Produção, qualidade e conservação pós-colheita de mandioquinha-salsa (Arracacia xanthorrhiza Bancroft) sob adubações mineral, orgânica e biodinâmica

Coordenação de Aperfeiçoamento de Pessoal de Nível Superior (CAPES)

Efecto de la fertilización orgánica y mineral en las propiedades del suelo, la emisión de los principales gases de efecto invernadero y en las diferentes fases fenológicas del cultivo de café (Coffea arabica L.)

El cultivo de café es de gran importancia a nivel mundial (ICO, 2011), y en el Ecuador ha sido uno de los cultivos más importantes en la generación de divisas (COFENAC, 2011). Sin embargo en los sistemas productivos de este país se puede apreciar el uso inapropiado de fertilizantes, lo que conlleva a una pérdida de nutrientes, por lo que es importante estudiar las dosis adecuadas para la fertilización tanto mineral como orgánica. El objetivo del trabajo fue evaluar el efecto de la fertilización mineral y orgánica en diferentes dosis en un monocultivo de café en la provincia de Loja, sobre las propiedades del suelo, la emisión de los principales gases que provocan el efecto invernadero y la fenología y productividad del cultivo. En la provincia de Loja (Ecuador) se seleccionó un área de 2.520 m2 en la que se establecieron 21 parcelas de café arábigo (Coffea arabica L.) var. caturra y se aplicó tres tratamientos con tres repeticiones de fertilización mineral y tres orgánicos con dosis: bajas minerales (MIN 1= 157 Kg NPK ha-1 año-1 para el primer año y 425 Kg NPK ha-1 año-1 para el segundo año), medias minerales (MIN 2= 325 Kg NPK ha-1 año-1 para el primer año y 650 Kg NPK ha-1 año-1 en el segundo año) y altas minerales (MIN 3= 487 y 875 Kg NPK ha-1 año-1 para el primer y segundo año respectivamente), bajas orgánicas (ORG 1= 147 Kg NPK ha-1 año-1 en el primer año y 388 Kg NPK ha-1 año-1 en el año dos), medias orgánicas (ORG 2= 265 Kg NPK ha-1 año-1 para el primer año y 541 Kg NPK ha-1 año-1 en el segundo año), altas orgánicas (ORG 3= 368 Kg NPK ha-1 año-1 para el primer año y 727 Kg NPK ha-1 año-1 en el segundo año) y fertilización cero (TES = sin fertilización). Se usó urea, roca fosfórica y muriato de potasio en la fertilización mineral y humus (Bioabor) en la orgánica, más un tratamiento testigo, cada tratamiento tuvo tres repeticiones. El tiempo de evaluación de los fertilizantes aplicados fue de dos años consecutivos, la fertilización se la realizó dos veces por año y en base a análisis del suelo y demandas nutricionales del cultivo. para determinar las características del suelo se realizó muestreos de suelos en cada parcela a una profundidad de 20 cm de estas muestras los parámetro iniciales determinados fueron: color (Munsell), textura (método del hidrómetro), pH (relación 1:2,5 suelo-agua), Materia orgánica (Walkey y Black), Nitrógeno (Micro Kjendahl), Fósforo (Bray y Kurtz), Potasio (Olsen), estos procesos se repitieron cada seis meses para poder evaluar los cambios de que se producen debido a la fertilización mineral y orgánica en el cultivo. Las emisiones de gases efecto invernadero desde el suelo al ambiente se determinaron por el método de cámara cerrada (Rondón, 2000) y la concentración por cromatografía de gases. Las mediciones fisiológicas (altura de planta, ancho de copa, grosor de tallo y producción) se las evaluó cada dos meses, a excepción de la producción que fue anual al término de cada cosecha. Además se realizó el análisis económico de la productividad del cultivo. El análisis estadístico de datos se lo realizó con el programa SPSS v. 17.0. Las medias fueron comprobadas mediante ANOVAS de un factor con test de Tukey (P < 0,05). El beneficio económico se estimó en términos de ingresos y gastos totales que se presentaron en el ensayo. Los resultados obtenidos al término del ensayo indican que los tratamientos MIN 2 y MIN 3 produjeron cambios más significativos en comparación con los otros tratamientos establecidos en la mejora de fertilidad del suelo, el pH ha sido menos afectado en la acidificación en comparación con los tratamientos orgánicos que se han acidificado mayormente; la materia orgánica (MO) tuvo incrementos considerablemente bueno en estos dos tratamientos, sin embargo fueron superados por los tratamientos de fertilización orgánica; el nitrógeno total (Nt )y el potasio (K) también presentaron mejores valores al termino del ensayo y el fósforo (P) mostro incrementos buenos aunque un poco menores que los de los tratamientos ORG 2 y ORG 3. En lo que respecta a las emisiones de gases efecto invernadero, los flujos acumulados de óxido nitroso (N2O) en los dos años han aumentado en todos los tratamientos en comparación con el tratamiento Testigo, pero de manera considerable y con mayores flujos en el tratamiento MIN 3 y MIN 