Simulating SOC changes in 11 land use change chronosequences from the Brazilian Amazon with RothC and Century models

Land use and land cover changes in the Brazilian Amazon have major implications for regional and global carbon (C) cycling. Cattle pasture represents the largest single use (about 70%) of this once-forested land in most of the region. The main objective of this study was to evaluate the accuracy of the RothC and Century models at estimating soil organic C (SOC) changes under forest-to-pasture conditions in the Brazilian Amazon. We used data from 11 site-specific 'forest to pasture' chronosequences with the Century Ecosystem Model (Century 4.0) and the Rothamsted C Model (RothC 26.3). The models predicted that forest clearance and conversion to well managed pasture would cause an initial decline in soil C stocks (0-20 cm depth), followed in the majority of cases by a slow rise to levels exceeding those under native forest. One exception to this pattern was a chronosequence in Suia-Missu, which is under degraded pasture. In three other chronosequences the recovery of soil C under pasture appeared to be only to about the same level as under the previous forest. Statistical tests were applied to determine levels of agreement between simulated SOC stocks and observed stocks for all the sites within the 11 chronosequences. The models also provided reasonable estimates (coefficient of correlation = 0.8) of the microbial biomass C in the 0-10 cm soil layer for three chronosequences, when compared with available measured data. The Century model adequately predicted the magnitude and the overall trend in delta C-13 for the six chronosequences where measured 813 C data were available. This study gave independent tests of model performance, as no adjustments were made to the models to generate outputs. Our results suggest that modelling techniques can be successfully used for monitoring soil C stocks and changes, allowing both the identification of current patterns in the soil and the projection of future conditions. Results were used and discussed not only to evaluate soil C dynamics but also to indicate soil C sequestration opportunities for the Brazilian Amazon region. Moreover, modelling studies in these 'forest to pasture' systems have important applications, for example, the calculation of CO, emissions from land use change in national greenhouse gas inventories. (0 2007 Elsevier B.V. All rights reserved.

Predicted soil organic carbon stocks and changes in the Brazilian Amazon between 2000 and 2030

Currently we have little understanding of the impacts of land use change on soil C stocks in the Brazilian Amazon. Such information is needed to determine impacts'6n the global C cycle and the sustainability of agricultural systems that are replacing native forest. The aim of this study was to predict soil carbon stocks and changes in the Brazilian Amazon during the period between 2000 and 2030, using the GEFSOC soil carbon (C) modelling system. In order to do so, we devised current and future land use scenarios for the Brazilian Amazon, taking into account: (i) deforestation, rates from the past three decades, (ii) census data on land use from 1940 to 2000, including the expansion and intensification of agriculture in the region, (iii) available information on management practices, primarily related to well managed pasture versus degraded pasture and conventional systems versus no-tillage systems for soybean (Glycine max) and (iv) FAO predictions on agricultural land use and land use changes for the years 2015 and 2030. The land use scenarios were integrated with spatially explicit soils data (SOTER database), climate, potential natural vegetation and land management units using the recently developed GEFSOC soil C modelling system. Results are presented in map, table and graph form for the entire Brazilian Amazon for the current situation (1990 and 2000) and the future (2015 and 2030). Results include soil organic C (SOC) stocks and SOC stock change rates estimated by three methods: (i) the Century ecosystem model, (ii) the Rothamsted C model and (iii) the intergovernmental panel on climate change (IPCC) method for assessing soil C at regional scale. In addition, we show estimated values of above and belowground biomass for native vegetation, pasture and soybean. The results on regional SOC stocks compare reasonably well with those based on mapping approaches. The GEFSOC system provided a means of efficiently handling complex interactions among biotic-edapho-climatic conditions (> 363,000 combinations) in a very large area (similar to 500 Mha) such as the Brazilian Amazon. All of the methods used showed a decline in SOC stock for the period studied; Century and RothC simulated values for 2030 being about 7% lower than those in 1990. Values from Century and RothC (30,430 and 25,000 Tg for the 0-20 cm layer for the Brazilian Amazon region were higher than those obtained from the IPCC system (23,400 Tg in the 0-30 cm layer). Finally; our results can help understand the major biogeochemical cycles that influence soil fertility and help devise management strategies that enhance the sustainability of these areas and thus slow further deforestation. (C) 2007 Elsevier B.V. All rights reserved.

