コウレイシャ シセツ ニオケル カイゴ サービス ギョウム ブンセキ ト ボランティア マネジメント ノ カノウセイ

The purpose of this study is to search for the possibility of volunteer management in a nursing home for elderly. The data was collected by questionnaire from 388 staff in 15 nursing homes for elderly. The nursing care service is classified 80 items into nine clusters by cluster analysis using four indexes of relation, difficulty, necessity and professional. Nine clusters emerged as follows: （1） non-care service, （2） spot care service, （3） care connective service, （4） care cooperative service, （5） based care service, （6） advanced care service, （7） core care service, （8） domestic care service, and （9） leisure care service. Leisure care service is characterized by high degree of relation, low degree of difficulty, high degree of necessity, and low degree of professional. Domestic service of care is characterized by low degree of difficulty and high degree of necessity. Leisure and domestic care service seems to be effective to practice volunteer management in a nursing home for elderly

トクベツ ヨウゴ ロウジン ホーム ニ オケル カイゴ ショクイン ノ リショク ト ショクバ カンキョウ ニ カンスル イチコウサツ

The purpose of this study is to search for the relation of care staff turnover rate and work environment in special nursing homes for the elderly. The candidate for analysis is the special elderly nursing home in Aichi Prefecture. This study analyzed the care worker rate and the years of service, qualified care worker rate, the location of institution, the management years as an index of workplace environment. As a result of analysis, the care staff turnover rate, and was seen the tendency of negative correlation to years of service and qualified care worker rate. It turned out that the location of institution and management years were connected with the care staff turnover rate. It was a center that many of existing researches explore the factor of an individual level to retirement of the care staff. This research was able to suggest that the factor of an organization level had influenced care staff turnover

Report on DELP 1989 Cruise in the TTT Junction Areas : Part 2: Upper Crustal Structure Near the Trench-Trench-Trench Triple Junction off the Boso Peninsula, Japan

In July 1989 twenty-two ocean bottom seismographs (OBSs) from 5 Japanese institutions were deployed in an array on the deep sea floor in the vicinity of the trench-trench-trench triple junction off the Boso Peninsula, Japan. The array is 300 km long and 80 km wide, including 3 profiles for study of crustal structure. A permanent OBS array telemetered by a cable system (Japan Meteorological Agency) was used as a part of the array. The sea floor array was complemented by five temporary land stations on the Boso Peninsula. Water depth along the seismic profile varies considerably from a few 100 m to 9000 m or more. We placed three OBSs specially designed for the very deep ocean. We conducted airgun-OBS profiling for the refraction survey. Two 16-liter airguns were fired every 40-50s spaced about 100m apart. Airgun signals were observed as far as 30-40 km from the OBS. To obtain the sedimentary and shallow crustal structure we transformed seismograms of airgun shots into the intercept time (τ)-ray parameter (p) domain and inverted them in a P-wave speed structure with depth by the τ-sum inversion method. We derived one-dimensional models for all OBSs. Both the sedimentary thickness and the P-wave speed in the sedimentary layer change along the profiles. The difference in sedimentary structure between the oceanic side of the trench axis and the continental side is evident: the sediment on the pacific plate consists of a vertically homogeneous unconsolidated layer (0.32 s-1 of vertical wave speed gradient) and a consolidated layer with a large gradient of 4.8s-1, while on the Northeast Japan plate the gradient is 0.65s-1 in the topmost and 0.8s-1 in the lower part of the sediment.1989年,房総沖海溝三重会合点付近において,上部地殻を精密に求めるため,エアガン-海底地震計(OBS)を用いた地震波探査が行われた. 22台のOBSを設置して,更に,気象庁の常時観測システムのOBS4台とあわせて,計26台でアレイ観測を行った.このうち3台は, 7000mを超える深海に設置された.長さ300km,巾80kmの調査海域に, 3本のエアガンの測線(全長450km)を設けた.東西に引かれた測線では,水深が数100mから9000mまで変化している.同時に,房総半島においても臨時観測点を5箇所設けた

1989年度DELP海溝三重会合点海域調査研究航海報告 : 第2部:房総沖海溝三重会合点付近の上部地殻構造

In July 1989 twenty-two ocean bottom seismographs (OBSs) from 5 Japanese institutions were deployed in an array on the deep sea floor in the vicinity of the trench-trench-trench triple junction off the Boso Peninsula, Japan. The array is 300 km long and 80 km wide, including 3 profiles for study of crustal structure. A permanent OBS array telemetered by a cable system (Japan Meteorological Agency) was used as a part of the array. The sea floor array was complemented by five temporary land stations on the Boso Peninsula. Water depth along the seismic profile varies considerably from a few 100 m to 9000 m or more. We placed three OBSs specially designed for the very deep ocean. We conducted airgun-OBS profiling for the refraction survey. Two 16-liter airguns were fired every 40-50s spaced about 100m apart. Airgun signals were observed as far as 30-40 km from the OBS. To obtain the sedimentary and shallow crustal structure we transformed seismograms of airgun shots into the intercept time (τ)-ray parameter (p) domain and inverted them in a P-wave speed structure with depth by the τ-sum inversion method. We derived one-dimensional models for all OBSs. Both the sedimentary thickness and the P-wave speed in the sedimentary layer change along the profiles. The difference in sedimentary structure between the oceanic side of the trench axis and the continental side is evident: the sediment on the pacific plate consists of a vertically homogeneous unconsolidated layer (0.32 s-1 of vertical wave speed gradient) and a consolidated layer with a large gradient of 4.8s-1, while on the Northeast Japan plate the gradient is 0.65s-1 in the topmost and 0.8s-1 in the lower part of the sediment.1989年,房総沖海溝三重会合点付近において,上部地殻を精密に求めるため,エアガン-海底地震計(OBS)を用いた地震波探査が行われた. 22台のOBSを設置して,更に,気象庁の常時観測システムのOBS4台とあわせて,計26台でアレイ観測を行った.このうち3台は, 7000mを超える深海に設置された.長さ300km,巾80kmの調査海域に, 3本のエアガンの測線(全長450km)を設けた.東西に引かれた測線では,水深が数100mから9000mまで変化している.同時に,房総半島においても臨時観測点を5箇所設けた