Spine trabecular bone score subsequent to bone mineral density improves fracture discrimination in women.

Bone mineral density (BMD) measured by dual-energy X-ray absorptiometry (DXA) is used to diagnose osteoporosis and assess fracture risk. However, DXA cannot evaluate trabecular microarchitecture. This study used a novel software program (TBS iNsight; Med-Imaps, Geneva, Switzerland) to estimate bone texture (trabecular bone score [TBS]) from standard spine DXA images. We hypothesized that TBS assessment would differentiate women with low trauma fracture from those without. In this study, TBS was performed blinded to fracture status on existing research DXA lumbar spine (LS) images from 429 women. Mean participant age was 71.3 yr, and 158 had prior fractures. The correlation between LS BMD and TBS was low (r = 0.28), suggesting these parameters reflect different bone properties. Age- and body mass index-adjusted odds ratios (ORs) ranged from 1.36 to 1.63 for LS or hip BMD in discriminating women with low trauma nonvertebral and vertebral fractures. TBS demonstrated ORs from 2.46 to 2.49 for these respective fractures; these remained significant after lowest BMD T-score adjustment (OR = 2.38 and 2.44). Seventy-three percent of all fractures occurred in women without osteoporosis (BMD T-score > -2.5); 72% of these women had a TBS score below the median, thereby appropriately classified them as being at increased risk. In conclusion, TBS assessment enhances DXA by evaluating trabecular pattern and identifying individuals with vertebral or low trauma fracture. TBS identifies 66-70% of women with fracture who were not classified with osteoporosis by BMD alone.

Mineral zoning and geochemistry of epithermal polymetallic Zn-Pb-Ag-Cu-Bi mineralization at Cerro de Pasco, Peru