Evaluation of two soil carbon models using two Kenyan long term experimental datasets

RothC and Century are two of the most widely used soil organic matter (SOM) models. However there are few examples of specific parameterisation of these models for environmental conditions in East Africa. The aim of this study was therefore, to evaluate the ability of RothC and the Century to estimate changes in soil organic carbon (SOC) resulting from varying land use/management practices for the climate and soil conditions found in Kenya. The study used climate, soils and crop data from a long term experiment (1976-2001) carried out at The Kabete site at The Kenya National Agricultural Research Laboratories (NARL, located in a semi-humid region) and data from a 13 year experiment carried out in Machang'a (Embu District, located in a semi-arid region). The NARL experiment included various fertiliser (0, 60 and 120 kg of N and P2O5 ha(-1)), farmyard manure (FYM - 5 and 10 t ha(-1)) and plant residue treatments, in a variety of combinations. The Machang'a experiment involved a fertiliser (51 kg N ha(-1)) and a FYM (0, 5 and 10 t ha(-1)) treatment with both monocropping and intercropping. At Kabete both models showed a fair to good fit to measured data, although Century simulations for treatments with high levels of FYM were better than those without. At the Machang'a site with monocrops, both models showed a fair to good fit to measured data for all treatments. However, the fit of both models (especially RothC) to measured data for intercropping treatments at Machang'a was much poorer. Further model development for intercrop systems is recommended. Both models can be useful tools in soil C Predictions, provided time series of measured soil C and crop production data are available for validating model performance against local or regional agricultural crops. (C) 2007 Elsevier B.V. All rights reserved.

National and sub-national assessments of soil organic carbon stocks and changes: The GEFSOC modelling system

Soil organic carbon (SOC) plays a vital role in ecosystem function, determining soil fertility, water holding capacity and susceptibility to land degradation. In addition, SOC is related to atmospheric CO, levels with soils having the potential for C release or sequestration, depending on land use, land management and climate. The United Nations Convention on Climate Change and its Kyoto Protocol, and other United Nations Conventions to Combat Desertification and on Biodiversity all recognize the importance of SOC and point to the need for quantification of SOC stocks and changes. An understanding of SOC stocks and changes at the national and regional scale is necessary to further our understanding of the global C cycle, to assess the responses of terrestrial ecosystems to climate change and to aid policy makers in making land use/management decisions. Several studies have considered SOC stocks at the plot scale, but these are site specific and of limited value in making inferences about larger areas. Some studies have used empirical methods to estimate SOC stocks and changes at the regional scale, but such studies are limited in their ability to project future changes, and most have been carried out using temperate data sets. The computational method outlined by the Intergovernmental Panel on Climate Change (IPCC) has been used to estimate SOC stock changes at the regional scale in several studies, including a recent study considering five contrasting eco regions. This 'one step' approach fails to account for the dynamic manner in which SOC changes are likely to occur following changes in land use and land management. A dynamic modelling approach allows estimates to be made in a manner that accounts for the underlying processes leading to SOC change. Ecosystem models, designed for site scale applications can be linked to spatial databases, giving spatially explicit results that allow geographic areas of change in SOC stocks to be identified. Some studies have used variations on this approach to estimate SOC stock changes at the sub-national and national scale for areas of the USA and Europe and at the watershed scale for areas of Mexico and Cuba. However, a need remained for a national and regional scale, spatially explicit system that is generically applicable and can be applied to as wide a range of soil types, climates and land uses as possible. The Global Environment Facility Soil Organic Carbon (GEFSOC) Modelling System was developed in response to this need. The GEFSOC system allows estimates of SOC stocks and changes to be made for diverse conditions, providing essential information for countries wishing to take part in an emerging C market, and bringing us closer to an understanding of the future role of soils in the global C cycle. (C) 2007 Elsevier B.V. All rights reserved.

Frozen tears II

Russell, J. [Ed. & designer]. Including texts by Kathy Acker, Dominique Auch, Dennis Cooper, Trinie Dalton, Sue De Beer, Felix Ensslin, Dan Fox, Matthew Greene, Pierre Guyotat, Rachel Howe, Kevin Killian, Christopher Knowles, Gean Moreno, J.P. Munro, Paulina Olowska, Damon Packard, Allison Smith, Banks Violette, Benjamin Weissman, & Thom Wolf. 832 pages.

A criança disfônica: diagnóstico, tratamento e evolução clínica

Os nódulos vocais são causas freqüentes de disfonias infantis, porém, através das vídeoendoscopias, outras lesões têm sido diagnosticadas na laringe infantil, como os cistos, sulcos, pontes e micromembranas, denominadas de lesões estruturais mínimas. OBJETIVO: Avaliar, em 71 crianças com disfonia agendadas nos ambulatórios de Foniatria da Faculdade de Medicina de Botucatu (Unesp) nos últimos cinco anos: sexo, idade, diagnósticos, tratamentos e evolução clínica. FORMA DE ESTUDO: Clínico retrospectivo. CASUÍSTICA E MÉTODO: Realizou-se estudo retrospectivo das avaliações otorrinolaringológicas e endoscópicas de 71 crianças com queixas de disfonia e idade entre 3 a 13 anos (45 meninos e 26 meninas). As crianças haviam sido submetidas a exame endoscópico com telescópio rígido ou nasofibroscópio flexível. Foram excluídas as crianças com disfonias funcionais ou com queixas de obstrução respiratória. RESULTADOS: Os principais diagnósticos foram: nódulo vocal (47 casos; 66,2%), cisto epidérmico (7 casos; 9,9%), cisto aberto fistulizado (6 casos; 8,4%), sulco vocal (5 casos; 7,1%), ponte + cisto (2 casos; 2,8%), micromembrana anterior (2 casos; 2,8%) e pólipo vocal (2 casos; 2,8%). As disfonias foram mais freqüentes entre os meninos (63,3%). A fonoterapia isolada foi o tratamento de escolha nos casos de nódulo vocal (evolução favorável), sulco vocal (evolução desfavorável) e micro-membrana (evolução desfavorável). Nas demais lesões (cistos, pontes e pólipos) o tratamento de escolha foi a cirurgia associada à fonoterapia, com resultados satisfatórios, exceto nos casos que recusaram a cirurgia. CONCLUSÃO: Os nódulos vocais são as principais causas de disfonias em crianças, porém as lesões estruturais mínimas mostraram-se também freqüentes, exigindo exame minucioso para o diagnóstico.

