http://chineseinput.net/에서 pinyin(병음)방식으로 중국어를 변환할 수 있습니다.
변환된 중국어를 복사하여 사용하시면 됩니다.
- 中文 을 입력하시려면 zhongwen을 입력하시고 space를누르시면됩니다.
- 北京 을 입력하시려면 beijing을 입력하시고 space를 누르시면 됩니다.
RISS 인기검색어
- 검색키워드
- 저자 : 이진용 (검색결과 1,698 건)
- 무료
- 기관 내 무료
- 유료
-
-
-
-
Combined performance of pumping and tracer tests: A case study
이진용,김정우,천정용,이명재,이강근 한국지질과학협의회 2003 Geosciences Journal Vol.7 No.3
A combined pumping and tracer test was conductedat a highly fractured aquifer system. The hydrogeologic unitsunderlying the test site are reclamation soil, weathered rock layer,and fractured layer. The fractured layer is the main aquifer forthis site. Prior to pumping and tracer tests, slug tests were con-ducted at four test wells. The test data revealed existence of a lowpermeability zone near wel OB-1. Generally the estimated hydraulicconductivities are in the order of 10-4 cm/sec. A pumping test witha discharge rate of 57 m3/d was performed for 1,230 min. Thepumping test data analysis yielded coherent hydraulic conductiv-ity values with those of the slug tests. However, the separate analysisfor each monitoring wel based on conventional analytical solutionswith highly strict boundary conditions and homogeneity assump-tion cannot efficiently show the potential existence of the low per-meability zone. During the pumping test, when the water levels ofthe pumping and monitoring wells are stabilized, a convergent radialtracer test was conducted. From the observed tracer concentration,a longitudinal dispersivity of 0.3 m was obtained, which is wel con-sistent with the values in the prominent literature considering thetest scale. This study excellently demonstrated a method complet-ing a combined pumping and tracer test at one time. A combined pumping and tracer test was conducted at a highly fractured aquifer system. The hydrogeologic units underlying the test site are reclamation soil, weathered rock layer, and fractured layer. The fractured layer is the main aquifer for this site. Prior to pumping and tracer tests, slug tests were conducted at four test wells. The test data revealed existence of a low permeability zone near well OB-1. Generally the estimated hydraulic conductivities are in the order of 10-4 cm/sec. A pumping test with a discharge rate of 57 m3/d was performed for 1,230 min. The pumping test data analysis yielded coherent hydraulic conductivity values with those of the slug tests. However, the separate analysis for each monitoring well based on conventional analytical solutions with highly strict boundary conditions and homogeneity assumption cannot efficiently show the potential existence of the low permeability zone. During the pumping test, when the water levels of the pumping and monitoring wells are stabilized, a convergent radial tracer test was conducted. From the observed tracer concentration, a longitudinal dispersivity of 0.3 m was obtained, which is well consistent with the values in the prominent literature considering the test scale. This study excellently demonstrated a method completing a combined pumping and tracer test at one time.
-
-
-
-
-
-
RISS연관 검색어 추천
이 검색어로 많이 본 자료
활용도 높은 자료
