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静岡県ひきこもり支援センターにおいて面接相談を行ったケースの状態変化ついて、静岡式ひきこもり評定尺度を用いて分析を行った。親が相談を行うことによって、親が当初抱いていた不安や焦りが和らぎ、本人との間の緊張が軽減し、本人にも良い変化が生じていた。本人のひきこもり状態の改善のためには、本人が安心できる環境を家族が整えることが重要であり、そのために支援者は家族が安心感を持てるように支援する必要がある。また、家族間のコミュニケーションが改善することによって、本人に大きな変化が 生じることが示された。この結果はひきこもり支援プログラム「CRAFT」の目指す方向性と一致するものであった。短期間で目に見える変化が生じにくいひきこもり支援においては、親や当事者の小さな変化や改善を可視化することで、長期にわたる支援の動機付けを維持していくことが有効であると 考えられる。, 紀要論文

To assess the influence of the Tsushima Warm Current (TWC) on radiolarian inflow to the Japan Sea, we determined the faunal characteristics and water properties (temperature, salinity, density, and fluorescence intensity) of surface-subsurface waters shallower than 100m depthe in the Japan Sea off Tassha, Sado Island, central Japan on June 4, 2007. Compared with the water properties measured in June 2005, a thick temperature-stratified layer of 16.0-16.6℃ was recorded in water shallower than 32m in June 2007, indicating that the flow force of the TWC had increased in June 2007 relative to that in 2005. This finding is independently supported by broad-based hydrographic data from the Japan Sea. Although the standing stock is very low, the radiolarian fauna consists of typical cold-water dwellers (Larcopyle butschlii, Cyrtidosphaera reticulata, Spongotrochus glacialis) throughout waters shallower than 100m depth, along with a warm-water species (Spongosphaera streptacantha) that usually occurs in summer around Sado Island. Based on the compiled radiolarian faunal and temperature data, S. streptacantha can be considered a typical inflowing species transported by the TWC.

The vertical distribution of radiolarian faunas on September 28, 2005 and the temperature, salinity, density, and fluorescence intensity profiles are documented from surface and subsurface waters (> 100m deep) in the Japan Sea, off Tassha, Sado City, Sado Island, Niigata Prefecture, central Japan. The features of the water mass structure shallower than 100m deep are distinguished by gentle gradients of temperature and salinity in waters between 100m and 20m deep (the lower layer: LL) and a homogeneous temperature and salinity (24.0℃, 32.9psu) in waters shallower than 20m (the upper layer: UL). The species composition of the deeper fauna (ca. 77-54m) is characterized by the abundant occurrence of Acanthosphaera actinota, Pseudocubus sp. A, Lophospyris sp., and Acanthodesmia sp. It is also noteworthy that each species in the deeper water fauna does not exceed 20％. In the shallower fauna (ca. 35-0m), Spongosphaera streptacantha, Pseudocubus obeliscus, and Pseudocubus sp. A comprise 87.5％ of the fauna. Considering the characteristics of vertical water properties, high standing stocks of these three species are likely caused by their temperature preferences and adaptive strategies for a summer environment in the Japan Sea. There is a slight difference in species composition between September faunas of 2000 and 2005 which is probably related to the Tsushima Warm Current (TWC). It is known that the flow force of the TWC varies in 2 to 3- and 10-year cycles, so the TWC fluctuation may influence the annual variation of the fauna around Sado Island.