2 que se podrían considerarse los de mayor contaminación por N2O al ambiente lo que se le atribuye a las dosis de fertilización mineral aplicadas en el periodo de investigación, los tratamiento MIN 1 y todos los tratamientos orgánicos muestran menores emisiones al ambiente. Las emisiones de metano (CH4) no muestran mayores diferencias de emisiones entre tratamientos, siendo los mayores emisores los tratamientos ORG 3 y ORG 2 posiblemente debido al abono orgánico y añadido al suelo; para las emisiones de dióxido de carbono (CO2) de manera similar al CH4 el tratamiento ORG 3 fue el que presento mayores emisiones, los flujos de CO2 al ambiente de los otros tratamientos fueron menores y no presentaron diferencias significativas entre ellos. La variables fisiológicas en todos los casos apoyaron al desarrollo de las plantas de café, esto al ser comparadas con el tratamiento Testigo, sin embargo las que alcanzaron las mayores altitudes, anchos de copas y diámetro de tallo fueron las plantas del tratamiento MIN 3, seguido del MIN 3, no mostrando significancia entre ellos, y para los tratamientos orgánicos el que presento muy buenos resultados en estas variables ha sido el ORG 3, el cual no presento diferencias significativas con el MIN 2, lo cual comprueba que la fertilización mineral es más efectiva en este caso frente a la orgánica. Para el primer año de producción el tratamiento mineral con fertilización MIN 3 es el que obtuvo mayor producción no presentando diferencia estadística con el tratamiento con el MIN 2, no obstante fueron significativamente mayores que los otros tratamientos. Vale indicar que también el tratamiento MIN 1 y el tratamiento ORG 3 han presentado una producción considerable de café no mostrando diferencias estadísticas entre ellos. Para el segundo año la producción el cultivo mostró mayores rendimientos que el primer año de evaluación en todos los tratamientos, esto debido a la fisiología propia del cultivo y por otra parte se atribuye a la adición de fertilizantes que se ha realizado durante todo el ensayo; de manera similar al anterior los tratamientos MIN 3 y MIN 2 obtuvieron mejores rendimientos, no enseñando diferencias estadísticas significativas entre ellos, no obstante el tratamiento mineral dosis MEDIA no presentó significancia estadística con el ORG 3. El benéfico económico ha resultado mayor en el tratamiento MIN 3 y MIN 2, aunque el tratamiento MIN 2, es el que obtiene la mejor relación costo-beneficio; los tratamientos ORG 2 y ORG 3 y Testigo has producido beneficios negativos para el productor. En cuanto a la parte ambiental se considera que los mejores tratamientos en cuanto ha cuidado ambiental serían los tratamientos MIN 1 y ORG 1, sin embargo a nivel de producción y rentabilidad para el productor baja. ABSTRACT Coffee growing has great importance worldwide (ICO, 2011), and in Ecuador, it has been one of the most important crops to generate income (COFENAC, 2011). However, in the productive systems of this country, the inappropriate use of fertilizers has been observed which produces loss of nutrients, thus it is important to study suitable doses for mineral and organic fertilizing. The purpose of the study was to evaluate the effect of mineral and organic fertilizing at different doses in a coffee monoculture in the province of Loja on soil characteristics, emission of the main gasses that produce the greenhouse effect and the phenology and productivity of crops. In the province of Loja (Ecuador) an area of 2.520 m2 was chosen, where 21 plots of Arabica coffee (Coffea arabica L.), the caturra variety were cultivated and three treatments with three repetitions each one for mineral and organic fertilization were used with doses that ranged from: mineral low (MIN 1= 157 Kg NPK ha-1 año-1 for the first year y 425 Kg NPK ha-1 año-1 for the second year), mineral medium (MIN 2= 325 Kg NPK ha-1 año-1 for the first year y 650 Kg NPK ha-1 año-1 I the second year) y mineral high (MIN 3= 487 y 875 Kg NPK ha-1 año-1 for the first and second year respectively), organic low (ORG 1= 147 Kg NPK ha-1 año-1 in the first year y 388 Kg NPK ha-1 año-1 in the second year), organics medium (ORG 2= 265 Kg NPK ha-1 año-1 for the first year y 541 Kg NPK ha-1 año-1 in the second year), organics high (ORG 3= 368 Kg NPK ha-1 año-1 for the first year and 727 Kg NPK ha-1 año-1 in the second year) y fertilization zero (TES = no fertilization).; urea, phosphoric rock and muriate of potash were used in the mineral fertilization and humus (Bioabor) in the organic, plus a blank treatment. Time to evaluate the applied fertilizers was for two consecutive years, fertilization was done twice per year based on soil analysis and nutritional requirements of the crops. In order to