The large Cerro de Pasco Cordilleran base metal deposit in central Peru is located on the eastern margin of a middle Miocene diatreme-dome complex and comprises two mineralization stages. The first stage consists of a large pyrite-quartz body replacing Lower Mesozoic Pucara carbonate rocks and, to a lesser extent, diatreme breccia. This body is composed of pyrite with pyrrhotite inclusions, quartz, and black and red chalcedony (containing hypogene hematite). At the contact with the pyrite-quartz body, the diatreme breccia is altered to pyrite-quartz-sericite-pyrite. This body was, in part, replaced by pipelike pyrrhotite bodies zoned outward to carbonate-replacement Zn-Pb ores hearing Fe-rich sphalerite (up to 24 mol % Fes). The second mineralization stage is partly superimposed on the first and consists of zoned east-west-trending Cu-Ag-(Au-Zn-Pb) enargite-pyrite veins hosted in the diatreme breccia in the western part of the deposit and well-zoned Zn-Pb-(Bi-Ag-Cu) carbonate-replacement orebodies; in both cases, sphalerite is Fe poor and the inner parts of the orebodies show typically advanced argillic alteration assemblages, including aluminum phosphate Sulfate (APS) minerals. The zoned enargite-pyrite veins display mineral zoning, from a core of enargite-pyrite +/- alunite with traces of Au, through an intermediate zone of tennantite, chalcopyrite, and Bi minerals to a poorly developed Outer zone hearing sphalerite-galena +/- kaolinite. The carbonate-hosted replacement ores are controlled along N 35 degrees E, N 90 degrees E, N 120 degrees E, and N 170 degrees E faults. They form well-zoned upward-flaring pipelike orebodies with a core of famatinite-pyrite and alunite, an intermediate zone with tetrahedrite-pyrite, chalcopyrite, matildite, cuprobismutite, emplectite, and other Bi minerals accompanied by APS minerals, kaolinite, and dickite, and an outer zone composed of Fe-poor sphalerite (in the range of 0.05-3.5 mol % Fes) and galena. The outermost zone consists of hematite, magnetite, and Fe-Mn-Zn-Ca-Mg carbonates. Most of the second-stage carbonate-replacement orebodies plunge between 25 degrees and 60 degrees to the west, suggesting that the hydrothermal fluids ascended from deeper levels and that no lateral feeding from the veins to the carbonate-replacement orebodies took place. In the Venencocha and Santa Rosa areas, located 2.5 km northwest of the Cerro de Pasco open pit and in the southern part of the deposit, respectively, advanced argillic altered dacitic domes and oxidized veins with advanced argillic alteration halos occur. The latter veins are possibly the oxidized equivalent of the second-stage enargite-pyrite veins located in the western part of the deposit. The alteration assemblage quartz-muscovite-pyrite associated with the pyrite-quartz body suggests that the first stage precipitated at slightly, acidic fin. The sulfide mineral assemblages define an evolutionary path close to the pyrite-pyrrhotite boundary and are characteristic of low-sulfidation states; they suggest that the oxidizing slightly acidic hydrothermal fluid was buffered by phyllite, shale, and carbonate host rock. However, the presence in the pyrite-quartz body of hematite within quartz suggests that, locally, the fluids were less buffered by the host rock. The mineral assemblages of the second mineralization stage are characteristic of high- to intermediate-sulfidation states. High-sulfidation states and oxidizing conditions were achieved and maintained in the cores of the second-stage orebodies, even in those replacing carbonate rocks. The observation that, in places, second-stage mineral assemblages are found in the inner and outer zones is explained in terms of the hydrothermal fluid advancing and waning. Microthermometric data from fluid inclusions in quartz indicate that the different ores of the first mineralization stage formed at similar temperatures and moderate salinities (200 degrees-275 degrees C and 0.2-6.8 wt % NaCl equiv in the pyrite-quartz body; 192 degrees-250 degrees C and 1.1-4.3 wt % NaCl equiv in the pyrrhotite bodies; and 183 degrees-212 degrees C and 3.2-4.0 wt % NaCl equiv in the Zn-Pb ores). These values are similar to those obtained for fluid inclusions in quartz and sphalerite from the second-stage ores (187 degrees-293 degrees C and 0.2-5.2 wt % NaCl equiv in the enargite-pyrite veins: 178 degrees-265 degrees C and 0.2-7.5 wt % NaCl equiv in quartz of carbonate-replacement orebodies; 168 degrees-999 degrees C and 3-11.8 wt % NaCl equiv in sphalerite of carbonate-replacement orebodies; and 245 degrees-261 degrees C and 3.2-7.7 wt % NaCl equiv in quartz from Venencocha). Oxygen and hydrogen isotope compositions oil kaolinite from carbonate-replacement orebodies (delta(18)O = 5.3-11.5%o, delta D = -82 to -114%o) and on alunite from the Venencocha and Santa Rosa areas (delta(18)O = 1.9-6.9%o, delta D = -56 to -73%o). Oxygen isotope compositions of quartz from the first and second stages have 6180 values from 9.1 to 1.7.8 per mil. Calculated fluids in equilibrium with kaolinite have delta(18)O values of 2.0 to 8.2 and delta D values of -69 to -97 per mil; values in equilibrium with alunite are -1.4 to -6.4 and -62 to -79 per mil. Sulfur isotope compositions of sulfides from both stages have a narrow range of delta(34)S values, between -3.7 and +4.2 per mil; values for sulfates from the second stage are between 4.2 and 31.2 per mil. These results define two mixing trends for the ore-forming fluids. The first trend reflects mixing between a moderately saline (similar to 10 wt % NaCl equiv) magmatic end member that had degassed (as indicated by the low delta D values) and meteoric water. The second mixing indicates condensation of magmatic vapor with HCl and SO(2) into meteoric water, which formed alunite. The hydrothermal system at Cerro de Pasco was emplaced at a shallow depth (similar to 500 m) in the epithermal and upper part of a porphyry environment. The similar temperatures and salinities obtained for the first stage and second stages, together with the stable isotope data, indicate that both stages are linked and represent successive stages of epithermal polymetallic mineralization in the upper part of a porphyry system.

Composição mineral de maçãs 'Gala' e 'Fuji' produzidas no Sul do Brasil

O objetivo deste trabalho foi avaliar a composição mineral de maçãs 'Gala' e 'Fuji', em pomares de diferentes regiões do Sul do Brasil. Foram avaliados pomares em vários municípios de Santa Catarina e do Rio Grande do Sul, agrupados em macrorregiões denominadas de Fraiburgo, Vacaria e São Joaquim, durante o período de 1991 a 2007. Os teores médios (em matéria fresca) de Ca, K, Mg, N e P nos frutos foram, respectivamente, 47, 1.027, 52, 419 e 116 mg kg‑1, para 'Gala', e de 41, 1.043, 46, 373 e 116 mg kg‑1, para 'Fuji'. Os valores médios das relações (K+Mg)/Ca e N/Ca foram respectivamente de 24 e 9,6, para 'Gala', e de 28 e 9,7, para 'Fuji'. Maçãs 'Gala' e 'Fuji' apresentaram teores médios de Ca e P acima dos níveis críticos mínimos (40 e 100 mg kg‑1, respectivamente), e relações médias de (K+Mg)/Ca e N/Ca acima dos níveis críticos máximos (30 e 14), considerados adequados para maior conservação da qualidade pós‑colheita (QPC). Maçãs de pomares de São Joaquim apresentaram maiores teores de Ca e P, menores teores de N e menores relações (K+Mg)/Ca e N/Ca, independentemente da cultivar. O percentual de amostras, com alto risco de perdas em QPC, foi maior para 'Fuji' do que para 'Gala', quanto aos teores de Ca e P e às relações (K+Mg)/Ca e N/Ca.

