• 사회복지연구
• /
• 제44권3호
• /
• pp.177-206
• /
• 2013

우리나라는 2004년부터 정부의 재정지원 일자리사업의 하나로, 노인일자리사업을 시행하고 있다. 그러나 시행된 지 10여년이 되었고, 내년부터 본격적인 확대를 앞두고 있지만, 정책대안과 방향설정에 대한 논의가 부족하다. 이에 본 연구는 문헌연구를 중심으로 OECD 국가의 적극적 노동시장정책, 특히 직접 일자리창출 정책을 살펴보았다. 그 후 OECD 국가의 고령자 고용지원정책을 검토한 후, OECD 국가 가운데 저소득 고령자를 대상으로 고용지원정책을 실시하는 국가를 유형화한 후 이를 토대로 노인일자리사업의 발전방안을 도출하였다. 연구결과 첫째, OECD 국가의 고령자 고용정책은 연금정책을 제외하면, 노동수요 장벽제거 전략(임금보조, 사회보험료 감면 등)의 비중이 높고, 고령근로자의 고용가능성 강화전략은 상대적으로 크게 다뤄지지 않는다. 그나마도 직접 일자리창출정책은 매우 주변적인 정책으로 나타났다. 둘째, 정책목표와 사회경제적 지표를 기준으로 저소득 고령근로자를 위한 고용지원정책을 유형화하면, 저소득 노인지원형, 조기퇴직 완화형, 완전고용 지원형으로 나눌 수 있다. 우리나라는 저소득 노인지원형 가운데 직접 일자리 창출형에 속한다. 노인빈곤율이 높고, 소득보장제도가 발달하지 않아서 직접일자리사업을 수행하는 것으로 보인다. 그러나 노인일자리사업은 직접 일자리창출사업으로서의 속성을 갖추지 못했다. 사회참여와 소득보충이라는 2가지 정책목표를 추진하고 있지만 이에 적합한 체제를 구축하지 못했다. 따라서 정책목표를 더 명확히 하여, 목표달성에 적합한 사업체계를 구축해야 한다. 노인일자리사업이 일자리로서 위상을 견고히 하고자 한다면 노동시장정책 차원에서 수정해야 하고, 현재 2가지 목표를 모두 유지하고자 한다면, 소득보충과 사회참여를 위해 사업을 이원화하는 것도 고려할 필요가 있다. 혹은 미국의 SCSEP처럼 훈련을 통해 보조금을 받지 않는 일자리로 이행하도록 지원하는 고용서비스 훈련체제로 바꾸는 것도 대안이 될 것이다.

• 동굴
• /
• 제68호
• /
• pp.23-73
• /
• 2005

Purpose of study; The purpose of this study is specifically classified as two parts. The one is to attempt the chronological annals of Quaternary topographic surface through the study over the formation process of alluvial surfaces in our country, setting forth the alluvial surfaces lower-parts of Han River area, as the basic deposit, and comparing it to the marginal landform surfaces. The other is to attempt the classification of micro morphology based on the and condition premising the land use as a link for the regional development in the lower-parts of Han river area. Reasons why selected the Lower-parts of Han river area as study objects: 1. The change of river course in this area is very serve both in vertical and horizontal sides. With a situation it is very easy to know about the old geography related to the formation process of topography. 2. The component materials of gravel, sand, silt and clay are deposited in this area. Making it the available data, it is possible to consider about not oかy the formation process of topography but alsoon the development history to some extent. 3. The earthen vessel, a fossil shell fish, bone, cnarcoal and sea-weed are included in the alluvial deposition in this area. These can be also valuable data related to the chronological annals. 4. The bottom set conglometate beds is also included in the alluvial deposits. This can be also valuable data related to the research of geomorphological development. 5. Around of this area the medium landform surface, lower landform surface, pediment and basin, are existed, and these enable the comparison between the erosion surfaces and the alluvial surfaces. Approach : 1. Referring to the change of river beds, I have calculated the vertical and horizontal differences comparing the topographic map published in 1916 with that published in 1966 and through the field work 2. In classifying the landform, I have applied the method of micro morphological classification in accordance with the synthetic index based upon the land conditions, and furthermore used the classification method comparing the topographic map published in 1916 and in that of 1966. 3. I have accorded this classification with the classification by mapping through appliying the method of classification in the development history for the field work making the component materials as the available data. 4. I have used the component materials, which were picked up form the outcrop of 10 places and bored at 5 places, as the available data. 5. I have referred to Hydrological survey data of the ministry of Construction (since 1916) on the overflow of Han-river, and used geologic map of Seoul metropolitan area. Survey Data, and general map published in 1916 by the Japanese Army Survbey Dept., and map published in 1966 by the Construction Research Laboratory and ROK Army Survey Dept., respectively. Conclusion: 1. Classification of Morphology: I have added the historical consideration for development, making the component materials and fossil as the data, to the typical consideration in accordance with the map of summit level, reliefe and slope distribution. In connection with the erosion surface, I have divided into three classification such as high, medium and low-,level landform surfaces which were classified as high and low level landform surfaces in past. furthermore I have divided the low level landform surface two parts, namely upper-parts(200-300m) and bellow-parts(${\pm}100m$). Accordingly, we can recognize the three-parts of erosion surface including the medium level landform surface (500-600m) in this area. (see table 22). In condition with the alluvial surfaces I have classified as two landform surfaces (old and new) which was regarded as one face in past. Meamwhile, under the premise of land use, the synthetic, micro morphological classification based upon the land condition is as per the draw No. 19-1. This is the quite new method of classification which was at first attempted in this country. 2. I have learned that the change of river was most severe at seeing the river meandering rate from Dangjung-ni to Nanjido. As you seee the table and the vertical and horizontal change of river beds is justly proportionable to the river meandering rate. 3. It can be learned at seeing the analysis of component materials of alluvial deposits that the component from each other by areas, however, in the deposits relationship upper stream, and between upper parts and below parts I couldn't always find out the regular ones. 4. Having earthern vessel, shell bone, fossil charcoal and and seaweeds includen in the component materials such as gravel, clay, sand and silt in Dukso and Songpa deposits area. I have become to attempt the compilation of chronicle as yon see in the table 22. 5. In according to hearing of basemen excavation, the bottom set conglomerate beds of Dukso beds of Dukso-beds is 7m and Songpa-beds is 10m. In according to information of dredger it is approx. 20m in the down stream. 6. Making these two beds as the standard beds, I have compared it to other beds. 7 The coarse sand beds which is covering the clay-beds of Dukso-beds and Nanjidobeds is shown the existence of so-called erosion period which formed the gap among the alluvial deposits of stratum. The former has been proved by the sorting, bedding and roundness which was supplied by the main stream and later by the branch stream, respectively. 8. If the clay-beds of Dukeo-bed and Songpa-bed is called as being transgressive overlap, by the Eustatic movement after glacial age, the bottom set conglomerate beds shall be called as being regressive overlap at the holocene. This has the closest relationship with the basin formation movement of Seoul besides the Eustatic movement. 9. The silt-beds which is the main component of deposits of flood plain, is regarded as being deposited at the Holocene in the comb ceramic and plain pottery ages. This has the closest relationship with the change of river course and river beds.