determine the characteristics of the soil, samples of soil in each plot with a depth of 20 cm were done; from these samples, the determined initial parameters were: color (Munsell), texture (hydrometer method), pH (soil-water 1:2,5 relation), organic matter (Walkey y Black), nitrogen (Micro Kjendahl), phosphorus (Bray y Kurtz), potassium (Olsen); these processes were repeated each six months in order to evaluate the changes that are produced due to mineral and organic fertilization in the crops. The emissions of greenhouse gasses from the soil to the atmosphere were determined by using enclosure method (Rondón, 2000) and the concentration, by using gas chromatography during the whole testing. The physiological measures (plant height, width of the top of the tree, thickness of the stem and production) were evaluated each two months, except for production which was annual at the end of each harvest. Moreover, the economic analysis of the productivity of the crops was done. The statistical analysis of the data was done using SPSS v. 17.0. The means were proved by ANOVAS with a factor of a Tukey test (P < 0,05). The economic benefit was estimated in terms of incomes and total expenses which were presented in the essay. The results obtained at the end of the essay show that the MIN 2 and MIN 3 treatments produced more meaningful changes in comparison with the other treatments used to improve soil fertility; pH was less affected in the acidification compared with the organic treatments which were greatly acidified; organic matter (MO) had increased considerably in these two treatments; however, they were surpassed by the organic treatments of fertilization; total nitrogen (Nt) and potassium (K) also presented better results at the end of the essay and phosphorus (P) showed good increasing figures although a little lower compared with ORG 2 and ORG 3 treatments. Regarding the emission of the greenhouse gasses, the fluxes accumulated from nitrous oxide (N2O) in two years increased in all the treatments in comparison with the blank treatment, but in a greater form and with higher fluxes in the MIN 3 and MIN 2 treatments which can be considered as the ones with greater contamination of N2O in the atmosphere, this can be due to the applied mineral doses to fertilize during the process; MIN 1 treatments and all the organic ones showed lower emission to the atmosphere. Methane emissions (CH4) did not show major differences in emissions in the treatments, being the greater emissions the ORG 3 and ORG 2 treatments; this is possibly due to the organic compost added to the soil; regarding carbon dioxide (CO2) emissions, in a similar way to CH4, the ORG 3 treatment was the one that presented greater emissions, the CO2 emissions to the atmosphere in the other treatments were lower and did not present meaningful differences among them. The physiological variables in all the cases helped coffee crops grow, this was observed when compared with the blank treatment; however, plants that reached the greatest height, width of top and diameter of stem were the plants of the MIN 3 treatment, followed by MIN 3, which did not show much significance among them, and for the organic treatments, the one that presented great results in these variables was ORG 3, which did not show meaningful differences compared with MIN 2, which proves that mineral fertilization is more effective in this case compared with the organic. In the first year of production, the mineral treatment with MIN 3 fertilization obtained greater production and thus did not show statistical difference with MIN 2 treatment, although the other treatments were greater. It is worth mentioning that MIN 1 treatment and ORG 3 treatment presented a meaningful production of coffee, not showing statistical differences among them. For the second year, the production of the crops showed greater profits than in the first year of evaluation in all the treatments, this was due to the physiological properties of the crops and on the other hand, it might be due to the addition of fertilizers during the whole essay; in a similar way, MIN 3 and MIN 2 performed better, not showing greater statistical differences among them, although the mineral treatment MEDIUM doses did not show statistical difference compared with ORG 3. The economic benefit was greater in the MIN 3 and MIN 2 treatments, although MIN 2 treatment is the one that shows the best cost-benefit ratios; ORG 2 and ORG 3 treatments and the blank produced negative benefits for the producer. Regarding the environment, the best treatments to care for the atmosphere are considered to be MIN 1 and ORG 1 treatments; however, regarding production volume and profitability they were low for the producer.

