Background Liquefaction induced land damage has been identified in more than 13 notable New Zealand earthquakes within the past 150 years, as presented on the timeline below. Following the 2010-2011 Canterbury Earthquake Sequence (CES), the consequences of liquefaction were witnessed first-hand in the city of Christchurch and as a result the demand for understanding this phenomenon was heightened. Government, local councils, insurers and many other stakeholders are now looking to research and understand their exposure to this natural hazard.
What does it mean to “be in a mood” at school? This question guides this thesis, which analyses the relationship between young people’s experiences of moods and the discourses and pedagogies of moods they encounter at school. The emotions and moods of young people in Christchurch, New Zealand, have, in recent years, come under considerable scrutiny. A national decline in rates of youth mental health and concern over the lasting psychological effects of the 2010-2011 Christchurch Earthquakes have justified increased attention to and funding for youth mental health promotion and school-based mental health education programs. Drawing on a year-long school ethnography at a public girl’s high school in Christchurch with 22 Year 10 students (age 14-15), this thesis examines how young people interact with state and psychiatric discourses of youth and mental health. It explores how young people integrate and transform these discourses in their experiences and knowledges of moods as they relate to mental health, education, friendships, and the (in)stability of the self in time. Additionally, this thesis proposes an anthropological reconsideration of moods. Developing insights from phenomenological and medical anthropology and bringing them into conversation with ethnographic analysis, the approach to moods in this thesis sees two necessarily interconnected ways in which moods become significant for understanding subjectivity and contemporary society. On the one hand, moods are an integral dimension of phenomenological experience in which it is possible to dwell in affective ambiguities, producing open-ended horizons of experience. On the other hand, young people’s experience of moods is refracted through moods’ medicalised formulation as experience that can be bounded, taxonomized, transformed into kinds of knowledge about the self, and thus acted on in distinct and morally situated ways. Attending to the experience of “being in a mood” at school reveals how medical and psychiatric knowledges are woven into moral experience in the everyday. This moral experience of moods has critical implications for how young people in New Zealand today situate the self in relationships, in the world, and in time, and therefore is particularly revealing for developing anthropological understandings of teenage subjectivity
The Canterbury Earthquake Sequence 2010-2011 (CES) induced widespread liquefaction in many parts of Christchurch city. Liquefaction was more commonly observed in the eastern suburbs and along the Avon River where the soils were characterised by thick sandy deposits with a shallow water table. On the other hand, suburbs to the north, west and south of the CBD (e.g. Riccarton, Papanui) exhibited less severe to no liquefaction. These soils were more commonly characterised by inter-layered liquefiable and non-liquefiable deposits. As part of a related large-scale study of the performance of Christchurch soils during the CES, detailed borehole data including CPT, Vs and Vp have been collected for 55 sites in Christchurch. For this subset of Christchurch sites, predictions of liquefaction triggering using the simplified method (Boulanger & Idriss, 2014) indicated that liquefaction was over-predicted for 94% of sites that did not manifest liquefaction during the CES, and under-predicted for 50% of sites that did manifest liquefaction. The focus of this study was to investigate these discrepancies between prediction and observation. To assess if these discrepancies were due to soil-layer interaction and to determine the effect that soil stratification has on the develop-ment of liquefaction and the system response of soil deposits.
