Seizure
发表于 2025-3-25 07:17:14
Stress, Coping and Personality,o be anything other than superficial. How we perceive pressures, what coping responses we use and what support systems apply will depend, to a large extent, on personality factors. This chapter will therefore explore the issues of personality that can be seen to play a part in the management of pressure and stress.
难理解
发表于 2025-3-25 09:20:52
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他一致
发表于 2025-3-25 15:19:52
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无政府主义者
发表于 2025-3-25 19:51:30
Sources of Stress,to appreciate the subtle and complex factors which lead to certain aspects of personal or work experience being, in some way, distressing or detrimental to one’s well-being. It is therefore necessary to preface a discussion of social work stressors with a brief outline of a theoretical model which h
affinity
发表于 2025-3-25 22:16:33
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ANTI
发表于 2025-3-26 04:12:06
The Social Work Task,related to the ways in which social work agencies are organised and managed — the factors that can be improved if the political will to bring about change exists or can be generated. The focus of this chapter, by contrast, is on those aspects of social work that cannot be changed — the factors that
怪物
发表于 2025-3-26 05:05:08
The Organisational Context,n indicator of the ineffectiveness of work environments, systems and practices is necessary’ (pp. 12–13). This is very much in line with the perspective we have adopted here, based on the view that stress is both an individual problem and an organisational one. Indeed, as our discussions in Chapter
错误
发表于 2025-3-26 10:16:40
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champaign
发表于 2025-3-26 13:39:02
Conclusion,e, the demands upon us complex and often intense. One implication of this is that there is a very strong need for clear and relatively simple guidance as to how to deal with these matters. This chapter, then, plays a dual role. On the one hand, it acts as a traditional final chapter with a focus on
STANT
发表于 2025-3-26 18:37:33
Chemical Oceanography of the Arctic Ocean,ity chemical data and stressed the importance of the use of tracers. Östlund’s measurements of Н bomb-produced tritium (HTO) have given us two “snapshots” (1972 and 1981) of how the deep Atlantic water is formed in the Greenland and Norwegian seas and penetrates toward the south Atlantic (Östlund, 1