Causes of legume rotation induced yield increases in cereals grown on West African soils

This study was conducted to investigate soil biological and chemical factors that give rise to cereal yield enhancing effects of legume rotations on sandy, nutrient poor West African soils. The aim was not only to gain more information on the role of legume residues and microorganisms in the soil nutrient cycle. But the study aimed at evaluating if differences in substrate qualities (e.g. root residues) cause changes in the microbial community structure due to specific and highly complex microbe-root-soil interactions. Site and system specific reactions of microorganisms towards rewetting, simulating the onset of rainy season, were observed. Higher respiration rates, higher amounts of microbial biomass carbon (Cmic) and nitrogen (Nmic) as well as higher ergosterol, muramic acid, glucosamine and adenylate concentrations were measured in CL soils of Koukombo and in both soils from Fada. The immediate increase in ATP concentrations after rewetting was likely caused by rehydration of microbial cells where N was not immobilized and, thus, available for plants facilitating their rapid development. Legume root residues led only to slightly better plant performances compared to the control, while the application of cereal roots reduced seedling growth. In contrast to sorghum seedlings, the microbial community did not react to the mineral treatment. Thus the energy supply in form of organic amendments increased microbial indices compared to mineral P application and the control. The results of basal respiration rates, Cmic and Corg levels indicate that the microbial community in the soil from Koukombo is less efficient in substrate use compared to microorganisms in the soil from Fada. However, the continuous carbon input by legume root residues might have contributed to these differences in soil fertility. With the 33P isotopic exchange method a low buffering capacity was detected in both soils irrespective of treatments. Calculated E values (E1min to E1min-1d and E1d-3m) indicated a slowly release of P due to root turnover while applied mineral P is taken up by plants or fixed to the soil. Due to the fact that sorghum growth reacted mainly to the application of mineral P and the microorganisms solely to the organic inputs, the combination of both amendments seems to be the best approach to a sustainable increase of crop production on many nutrient-poor, sandy West African soils. In a pot experiment, were CC and CL soils from Fada and Koukombo were adjusted to the same level of P and N concentrations, crop growth was significantly higher on CL soils, compared to the respective treatments on CC soils. Mycorrhizal infection of roots was increased and the number of nematodes, predominantly free living nematodes, was almost halfed on rotation soils. In conclusion, increased nutrient availability (especially P and N) through the introduction of legumes is not the only reason for the observed yield increasing effects. Soil biological factors seem to also play an important role. In a root chamber experiment the pH gradient along the root-soil-interface was measured at three times using an antimony microelectrode. For Fada soils, pH values were higher on CL than CC soils while the opposite was true for the Koukombo soils. Site-specific differences between Fada and Koukombo soils in N content and microbial community structures might have created varying crop performances leading to the contrasting pH findings. However, the mechanisms involved in this highly complex microbe-root-soil interaction remain unclear.

