British Methodist Episcopal Church Tithing Ticket, 1879

A first quarterly tithing ticket from the British Methodist Episcopal Church, signed by W. Grayson, Minister, and dated August 1, 1879. This ticket was in the possession of the Rick Bell Family of St. Catharines, Ontario. Relatives of the Bell family include former Black slaves from the United States who settled in Canada.

British Methodist Episcopal Church Tithing Ticket, 1884

A third quarterly tithing ticket from the British Methodist Episcopal Church, signed by the Minister, and dated February 17, 1884. This ticket was in the possession of the Rick Bell family of St. Catharines, Ontario. Relatives of the Bell family include former Black slaves from the United States who settled in Canada.

British Methodist Episcopal Church Tithing Ticket, 1889

A second quarterly tithing ticket from the British Methodist Episcopal Church, signed by Rev. P. Brooks, Minister, issued on November 24, 1889. This ticket was in the possession of the Richard Bell family of St. Catharines, Ontario. The Bell family ancestry includes former Black American slaves who settled in Canada.

St. Catharines documents including mortgages, wills and declarations, 1871-1914 (not inclusive)

Most of these documents refer to a tract of land located on the intersection of King and Court Streets (part of the Lawrie plan) and Carter properties in St. Catharines Ontario. The Security Loan and Savings Company of St. Catharines existed between 1870 and 1906. Thomas Rodman Merritt was the president.

Photograph of St. Catharines Collegiate Institute students, October 20, 1925

The origins of the St. Catharines Collegiate Institute can be traced back to the formation of the Grantham Academy on Church St. in 1829. In 1845, the name was changed to the St. Catharines District Grammar School and in 1890 the Grammar School was renamed the St. Catharines Collegiate Institute. The current site of the school on Catherine Street was built in 1923 to accommodate the increasing demand for technical education, and became known as the St. Catharines Collegiate Institute and Vocational School. The school was enlarged with additions in 1945, 1965 and 1969. In 2006, the school underwent major renovations, which were completed in 2008. It is currently a secondary school administered by the District School Board of Niagara.

St. Catharines Collegiate Institute Entrance Examination Letter

A letter from the principal of St. Catharines Collegiate Institute, A. E. Coombs, notifying the mother of Helen Smith of her examination results. Helen received honours for her entrance examination mark and the letter reads as follows: "Dear Helen, I am glad to be able to inform you that Helen Smith of 39 Church St. obtained Honours at the entrance examination with a total of 517 marks out of 650. The less fortunate H. Smith was Howard Smith of 122 Queenston St, whose name appears in the pass list. Yours truly A.E. Coombs"

Letter to S. D. Woodruff regarding Church Pew

Letter to S.D. Woodruff regarding the pew formerly occupied by Mrs. Helliwell which will be rented after July 1st and “you will be relieved of your rent as requested”. This is signed by P. H. Guiton, church warden, July 5, 1881.

Physik lernen, um Physik zu lehren

Aus mehreren Untersuchungen zum Interesse der Schülerinnen und Schüler am Physikunterricht ist bekannt, dass der Unterricht dann für sie interessant ist, wenn die fachlichen Inhalte in einen für die Schülerinnen und Schüler relevanten Kontext eingebunden sind. Die vorliegende empirische Untersuchung beschäftigt sich mit dem Kontext „Physik lernen durch lehren“. Bei diesem Kontext sollen Schülerinnen und Schüler des Gymnasiums Physik lernen, um anschließend Kindern in der Vor- und Grundschule selbst naturwissenschaftliche Inhalte zu vermitteln. Der Kontext wurde dahingehend untersucht, inwiefern er das situationale Interesse der Schülerinnen und Schüler am Physikunterricht beeinflusst und welchen Einfluss er auf die Vermittlung fachlicher und überfachlicher Kompetenzen hat. Die Arbeit basiert auf der Selbstbestimmungstheorie der Motivation von Deci u. Ryan (1993) sowie der pädagogischen Interessentheorie von Krapp u. Prenzel (1992). Um die Interessantheit des Unterrichts im Kontext und den Erwerb von Kompetenzen festzustellen, wurden im Rahmen der Untersuchung zwei quantitative Studien mittels Fragebogenerhebungen und eine qualitative Studie in Form von Leitfaden-Interviews sowohl mit Schülerinnen und Schülern als auch mit Lehrkräften durchgeführt. Die Ergebnisse der Untersuchung zeigen, dass der Unterricht im Kontext „Physik lernen durch lehren“ hinsichtlich der Interessantheit deutlich den herkömmlichen Zugängen überlegen ist. In der Untersuchung wurde eine Reihe von potenziellen Einflussvariablen auf die festgestellte Interessantheit am Unterricht in dem zu unter-suchenden Kontext ermittelt. Der Unterricht wurde in erster Linie aufgrund der naturwissenschaftlichen Veranstaltungen mit den Vor- und Grundschulkindern für die Schülerinnen und Schüler interessanter. Es wurde festgestellt, dass der Kontext besonders bei Schülerinnen und Schülern, die am Unterrichtsfach Physik allgemein unterdurchschnittlich interessiert sind, auf ein größeres situationales Interesse st��ßt. Insbesondere Mädchen zeigen ein großes situationales Interesse an dem Kontext. Bei dem kontextorientierten Unterricht werden neben fachlichen Kompetenzen vor allem überfachliche Kompetenzen bei den Schülerinnen und Schülern gefördert. Der Schwerpunkt bei den fachlichen Kompetenzen liegt im Bereich des Prozesswissens, und bei den überfachlichen Kompetenzen werden primär das methodisch-problemlösende Lernen und das sozial-kommunikative Lernen gefördert.