Correlação ultrassonográfica e histeroscópica no diagnóstico de pólipos endometriais em mulheres na pós-menopausa

Coordenação de Aperfeiçoamento de Pessoal de Nível Superior (CAPES)

Expressão das proteinas p53, Ki67 e CD31 nos pólipos endometriais em mulheres na pós-menopausa usuárias de tamoxifeno

Pós-graduação em Ginecologia, Obstetrícia e Mastologia - FMB

Estudo analítico dos pólipos endometriais: a importância da polipectomia

Pós-graduação em Ginecologia, Obstetrícia e Mastologia - FMB

Histeroscopia ambulatorial com laser diodo: uma nova modalidade para tratamento de pólipos endometriais

Pós-graduação em Ginecologia, Obstetrícia e Mastologia - FMB

Avaliação dos fatores preditivos dos pólipos endometriais em mulheres na pós-menopausa

Pós-graduação em Ginecologia, Obstetrícia e Mastologia - FMB

Inflammatory fibroid polyp (Vanek’s polyp): a case report and literature review

Inflammatory fibroid polyp (IFP) is a benign uncommon lesion (1%-4% of gastric benign lesions), originated from the submucosa of the gastrointestinal tract. Its origin is controversial and immunohistochemical studies of lesions have largely refuted the possible vascular, neural or smooth muscle origin. Recent studies suggest a neoplastic etiology due to a mutation, in some cases, in the alpha-type platelet-derived growth factor receptor gene (PDGFRa). Our objective is to report the case of a patient aged 70 years, with gastric IFP, comparing her immunohistochemical profile with those of other studies, and a brief review of the literature.

Osteotomia ventral da bula timpânica em gatos: revisão de literatura

Otite média e pólipos são as principais afecções da orelha média em gatos. A otite média geralmente é decorrente de otite externa crônica, enquanto os pólipos se formam a partir de um processo inflamatório crônico presente na orelha média. Quando o pólipo sai da cavidade timpânica pela tuba auditiva, aparecendo na nasofaringe, é denominado pólipo nasofaríngeo. Outra possibilidade é o pólipo romper a membrana do tímpano e surgir no meato acústico externo. O tratamento indicado para essas afecções é a osteotomia ventral da bula timpânica, procedimento cirúrgico cuja finalidade é remover exsudatos inflamatórios presentes na cavidade timpânica. Apesar de possíveis complicações, como síndrome de Horner e lesão na orelha interna, essa cirurgia proporciona resultados muito satisfatórios. O objetivo da presente revisão é relatar essas afecções da orelha média em gatos e descrever a técnica cirúrgica de osteotomia ventral da bula timpânica.

Avaliação da cavidade uterina com histerossonografia, uma revisão

Sonohysterography was firstly described three decades ago. The saline solution infusion into the uterine cavity favors its use and provides excellent visualization of the anatomy and the inner cavity of the uterus better than the conventional transvaginal sonography To check the current role of sonohysterography in the uterine cavity assessment in women with abnormal uterine bleeding and asymptomatic, a literature review comparing sonohysterograph with conventional transvaginal sonography and/or ambulatory diagnostic hysteroscopy was carried out. To this end, relevant studies were researched in electronic databases Medline/PubMed, SciELO/LILACS. The sonohysterography is an ambulatory procedure, non-invasive, better cost-benefit, better sensitivity and specificity to identify uterine abnormalities, causing minimal discomfort and low complications rate. It was subject to revision which there is no more doubt about its accuracy. It can be concluded that the sonohysterography is a useful tool in the propedeutics to assess uterine cavity of symptomatic patients with abnormal uterine bleeding, infertility, recurrent miscarriages, and embryonic implantation failures in assisted reproduction treatment / in vitro fertilization and in any other intra and extra uterine cavity alteration. Hence, conventional transvaginal sonography is indicated as an initial method of assessment of the uterine cavity previously to ambulatory diagnostic hysteroscopy.