Yield and phytochemical characterization of essential oil from Ocimum selloi B. obtained by hydrodistillation and supercritical fluid extraction

The yield and chemical composition of essential oils from leaves of Ocimum selloi B. submitted to organic and mineral fertilization, obtained by hydrodistillation and supercritical fluid extraction (SFE) were compared. Essential oil was extracted in a Clevenger-type apparatus for 2 h 30 min and analyzed by GC-MS (Shimadzu, QP 5050-DB-5 capillary column - 30 m × 0.25 mm × 0.25 μm). Carrier gas was helium (1.7 ml/min); split ratio: 1:30. Temperature program: 50°C, rising to 180°C at 5°C/min, 180°C, rising to 280°C at 10°C/min. Injector temperature: 240°C and detector temperature: 230°C. Identifications of chemical compounds were made by matching their mass spectra and Kovat's indices (IK) values with known compounds reported in the literature. An Applied Separations-apparatus (Speed SFE, model 7071, Allentown, PA, EUA) was used for SFE extractions. They were conducted at pressure 200 bar and temperature 30°C (20 min in static mode and 40 min in dynamic mode). The supercritical CO2 flow rate was (6.8±0.7)×10-5 kg-CO2/s. The essential oil collected was immersed in ethylene glycol bath (5°C). The yield of essential oils obtained by SFE was larger than hydrodistillation in both fertilization treatments (279 and 333% for organic and mineral fertilizations, respectively). There were no differences between the fertilization treatments. The amount of the volatile components showed by GC-MS chromatogram was highest in the essential oil obtained by hydrodistillation than SFE. The main volatile constituents of the essential oils were trans-anethole (Hydrodistillation: organic - 52.4%; mineral - 55.0%/ SFE: Hydrodistillation - 62.8%; mineral - 66.8%) and methyl-chavicol (Hydrodistillation: organic - 37.3%; mineral - 38.3%/ SFE: organic - 8.4%; mineral - 4.3%). A reduction of methyl-chavicol relative proportion of essential oil obtained by SFE was observed. Cys-anethole, α-copaene, trans-cariofilene, germacrene-D, β-selinene, biciclogermacrene and spathulenol were expressed only in hydrodistillation. The extraction of essential oil by SFE presented larger yield of essential oil than hydrodistillation technique, presenting, however, these essential oils, different phytochemical profiles.

Mineral trioxide aggregate as an alternative treatment for intruded permanent teeth with root resorption and incomplete apex formation

A case of extensive crown fracture associated with intrusion of the permanent maxillary central incisors in an 8-year-old boy is reported. The treatment of both injured teeth included attempts of apexification and arrest of root resorption with calcium hydroxide. After 8 months of the trauma, there was no calcified barrier formation in the apex. Mineral trioxide aggregate (MTA) was then used as a filling material. At 15-month follow up, the teeth were asymptomatic and correctly sealed, the external inflammatory root resorption had stopped, and the radiolucent image had disappeared, which meant the initial healing of the periapical lesion. MTA may be considered as an alternative option for the treatment of traumatized and immature permanent teeth.

Effects of Exemestane and Tamoxifen Treatment on Bone Texture Analysis Assessed by TBS in Comparison With Bone Mineral Density Assessed by DXA in Women With Breast Cancer.

We performed an analysis of a substudy of the randomized Tamoxifen Exemestane Adjuvant Multinational trial to determine the effects of exemestane (EXE) and tamoxifen (TAM) adjuvant treatment on bone mineral density (BMD) measured by dual-energy X-ray absorptiometry compared with the trabecular bone score, a novel grey-level texture measurement that correlates with 3-dimensional parameters of bone texture in postmenopausal women with hormone receptor-positive breast cancer for the first time. In total, 36 women were randomized to receive TAM (n = 17) or EXE (n = 19). Patients receiving TAM showed a mean increase of BMD in lumbar spine from baseline of 1.0%, 1.5%, and 1.9% and in trabecular bone score of 2.2%, 3.5%, and 3.3% at 6-, 12-, and 24-mo treatment, respectively. Conversely, patients receiving EXE showed a mean decrease from baseline in lumbar spine BMD of -2.3%, -3.6%, and -5.3% and in trabecular bone score of -0.9%, -1.7%, and -2.3% at 6-, 12-, and 24-mo treatment, respectively. Changes in trabecular bone score from baseline at spine were also significantly different between EXE and TAM: p = 0.05, 0.007, and 0.006 at 6, 12, and 24mo, respectively. TAM induced an increase in BMD and bone texture analysis, whereas EXE resulted in decreases. The results were independent from each other.