Evaluation von Schule und Unterricht in historischer Perspektive: Schul- und Unterrichtsinspektionen am Kasseler Gymnasium während der Zeit des Vormärz

Der vorliegenden Aufsatz handelt von einem frühen Beispiel schulischer und unterrichtlicher Evaluation. Im Zuge der Modernisierung des kurhessischen Schulwesens nach 1832 wurde auch das Kasseler Gymnasium einer gründlichen Inspektion unterzogen, die wenig erfreuliche Zust��nde zutage brachte. In der Folge kam es zu einer Reorganisation der Schule und der Berufung eines neuen Schulleiters, dessen Dienstordnung ihn zur halbjährlichen Berichterstattung über "Zustand und Wirksamkeit" seines Gymnasiums verpflichtete. Wie er das Bildungsgeschehen an seiner Schule evaluiert hat und wie sich seine diesbezüglichen Interventionen gestalteten wird am Beispiel des neu eingeführten Unterrichtsfaches 'Gesang' rekonstruiert.

Effects of tillage on processes of organic matter sequestration

To increase the organic matter (OM) content in the soil is one main goal in arable soil management. The adoption of tillage systems with reduced tillage depth and/or frequency (reduced tillage) or of no-tillage was found to increase the concentration of soil OM compared to conventional tillage (CT; ploughing to 20-30 cm). However, the underlying processes are not yet clear and are discussed contradictorily. So far, few investigations were conducted on tillage systems with a shallow tillage depth (minimum tillage = MT; maximum tillage depth of 10 cm). A better understanding of the interactions between MT implementation and changes in OM transformation in soils is essential in order to evaluate the possible contribution of MT to a sustainable management of arable soils. The objectives of the present thesis were (i) to compare OM concentrations, microbial biomass, water-stable aggregates, and particulate OM (POM) between CT and MT soils, (ii) to estimate the temporal variability of water-stable aggregate size classes occurring in the field and the dynamics of macroaggregate (>250 µm) formation and disruption under controlled conditions, (iii) to investigate whether a lower disruption or a higher formation rate accounts for a higher occurrence of macroaggregates under MT compared to CT, (iv) to determine which fraction is the major agent for storing the surplus of OM found under MT compared to CT, and (v) to observe the early OM transformation after residue incorporation in different tillage systems simulated. Two experimental sites (Garte-Süd and Hohes Feld) near Göttingen, Germany, were investigated. Soil type of both sites was a Haplic Luvisol. Since about 40 years, both sites receive MT by a rotary harrow (to 5-8 cm depth) and CT by a plough (to 25 cm depth). Surface soils (0-5 cm) and subsoils (10-20 cm) of two sampling dates (after fallow and directly after tillage) were investigated for concentrations of organic C (Corg) and total N (N), different water-stable aggregate size classes, different density fractions (for the sampling date after fallow only), microbial biomass, and for biochemically stabilized Corg and N (by acid hydrolysis; for the sampling date after tillage only). In addition, two laboratory incubations were performed under controlled conditions: Firstly, MT and CT soils were incubated (28 days at 22°C) as bulk soil and with destroyed macroaggregates in order to estimate the importance of macroaggregates for the physical protection of the very labile OM against mineralization. Secondly, in a microcosm experiment simulating MT and CT systems with soil <250 µm and with 15N and 13C labelled maize straw incorporated to different depths, the mineralization, the formation of new macroaggregates, and the partitioning of the recently added C and N were followed (28 days at 15°C). Forty years of MT regime led to higher concentrations of microbial biomass and of Corg and N compared to CT, especially in the surface soil. After fallow and directly after tillage, a higher proportion of water-stable macroaggregates rich in OM was found in the MT (36% and 66%, respectively) than in the CT (19% and 47%, respectively) surface soils of both sites (data shown are of the site Garte-Süd only). The subsoils followed the same trend. For the sampling date after fallow, no differences in the POM fractions were found but there was more OM associated to the mineral fraction detected in the MT soils. A large temporal variability was observed for the abundance of macroaggregates. In the field and in the microcosm simulations, macroaggregates were found to have a higher formation rate after the incorporation of residues under MT than under CT. Thus, the lower occurrence of macroaggregates in CT soils cannot be attributed to a higher disruption but to a lower formation rate. A higher rate of macroaggregate formation in MT soils may be due to (i) the higher concentrated input of residues in the surface soil and/or (ii) a higher abundance of fungal biomass in contrast to CT soils. Overall, as a location of storage of the surplus of OM detected under MT compared to CT, water-stable macroaggregates were found to play a key role. In the incubation experiment, macroaggregates were not found to protect the very labile OM against mineralization. Anyway, the surplus of OM detected after tillage in the MT soil was biochemically degradable. MT simulations in the microcosm experiment showed a lower specific respiration and a less efficient translocation of recently added residues than the CT simulations. Differences in the early processes of OM translocation between CT and MT simulations were attributed to a higher residue to soil ratio and to a higher proportion of fungal biomass in the MT simulations. Overall, MT was found to have several beneficial effects on the soil structure and on the storage of OM, especially in the surface soil. Furthermore, it was concluded that the high concentration of residues in the surface soil of MT may alter the processes of storage and decomposition of OM. In further investigations, especially analysis of the residue-soil-interface and of effects of the depth of residue incorporation should be emphasised. Moreover, further evidence is needed on differences in the microbial community between CT and MT soils.