1000 resultados para 7137-137
Resumo:
This study investigates the landscape evolution and soil development in the loess area near Regensburg between approximately 6000-2000 yr BP (radiocarbon years), Eastern Bavaria. The focus is on the question how man and climate influenced landscape evolution and what their relative significance was. The theoretical background concerning the factors that controlled prehistoric soil erosion in Middle Europe is summarized with respect to rainfall intensity and distribution, pedogenesis, Pleistocene relief, and prehistoric farming. Colluvial deposits , flood loams, and soils were studied at ten different and representative sites that served as archives of their respective palaeoenvironments. Geomorphological, sedimentological, and pedological methods were applied. According to the findings presented here, there was a high asynchronity of landscape evolution in the investigation area, which was due to prehistoric land-use patterns. Prehistoric land use and settlement caused highly difIerenciated phases of morphodynamic activity and stability in time and space. These are documented at the single catenas ofeach site. In general, Pleistocene relief was substantially lowered. At the same time smaller landforms such as dells and minor asymmetric valleys filled up and strongly transformed. However, there were short phases at many sites, forming short lived linear erosion features ('Runsen'), resulting from exceptional rainfalls. These forms are results of single events without showing regional trends. Generally, the onset of the sedimentation of colluvial deposits took place much earlier (usually 3500 yr BP (radiocarbon) and younger) than the formation of flood loams. Thus, the deposition of flood loams in the Kleine Laaber river valley started mainly as a consequence of iron age farming only at around 2500 yr BP (radiocarbon). A cascade system explains the different ages of colluvial deposits and flood loams: as a result of prehistoric land use, dells and other minor Pleistocene landforms were filled with colluvial sediments. After the filling of these primary sediment traps , eroded material was transported into flood plains, thus forming flood loams. But at the moment we cannot quantify the extent ofprehistoric soil erosion in the investigation area. The three factors that controlled the prehistoric Iandscapc evolution in the Ioess area near Regensburg are as follows: 1. The transformation from a natural to a prehistoric cultural landscape was the most important factor: A landscape with stable relief was changed into a highly morphodynamic one with soil erosion as the dominant process of this change. 2. The sediment traps of the pre-anthropogenic relief determined where the material originated from soil erosion was deposited: either sedimentation took place on the slopes or the filled sediment traps of the slopes rendered flood loam formation possible. Climatic influence of any importance can only be documented as the result of land use in connection with singular and/or statistic events of heavy rainfalls. Without human impact, no significant change in the Holocene landscape would have been possible.
Resumo:
Dermatophytoses are common fungal infections caused by dermatophytes but there are few data about this condition in the childhood. 137 children below the age of 12 and clinically diagnosed as tineas were investigated prospectively at Instituto de Puericultura e Pediatria, Rio de Janeiro, from 1994 to 1999. Hair, skin/nails scraping and pus swabs were collected from lesions and processed for fungus. Male children from 2 to 12 years were mostly affected; tinea capitis (78 cases) mainly caused by Microsporum canis (46 cases) was the most common clinical form. Tinea corporis (43 cases) mainly caused by Trichophyton rubrum (17 cases) accounted for the second most frequent clinical form. Tinea cruris (10 cases) with Trichophyton rubrum (5 cases) as the most common etiologic agent accounted for the third most frequent clinical form. Tinea pedis and tinea unguium were much less frequent (3 cases each). Trichophyton rubrum was the most common etiologic agent isolated in these cases (3 cases).
Resumo:
Utilizou-se o césio-137 para avaliar as taxas de perda ou ganho de solo numa microbacia com diferentes culturas, situada no município de Cambe (PR), a 23º16' Sul e 51º17' Oeste. Foi utilizada uma equação teórica que considera a perda ou ganho de solo num ponto diretamente proporcional à redistribuição de césio-137. Uma amostragem em transectos foi efetuada com o objetivo de avaliar a redistribuição de solo dentro da microbacia. Um ponto em mata nativa na microbacia foi amostrado para estimar a quantidade de césio-137 depositado na região pela precipitação radioativa. Os pontos amostrados em área de pastagem apresentaram, em sua maioria, perda de solo. Os pontos amostrados em área de cafeeiro não apresentaram perda nem ganho de solo. Os pontos amostrados em área de soja, em sistema convencional de preparo de solo, apresentaram perda de solo.
Resumo:
Bureau of Nutrition and Health Promotion part of the Iowa Department of Public Health produces of weekly newsletter about the Iowa WIC Program for the State of Iowa citizen.
Resumo:
A liberação de cultivares de elevado potencial produtivo e com resistência a doenças é fundamental para continuar agregando rendimento na produção brasileira de soja. A cultivar BRS 137 é resultado do programa de melhoramento de soja desenvolvido pela Embrapa. A cultivar apresentou rendimento médio de grãos 2% superior ao da cultivar IAS 5, em 24 ambientes, no Rio Grande do Sul. É resistente à pústula-bacteriana (Xanthomonas axonopodis pv. glycines), ao cancro-da-haste (Diaporthe phaseolorum f. sp. meridionalis), à podridão-parda-da-haste (Phialophora gregata), à mancha-olho-de-rã (Cercospora sojina) e ao oídio (Microsphaera diffusa). É indicada para cultivo no Rio Grande do Sul, em semeaduras realizadas a partir de meados de outubro até fim de novembro, com população máxima de 300.000 plantas/ha.
Resumo:
General equations are presented for predicting loss of prestress and camber of both composite and non- composite prestressed concrete structures. Continuous time functins of all parameters needed to solve the equations are given, and sample results included. Computed prestress loss and camber are compared with experimental data for normal weight and lightweight concrete. Methods are also presented for predicting the effect of non-prestressed tension steel in reducing time-dependent loss of prestress and camber, and for the determination of short-time deflections of uncracked and cracked prestressed members. Comparisons with experimental results are indicated for these partially prestressed methods.
Resumo:
Soitinnus: Viulu, piano.