Bone mineral density measurement and osteoporosis treatment after a fragility fracture in older adults: regional variation and determinants of use in Quebec

Affiliation: Pierre Dagenais : Hôpital Maisonneuve-Rosemont, Faculté de médecine, Université de Montréal

Combining adapted Judo training and pharmacological treatment to improve bone mineral density on postmenopausal women: A two years study

Background & Study Aim: Physical activity has been an important factor to increase bone mineral density (BMD) and, consequently, to prevent and treat osteoporosis. The study aimed the effects of adapted Judo training on BMD in postmenopausal women, during pharmacological treatment. Material & Methods: Eighteen female volunteers participated in this study. They were separated into two groups: Adapted Judo training (AJT) (n=11; 52.2±5.3 years) and control group (CG) (n=7; 53.8±4.4 years). Lunar GE Dual Energy X-Ray Absorptiometry (DXA) measured BMD at lumbar L2-L4, femoral neck and trochanter sites. The training period for AJT was two years, comprised 12 mesocycles with different intensities. ANOVA compared 2 groups in 3 moments of testing and Scheffé Test allowed multiple comparisons between groups for the L2-L4 and femoral neck sites, but at trochanter was Fisher LSD. Results: ANOVA showed significant differences in the AJT group (F(2, 32)=15.187, p=0.000023). Scheffé Test showed significant increase on lumbar BMD after one year of AJT (Δ%=+8.9%, p=0.000017) and after two years this improvement stand still (p=0.33). The CG after one year presented significant decrease in BMD of femoral neck (Δ%=-6.9%, p=0.03) and trochanter (Δ%=-3.7%, p=0.0084). However, the CG recovered the loss of BMD of femoral neck (Δ%=+7.6%, p=0.02) and trochanter (Δ%=+3.8%, p=0.0079) after two years of study. Conclusions: Drug therapy, without the physical activity practice, can aid the maintenance of BMD. AJT may be considered as an efficient physical activity for postmenopausal women with low BMD in pharmacological treatment. © ARCHIVES OF BUDO | SCIENCE OF MARTIAL ARTS.

Bone mineral density and body composition in girls with idiopathic central precocious puberty before and after treatment with a gonadotropin-releasing hormone agonist

OBJECTIVES: Idiopathic central precocious puberty and its postponement with a (gonadotropin-releasing hormone) GnRH agonist are complex conditions, the final effects of which on bone mass are difficult to define. We evaluated bone mass, body composition, and bone remodeling in two groups of girls with idiopathic central precocious puberty, namely one group that was assessed at diagnosis and a second group that was assessed three years after GnRH agonist treatment. METHODS: The precocious puberty diagnosis and precocious puberty treatment groups consisted of 12 girls matched for age and weight to corresponding control groups of 12 (CD) and 14 (CT) girls, respectively. Bone mineral density and body composition were assessed by dual X-ray absorptiometry. Lumbar spine bone mineral density was estimated after correction for bone age and the mathematical calculation of volumetric bone mineral density. CONEP: CAAE-0311.0.004.000-06. RESULTS: Lumbar spine bone mineral density was slightly increased in individuals diagnosed with precocious puberty compared with controls; however, after correction for bone age, this tendency disappeared (CD = -0.74 +/- 0.9 vs. precocious puberty diagnosis = -1.73 +/- 1.2). The bone mineral density values of girls in the precocious puberty treatment group did not differ from those observed in the CT group. CONCLUSION: There is an increase in bone mineral density in girls diagnosed with idiopathic central precocious puberty. Our data indicate that the increase in bone mineral density in girls with idiopathic central precocious puberty is insufficient to compensate for the marked advancement in bone age observed at diagnosis. GnRH agonist treatment seems to have no detrimental effect on bone mineral density.