Nutrição mineral da cana‑de‑açúcar irrigada com efluente de esgoto tratado, em área com aplicação de fosfogesso

O objetivo deste trabalho foi quantificar o aporte e a remoção de nutrientes em sistemas de cultivo de cana‑de‑açúcar irrigados, ou não, com efluente de estação de tratamento de esgoto (EETE), com e sem adição de fosfogesso, bem como avaliar os efeitos desses sistemas de cultivo no estado nutricional das plantas. Foram avaliados tratamentos sem irrigação e com irrigação a 100 e 150% da necessidade hídrica da cultura. Os tratamentos com fosfogesso foram aplicados em área de terceiro corte, irrigada com EETE desde o plantio. As avaliações foram realizadas em duas safras. Os tratamentos não afetaram os rendimentos de colmos. O tratamento com EETE e fosfogesso apresentou efeito sinérgico sobre o conteúdo de nitrogênio e de enxofre nas plantas. O EETE beneficiou a nutrição das plantas quanto ao fósforo, mas não causou melhorias na nutrição com potássio e enxofre. A nutrição com ferro, zinco e manganês não foi influenciada pelo aporte desses micronutrientes pelo EETE. O fósforo e o nitrogênio aportados na irrigação com EETE devem ser considerados na recomendação de adubação. Porém, potássio, enxofre, ferro, zinco e manganês do efluente não são fontes eficientes desses nutrientes para as plantas.

Migration of dissolved organic carbon in biochars and biochar-mineral complexes

The objective of this work was to determine the contribution of dissolved organic carbon (DOC) from a biochar mineral complex (BMC), so as to better understand the interactions between DOC, biochar, clay, and minerals during thermal treatment, and the effects of BMC on amended soils. The BMC was prepared by heating a mixture of a H3PO4-treated saligna biochar from Acacia saligna, clays, other minerals, and chicken manure. The BMC was applied to a sandy loam soil in Western Australia, where wheat was grown. Liquid chromatography-organic carbon detection (LC-OCD) tests were carried out on water extracts from the untreated biochar, the BMC, the BMC-amended soil, and on a control soil to measure the DOC concentration. LC-OCD tests provide a fingerprint of the DOC, which allows the fractions of DOC to be determined. Thermal processing enhanced the reaction of the A. saligna biochar with manure, clays and minerals, and affected the distribution of the DOC fractions. Notably, the process leads to immobilization of hydrophobic DOC and to an increase in the concentration of low-molecular-weight neutrals in the BMC. The application of the BMC to soil increases the DOC in the amended soil, especially the biopolymer fraction.

Bone mineral density (BMD), micro-architecture estimation (TBS) and vertebral fracture assessment (VFA) extracted from a single DXA device in combination with clinical risk factors improve significantly the identification of women at high risk of fracture.

