age dating according to the EPA's demand. The obtained results including radioactive age dating pointed out that all the cores cover the age interval from present back to older than AD 1934 which the dam began to be constructed. Age dating results also indicate that the sediments from Sun Lake provide better age controlled data than that of the Moon Lake. The estimated sedimentation rate showed that the site Sun 2 was three times faster than that of the site Moon 1. The result reveals that the main sediment transportation path is from northeastern side of Sun Lake toward the Moon Lake. Physical property parameters, such as the -ray density, porosity, magnetic susceptibility etc., all show very different patterns before and after the dam construction. The trend reflects that the organic material content in the lake sediments dramatically decreased after the reservoir running. Results of X-ray Fluorescence scanning present that the variations in composition of heavy elements may be also due to sediment source changes. High Ni content before AD 1934 may represent the sediment source from the in-situ basin. Thus, the contents of Pb, Zn, Cr increased and the content of Ca started rising and fluctuating after the dam been constructed might conduct the sediment source from faraway after AD 1934. Increasing Pb, Zn, Cr and Ca may imply the pollutions derived from Zhuoshui River or surrounding area, which is worth to be paid attention on it in the future. Besides, extra high sedimentation rate found in our cores most recently may be due to the destructions of 1999 Chi-Chi earthquake and much heavy rainfall brought by several later typhoons passed through. Therefore, the rapid sediment accumulation in the reservoir may be another important issue to be paid attention on.
英文關鍵字 Sun-Moon Lake, sediment, seismic, heavy element, dating