The influence of heat treatment on the phase relations in mineral growth systems

ABSTRACT Corundum is one of the most famous gems materials. Different heat treatment methods for enhancement purposes are commonly applied and accepted in the gem market. With this reason, the identification of the natural, unheated corundum is intensively investigated. In this study, aluminium hydroxide minerals and zircon are focused to observe the crystallization and phase change of these minerals during heat treatment procedures. Aluminium hydroxide minerals can be transformed to alumina with the corundum structure by heating. The reaction history of aluminium hydroxide minerals containing corundum was investigated comparing it with diaspore, boehmite, gibbsite and bayerite by TG and DTA methods. These hydroxide minerals were entirely transformed to corundum after heating at 600°C. Zircon inclusions in corundums from Ilakaka, Madagascar, were investigated for the influence of different heat-treatment temperatures on the recovery of their crystalline structure and on possible reactions within and with the host crystals. The host corundum was heated at 500, 800, 1000, 1200, 1400, 1600 and 1800°C. The crystallinity, the trapped pressure, and the decomposition of the zircon inclusions within the host corundum have been investigated by Raman spectroscopy. Radiation-damaged zircon inclusions may be used as an indicator for unheated Ilakaka corundum crystals. They are fully recrystallized after heating at 1000°C influencing the lowering of the 3 Raman band shift, the decreasing of FWHM of the 3 Raman band and the decreasing of the trapped pressure between the inclusion and the host corundum. Under microscopic observation, surface alterations of the inclusions can be firstly seen from transparent into frosted-like appearance at 1400°C. Then, between 1600°C and 1800 °C, the inclusion becomes partly or even completely molten. The decomposition of the zircon inclusion to m-ZrO2 and SiO2-glass phases begins at the rim of the inclusion after heating from 1200°C to 1600°C which can be detected by the surface change, the increase of the 3 Raman band position and the trapped pressure. At 1800°C, the zircon inclusions entirely melt transforming to solid phases during cooling like m-ZrO2 and SiO2-glass accompanied by an increase of pressure between the transformed inclusion and its host.

Guided tissue regeneration/deproteinized bovine bone mineral or papilla preservation flaps alone for treatment of intrabony defects. II: radiographic predictors and outcomes

OBJECTIVES: This study reports the secondary analysis of a randomized-controlled clinical trial designed to assess the efficacy of deproteinized bovine mineral and a collagen membrane in the treatment of intrabony defects. The specific aims of this report are (1) to analyse the radiographic bone changes 1 year after therapy and (2) to assess the association between radiographic defect angle and treatment outcomes. MATERIALS AND METHODS: Baseline and 12-month radiographs were collected from 120 patients with advanced chronic periodontitis from 10 centres in seven countries as part of a multi-centre clinical trial. All patients had at least one intrabony defect > or =3 mm in depth. The treatment consisted of simplified or modified papilla preservation flaps to access the defect. After debridement of the area, a deproteinized bovine mineral and a collagen membrane were applied in the test subjects, and omitted in the controls. Main outcome measures were radiographic bone fill and defect resolution 1 year after surgery. RESULTS: One hundred and twenty pairs of radiographs were obtained, of which 110 pairs were measurable (57 tests and 53 controls). One year after treatment, radiographic resolution of the intrabony component was significantly higher in the test group (3.2+/-1.7 mm) when compared with the controls (1.7+/-1.9 mm). Multivariate analysis indicated that the treatment and the baseline radiographic depth of the intrabony defect significantly influenced the radiographic bone fill of the intrabony defect 1 year following treatment. The percentage of resolution of the defect was influenced by the treatment provided and the baseline plaque score. The baseline radiographic defect angle did not show a significant impact on the clinical and radiographic outcomes. CONCLUSIONS: Regenerative periodontal surgery with a deproteinized bovine bone mineral and a collagen membrane offered additional benefits in terms of radiographic resolution of the intrabony defect and predictability of outcomes with respect to papilla preservation flaps alone.

