Experiencing archives at universities : archivists, librarians, understanding, and collaboration

Collaboration is one of the top trends in academic librarianship in the United States as noted by the Association of College and Research Libraries (ACRL), and is likely to be a growing trend in other countries as well (Association of College and Research Libraries [ACRL] Research Planning and Review Committee, 2014). While ACRL is focusing on library participation in various initiatives and projects on campus that are external to the library, this trend can be broadened to include the possibility for further collaboration within many academic libraries between the librarians and archivists.

Teacher education for high-poverty schools : keeping the bar high

For some time now, there has been a focus, both in Australia and internationally, on quality teaching as a fundamental component that affects the educational outcomes of all students. The question of how teacher education programs in Australia prepare effective teachers to work across all school settings-including low-SES schools-has been elevated to national prominence by data from the 20 12 Programme for International Student Assessment (PIS A), which revealed a fall in Australian students' world ranking across Mathematics, Reading and Science. Education is commonly acknowledged as a "foundation capability" that improves a person's life chances, including employment prospects, and it is widely understood to be a "route out of disadvantage" (McLachlan, Gilfillan, and Gordon 20 13). The Australian Bureau of Statistics 201 1- 12 data suggest that around 2.6 million (11.8%) Australians currently live under the poverty line (Phillips et a!. 2012, 8). According to the Organisation for Economic Cooperation and Development (OECD), despite the significant effects teachers have on student performance, disadvantaged schools are not always staffed with the highest quality teachers (see Darling-Hammond, 2006).

Teacher education for high poverty schools : the National Exceptional Teachers for Disadvantaged Schools program

A vital element to improve outcomes for disadvantaged students is outstanding teachers. A reality, however, is that teacher graduates in the top quartile of academic scores are far less likely to accept positions in tough urban, regional, rural and remote schools. Further, because high poverty schools can be challenging environments, these teachers are retained for much shorter periods of time. In response to this challenge, the National Exceptional Teachers for Disadvantaged Schools program (NETDS) creates a pathway for the highest quality pre-service teachers to be fully prepared, professionally and personally, for roles within high poverty schools. The program identifies the highest-achieving mainstream preservice teachers in university programs across the country and offers them a specialised curriculum and supported practicum experience in a network of disadvantaged partner schools. By working closely with government, philanthropy and partner schools, the program also works to channel these exceptional pre-service teachers into employment in schools where they will have the greatest impact. Its initial results have been exceptional: over 90% of graduates are now employed as teachers in high poverty schools. This paper will discuss their research on how they are working to build the infrastructure and capacity for research on innovations that prepare teachers for 21st century schools in the Australian context.

Toward a model for predicting magnetic susceptibility of bedrock regolith and soils

One of the Department of Defense's most pressing environmental problems is the efficient detection and identification of unexploded ordnance (UXO). In regions of highly magnetic soils, magnetic and electromagnetic sensors often detect anomalies that are of geologic origin, adding significantly to remediation costs. In order to develop predictive models for magnetic susceptibility, it is crucial to understand modes of formation and the spatial distribution of different iron oxides. Most rock types contain iron and their magnetic susceptibility is determined by the amount and form of iron oxides present. When rocks weather, the amount and form of the oxides change, producing concomitant changes in magnetic susceptibility. The type of iron oxide found in the weathered rock or regolith is a function of the duration and intensity of weathering, as well as the original content of iron in the parent material. The rate of weathering is controlled by rainfall and temperature; thus knowing the climate zone, the amount of iron in the lithology and the age of the surface will help predict the amount and forms of iron oxide. We have compiled analyses of the types, amounts, and magnetic properties of iron oxides from soils over a wide climate range, from semi arid grasslands, to temperate regions, and tropical forests. We find there is a predictable range of iron oxide type and magnetic susceptibility according to the climate zone, the age of the soil and the amount of iron in the unweathered regolith.

Mineralogy and Magnetic Properties of Basaltic Substrate Soils: Kaho'olawe and Big Island, Hawaii

Magnetic behavior of soils can seriously hamper the performance of geophysical sensors. Currently, we have little understanding of the types of minerals responsible for the magnetic behavior, as well as their distribution in space and evolution through time. This study investigated the magnetic characteristics and mineralogy of Fe-rich soils developed on basaltic substrate in Hawaii. We measured the spatial distribution of magnetic susceptibility (χlf) and frequency dependence (χfd%) across three test areas in a well-developed eroded soil on Kaho'olawe and in two young soils on the Big Island of Hawaii. X-ray diffraction spectroscopy, x-ray fluorescence spectroscopy (XFCF), chemical dissolution, thermal analysis, and temperature-dependent magnetic studies were used to characterize soil development and mineralogy for samples from soil pits on Kaho'olawe, surface samples from all three test areas, and unweathered basalt from the Big Island of Hawaii. The measurements show a general increase in magnetic properties with increasing soil development. The XRF Fe data ranged from 13% for fresh basalt and young soils on the Big Island to 58% for material from the B horizon of Kaho'olawe soils. Dithionite-extractable and oxalate-extractable Fe percentages increase with soil development and correlate with χlf-and χfd%, respectively. Results from the temperature-dependent susceptibility measurements show that the high soil magnetic properties observed in geophysical surveys in Kaho'olawe are entirely due to neoformed minerals. The results of our studies have implications for the existing soil survey of Kaho'olawe and help identify methods to characterize magnetic minerals in tropical soils.