Osteoporosis (OP) is a systemic skeletal disease characterized by a low bone mineral density (BMD) and a micro-architectural (MA) deterioration. Clinical risk factors (CRF) are often used as a MA approximation. MA is yet evaluable in daily practice by the trabecular bone score (TBS) measure. TBS is very simple to obtain, by reanalyzing a lumbar DXA-scan. TBS has proven to have diagnosis and prognosis values, partially independent of CRF and BMD. The aim of the OsteoLaus cohort is to combine in daily practice the CRF and the information given by DXA (BMD, TBS and vertebral fracture assessment (VFA)) to better identify women at high fracture risk. The OsteoLaus cohort (1400 women 50 to 80 years living in Lausanne, Switzerland) started in 2010. This study is derived from the cohort COLAUS who started in Lausanne in 2003. The main goal of COLAUS is to obtain information on the epidemiology and genetic determinants of cardiovascular risk in 6700 men and women. CRF for OP, bone ultrasound of the heel, lumbar spine and hip BMD, VFA by DXA and MA evaluation by TBS are recorded in OsteoLaus. Preliminary results are reported. We included 631 women: mean age 67.4 ± 6.7 years, BMI 26.1 ± 4.6, mean lumbar spine BMD 0.943 ± 0.168 (T-score − 1.4 SD), and TBS 1.271 ± 0.103. As expected, correlation between BMD and site matched TBS is low (r2 = 0.16). Prevalence of VFx grade 2/3, major OP Fx and all OP Fx is 8.4%, 17.0% and 26.0% respectively. Age- and BMI-adjusted ORs (per SD decrease) are 1.8 (1.2-2.5), 1.6 (1.2-2.1), and 1.3 (1.1-1.6) for BMD for the different categories of fractures and 2.0 (1.4-3.0), 1.9 (1.4-2.5), and 1.4 (1.1-1.7) for TBS respectively. Only 32 to 37% of women with OP Fx have a BMD < − 2.5 SD or a TBS < 1.200. If we combine a BMD < − 2.5 SD or a TBS < 1.200, 54 to 60% of women with an osteoporotic Fx are identified. As in the already published studies, these preliminary results confirm the partial independence between BMD and TBS. More importantly, a combination of TBS subsequent to BMD increases significantly the identification of women with prevalent OP Fx which would have been misclassified by BMD alone. For the first time we are able to have complementary information about fracture (VFA), density (BMD), micro- and macro architecture (TBS and HAS) from a simple, low ionizing radiation and cheap device: DXA. Such complementary information is very useful for the patient in the daily practice and moreover will likely have an impact on cost effectiveness analysis.

Nitrogen fluxes from irrigated common‑bean as affected by mulching and mineral fertilization

The objective of this work was to measure the fluxes of N2O‑N and NH3‑N throughout the growing season of irrigated common‑bean (Phaseolus vulgaris), as affected by mulching and mineral fertilization. Fluxes of N2O‑N and NH3‑N were evaluated in areas with or without Congo signal grass mulching (Urochloa ruziziensis) or mineral fertilization. Fluxes of N were also measured in a native Cerrado area, which served as reference. Total N2O‑N and NH3‑N emissions were positively related to the increasing concentrations of moisture, ammonium, and nitrate in the crop system, within 0.5 m soil depth. Carbon content in the substrate and microbial biomass within 0.1 m soil depth were favoured by Congo signal grass and related to higher emissions of N2O‑N, regardless of N fertilization. Emission factors (N losses from the applied mineral nitrogen) for N2O‑N (0.01-0.02%) and NH3‑N (0.3-0.6%) were lower than the default value recognized by the Intergovernmental Panel on Climate Change. Mulch of Congo signal grass benefits N2O‑N emission regardless of N fertilization.

Yield and mineral nutrition of soybean, maize, and Congo signal grass as affected by limestone and slag

The objective of this work was to evaluate the efficiency of superficial application of limestone and slag, and their effects on soil chemical attributes and on yield and mineral nutrition of soybean, maize, and Congo signal grass (Urochloa ruziziensis). The experiment was carried out in a Rhodic Hapludox under no tillage system. The treatments consisted of the use of limestone or slag (silicates of calcium and magnesium) to correct soil acidity, and of a control treatment without the use of soil correctives. Rates were calculated in order to raise soil base saturation up to 70%. Soybean was sown in November 2006 and maize in December 2007. Congo signal grass was sown right after the harvests of soybean and maize, and it was cropped during the off-seasons. Soil chemical attributes were evaluated at 6, 12, and 18 months after the application of the corrective materials. Slag is an efficient source for soil acidity correction, being able to raise the exchangeable base levels in the soil profile faster than lime. Both limestone and slag increase dry matter yield of Congo signal grass, and grain yield of soybean and maize. Slag is more effective in improving maize grain yield.

Alkaline mineral water lowers bone resorption even in calcium sufficiency: alkaline mineral water and bone metabolism.

