A Study on Improving a Continuing Education for Public Librarians: Focusing on Privatized Public Libraries
This study aims to make suggestions on how to effectively provide continuing education for librarians in privatized public libraries. For this end, the study examined concepts and importance of continuing education. It then investigated a current status of education/training procedures provided by Librarian Training Division of the National Library of Korea, and continuing education programs for public librarians implemented by primary regional libraries. It also analyzed continuing education programs of library associations in the U.S. and the U.K. Based on these analyses, the study conducted a survey for a sample of librarians in privatized public libraries, identified problems of continuing education for them, and made recommendations for its improvement. 키워드: 위탁공공도서관, 사서, 계속교육, 재교육, 공공도서관 privatized public library, librarian, continuing education, reeducation, public library * ** 이화여자대학교 문헌정보학과 대학원(feelingpj@ewha.ac.kr) (제1저자) 이화여자대학교 문헌정보학과 교수(syly@ewha.ac.kr) (교신저자) 논문접수일자 : 2014년 3월 3일 논문심사일자 : 2014년 3월 3일 게재확정일자 : 2014년 3월 17일 한국비블리아학회지, 25(1): 363-395, 2014. [http://dx.doi.org/10.14699/kbiblia.2014.25.1.363] 364 한국비블리아학회지 제25권 제1호 2014
우리나라 공공도서관 민간위탁의 성과 분석에 관한 연구
본 연구의 목적은 공공도서관의 운영 활성화에 기여하기 위하여 현행 공공도서관의 민간 위탁의 성과를 분석하는 것이다. 성과의 분석 대상으로는 민간 위탁을 실시하고 있는 3개 공공도서관을 선정하여, 문헌연구, 설문 및 방문조사를 수행하였다. 주요한 고찰사항은 첫째. 공공도서관 민간위탁의 필요성과 배경 및 현황의...
Mississippian Barnett Shale: Lithofacies and depositional setting of a deep-water shale-gas succession in the Fort Worth Basin, Texas
The Mississippian Barnett Formation of the Fort Worth Basin is a classic shale-gas system in which the rock is the source, reservoir, and seal. Barnett strata were deposited in a deeper water foreland basin that had poor circulation with the open ocean. For most of the basin's history, bottom waters were euxinic, preserving organic matter and, thus, creating a rich source rock, along with abundant framboidal pyrite. The Barnett interval comprises a variety of facies but is dominated by fine-grained (clay- to silt-size) particles. Three general lithofacies are recognized on the basis of mineralogy, fabric, biota, and texture: (1) laminated siliceous mudstone; (2) laminated argillaceous lime mudstone (marl); and (3) skeletal, argillaceous lime packstone. Each facies contains abundant pyrite and phosphate (apatite), which are especially common at hardgrounds. Carbonate concretions, a product of early diagenesis, are also common. The entire Barnett biota is composed of debris transported to the basin from the shelf or upper oxygenated slope by hemipelagic mud plumes, dilute turbidites, and debris flows. Biogenic sediment was also sourced from the shallower, better oxygenated water column. Barnett deposition is estimated to have occurred over a 25-m.y. period, and despite the variations in sublithofacies, sedimentation style remained remarkably similar throughout this span of time.