3,491 research outputs found

    SOIL MOISTURE AT PERMANENT WILTING OF PLANTS

    Full text link

    Place-Based Engagement on Chicago\u27s Northeast Side

    Get PDF
    Loyola University Chicago (LUC) is a Jesuit university with a mission to prepare students to “set the world on fire” by promoting justice in the world. Led by its School of Education, LUC has worked to engage this mission in its emerging work with public school partners guided by core principles of mutual benefit among partners, place-based engagement within our communities, and a focus on sustainable relationships. While serving others represents the genotype of our 150-year-old Jesuit university and community and civic engagement represents its phenotype, the last ten years has seen change in the university’s phenotype through dramatic growth in both the strategic approach of its place-based engagement commitments and its direct work among multiple community schools. In 2011, the School of Education engineered a radical overhaul of its teacher preparation program moving from a traditional approach to teacher education that was campus- and text-based to a field-based apprenticeship model (Heineke & Ryan, 2018). To achieve this ambitious project, the School of Education generated and solidified relationships with 20-25 core school partners where field-based learning could take place. Transformation of the teacher preparation program coincided with a comprehensive school-university partnership at a neighborhood-based public high school that currently features more than 20 academic initiatives. In 2016, LUC introduced Schools 2020 to build on this success with five additional public schools. In 2018, LUC began to serve as the Lead Partner Agency (LPA) at six Chicago Public Schools (CPS) Community School Initiatives (CSI) sites. Currently more than 1000 students are served through out-of-school (OST) programs while 100 part-time instructors (LUC faculty and students, school teachers, and community organization staff ) work with students through more than 100 unique program activities. More than $4 million in CPS-CSI funding has been secured through 2024 to support this work. In this article, we seek to present the historical context in which our university-school partnership emerged and has developed, our approaches to and examples of the work, discuss challenges that have surfaced in the work and, finally, describe horizon opportunities for LUC. We argue here for a place-based, mutually beneficial approach to university-school partnerships that places relationships at the center of the work in order to achieve sustainability over time. We believe that relationships based in trust and mutuality throughout and across our institutions lead to powerful outcomes for faculty, teachers, students, and ultimately communities. We argue here that a focus on relationships can lead to organizational and community transformation in ways that transactional operational systems may not

    Water Use Efficiency by Switchgrass Compared to a Native Grass or a Native Grass Alfalfa Mixture

    Get PDF
    Perennial grass systems are being evaluated as a bioenergy feedstock in the northern Great Plains. Inter-annual and inter-seasonal precipitation variation in this region will require efficient water use to maintain sufficient yield production to support a mature bioenergy industry. Objectives were to evaluate the impact of a May–June (early season) and a July–August (late season) drought on the water use efficiency (WUE), amount of water used, and biomass production in monocultures of switchgrass (Panicum virgatum L.), western wheatgrass (Pascopyrum smithii (Rydb.) Á. Löve), and a western wheatgrass–alfalfa (Medicago sativa L.) mixture using an automated rainout shelter. WUE was strongly driven by biomass accumulation and ranged from 5.6 to 7.4 g biomass mm−1 water for switchgrass to 1.06 to 2.07 g biomass mm−1 water used with western wheatgrass. Timing of water stress affected WUE more in western wheatgrass and the western wheatgrass–alfalfa mixture than switchgrass. Water deficit for the western wheatgrass–alfalfa mixture was 23 % lower than western wheatgrass (P=0.0045) and 31 % lower than switchgrass (P\u3c0.0001) under the May–June stress water treatment, while switchgrass had a 37 and 38%greater water deficit than did western wheatgrass or western wheatgrass–alfalfa mixture, respectively (P\u3c0.001) under the July–August water stress treatment. Water depletion was always greatest in the upper 30 cm. Switchgrass had greater WUE but resulted in greater soil water depletion at the end of the growing season compared to western wheatgrass and a western wheatgrass– alfalfa mixture which may be a concern under multi-year drought conditions

    Dip coating process: Silicon sheet growth development for the large-area silicon sheet task of the low-cost silicon solar array project

    Get PDF
    To date, an experimental dip-coating facility was constructed. Using this facility, relatively thin (1 mm) mullite and alumina substrates were successfully dip-coated with 2.5 - 3.0 ohm-cm, p-type silicon with areas of approximately 20 sq cm. The thickness and grain size of these coatings are influenced by the temperature of the melt and the rate at which the substrate is pulled from the melt. One mullite substrate had dendrite-like crystallites of the order of 1 mm wide and 1 to 2 cm long. Their axes were aligned along the direction of pulling. A large variety of substrate materials were purchased or developed enabling the program to commence a substrate definition evaluation. Due to the insulating nature of the substrate, the bottom layer of the p-n junction may have to be made via the top surface. The feasibility of accomplishing this was demonstrated using single crystal wafers

    Hydrology, Water Chemistry and Ecological Relations in the Raised Mound of Cowles Bog

    Get PDF
    The Cowles Bog National Natural Landmark and the wetlands between the dunes near the south shore of Lake Michigan, in Indiana, contain plant species that are typical of circum-neutral fens. The distribution of eight, rather sharply delineated, vegetation types correlates most strongly with water level variations resulting from the presence of a 4.1-ha convex peat mound. A network of shallow ground-water wells installed in the wetland has identified an upwelling of water under artesian pressure at sites underlying the mound. The well-buffered water, containing high concentrations of inorganic solutes, is derived from an aquifer that is recharged on an upland moraine and is confined beneath a clay till sheet. A breach in this clay layer beneath the mound allows water to flow upward and radially outward as the hydraulic head is dissipated in the overlying marl and peat. The marl and organic lake sediments in the wetland were formed during the Nipissing level of ancestral Lake Michigan (4000-6000 years ago) when the wetland basin was probably a small bay of the lake. The peat mound developed when the lake level fell from the Algoma through to modern times. This increased the difference in hydraulic head and increased spring flows, which in turn induced peat formation
    • 

    corecore