Cortical and trabecular bone mineral density in transsexuals after long-term cross-sex hormonal treatment: a cross-sectional study

The aim of this study was to explore the effect of long-term cross-sex hormonal treatment on cortical and trabecular bone mineral density and main biochemical parameters of bone metabolism in transsexuals. Twenty-four male-to-female (M-F) transsexuals and 15 female-to-male (F-M) transsexuals treated with either an antiandrogen in combination with an estrogen or parenteral testosterone were included in this cross-sectional study. BMD was measured by DXA at distal tibial diaphysis (TDIA) and epiphysis (TEPI), lumbar spine (LS), total hip (HIP) and subregions, and whole body (WB) and Z-scores determined for both the genetic and the phenotypic gender. Biochemical parameters of bone turnover, insulin-like growth factor-1 (IGF-1) and sex hormone levels were measured in all patients. M-F transsexuals were significantly older, taller and heavier than F-M transsexuals. They were treated by cross-sex hormones during a median of 12.5 years before inclusion. As compared with female age-matched controls, they showed a significantly higher median Z-score at TDIA and WB (1.7+/-1.0 and 1.8+/-1.1, P < 0.01) only. Based on the WHO definition, five (who did not comply with cross-sex hormone therapy) had osteoporosis. F-M transsexuals were treated by cross-sex hormones during a median of 7.6 years. They had significantly higher median Z-scores at TEPI, TDIA and WB compared with female age-matched controls (+0.9+/-0.2 SD, +1.0+/-0.4 SD and +1.4+/-0.3 SD, respectively, P < 0.0001 for all) and reached normal male levels except at TEPI. They had significantly higher testosterone and IGF-1 levels (p < 0.001) than M-F transsexuals. We conclude that in M-F transsexuals, BMD is preserved over a median of 12.5 years under antiandrogen and estrogen combination therapy, while in F-M transsexuals BMD is preserved or, at sites rich in cortical bone, is increased to normal male levels under a median of 7.6 years of androgen treatment in this cross sectional study. IGF-1 could play a role in the mediation of the effect of androgens on bone in F-M transsexuals.

Ten-year results following treatment of intrabony defects with an enamel matrix protein derivative combined with either a natural bone mineral or a β-tricalcium phosphate

BACKGROUND The purpose of the present study is to evaluate the 10-year results following treatment of intrabony defects treated with an enamel matrix protein derivative (EMD) combined with either a natural bone mineral (NBM) or β-tricalcium phosphate (β-TCP). METHODS Twenty-two patients with advanced chronic periodontitis and displaying one deep intrabony defect were randomly treated with a combination of either EMD + NBM or EMD + β-TCP. Clinical evaluations were performed at baseline and at 1 and 10 years. The following parameters were evaluated: plaque index, bleeding on probing, probing depth, gingival recession, and clinical attachment level (CAL). The primary outcome variable was CAL. RESULTS The defects treated with EMD + NBM demonstrated a mean CAL change from 8.9 ± 1.5 mm to 5.3 ± 0.9 mm (P <0.001) and to 5.8 ± 1.1 mm (P <0.001) at 1 and 10 years, respectively. The sites treated with EMD + β-TCP showed a mean CAL change from 9.1 ± 1.6 mm to 5.4 ± 1.1 mm (P <0.001) at 1 year and 6.1 ± 1.4 mm (P <0.001) at 10 years. At 10 years two defects in the EMD + NBM group had lost 2 mm, whereas two other defects had lost 1 mm of the CAL gained at 1 year. In the EMD + β-TCP group three defects had lost 2 mm, whereas two other defects had lost 1 mm of the CAL gained at 1 year. Compared with baseline, at 10 years, a CAL gain of ≥3 mm was measured in 64% (i.e., seven of 11) of the defects in the EMD + NBM group and in 82% (i.e., nine of 11) of the defects in the EMD + β-TCP group. No statistically significant differences were found between the 1- and 10-year values in either of the two groups. Between the treatment groups, no statistically significant differences in any of the investigated parameters were observed at 1 and 10 years. CONCLUSION Within their limitations, the present findings indicate that the clinical improvements obtained with regenerative surgery using EMD + NBM or EMD + β-TCP can be maintained over a period of 10 years.