BACKGROUND: Dietary acid charge enhances bone loss. Bicarbonate or alkali diet decreases bone resorption in humans. We compared the effect of an alkaline mineral water, rich in bicarbonate, with that of an acid one, rich in calcium only, on bone markers, in young women with a normal calcium intake. METHODS: This study compared water A (per litre: 520 mg Ca, 291 mg HCO(3)(-), 1160 mg SO(4)(-), Potential Renal Acid load (PRAL) +9.2 mEq) with water B (per litre: 547 mg Ca, 2172 mg HCO(3)(-), 9 mg SO(4)(-), PRAL -11.2 mEq). 30 female dieticians aged 26.3 yrs (SD 7.3) were randomized into two groups, followed an identical weighed, balanced diet (965 mg Ca) and drank 1.5 l/d of the assigned water. Changes in blood and urine electrolytes, C-telopeptides (CTX), urinary pH and bicarbonate, and serum PTH were measured after 2 and 4 weeks. RESULTS: The two groups were not different at baseline, and showed a similar increase in urinary calcium excretion. Urinary pH and bicarbonate excretion increased with water B, but not with water A. PTH (p=0.022) and S-CTX (p=0.023) decreased with water B but not with water A. CONCLUSION: In calcium sufficiency, the acid calcium-rich water had no effect on bone resorption, while the alkaline water rich in bicarbonate led to a significant decrease of PTH and of S-CTX.

Prevalence and characteristics of vitamin or dietary supplement users in Lausanne, Switzerland: the CoLaus study.

BACKGROUND AND OBJECTIVES: Vitamin+mineral supplement (VMS) and dietary supplement (DS) use is widespread in the general population, but the motivations for such use are poorly known. The prevalence and characteristics of VMS and DS users in Lausanne, Switzerland, were thus assessed. METHOD: Cross-sectional study was performed including 3249 women and 2937 men (CoLaus study). VMS were defined as single or multivitamin-multimineral preparations. DS included omega-3 or omega-6 fatty acids, herbal teas, plant or animal extracts and bacterial (Lactobacillus) preparations. Calcium and iron supplements were assessed separately. RESULTS: Twenty-six percent of the subjects reported using VMS or DS. VMS were the most frequently consumed item (16.8%), followed by DS (10%), calcium (6.6%) and iron (1.8%). Women reported a higher consumption than men. In women, VMS, DS and calcium use increased and iron use decreased with age, whereas in men only VMS and calcium intake increased with age. Multivariate analysis showed female gender, being born in Switzerland, increased age, higher education and increased physical activity to be positively related with VMS and DS. On bivariate analysis, VMS and DS users presented more frequently with arthritis, anxiety, depression and osteoporosis, but on multivariate analysis only positive relationships between DS use and anxiety/depression (odds ratio (OR)=1.40; 95% confidence interval (CI): [1.16-1.70]) and calcium and osteoporosis (OR=10.6; 95% CI [7.77-14.4]) were found. CONCLUSION: VMS and DS use is common in the population of Lausanne and associated with a better health profile. Calcium supplements are taken to prevent osteoporosis, whereas the rationale for taking other VMS and DS is unclear.

Dry matter accumulation and mineral nutrition of arracacha in response to nitrogen fertilization

Abstract:The objective of this work was to evaluate the effect of nitrogen fertilization on the growth and yield of arracacha (Arracacia xanthorrhiza), as well as on the plant's nutrient uptake, distribution, and removal. The experiment was carried out in a typical Oxisol, with sandy texture. A randomized complete block design was used, with four replicates. The treatments consisted of five N rates: 0, 50, 100, 200, and 400 kg ha-1. The plots were composed of three 8-m-length rows, spaced at 0.60 m between rows and 0.40 m between plants. The plants were harvested after an 8-month cycle. Nitrogen fertilization significantly increased the proportion of N and S accumulated in stems, and of Ca, Mg, Fe, and Mn in leaves. N supply increased Zn distribution to stems and leaves, whereas high N rates increased Cu allocation to stems more than to the rootstock. High N rates increase plant dry matter (DM) production and nutrient uptake and removal, but do not result in the greatest yield due to the greater development of leaves and stems, and to the lower allocation of DM in storage roots.

CRESCIMENTO DE MUDAS DE CAJUEIRO-ANÃO-PRECOCE 'CCP¾ 76' SUBMETIDAS À ADUBAÇÃO ORGÂNICA E MINERAL

A adição de doses de matéria orgânica e fertilizante mineral ao substrato, para a produção de mudas em recipientes é uma técnica bastante utilizada nos sistemas modernos de produção de mudas. Contudo, para a cultura do cajueiro são poucas as informações que definam passíveis doses de matéria orgânica e fertilizantes minerais capazes de produzirem mudas vigorosas a curtos intervalos de tempo. Durante a fase de produção de mudas de cajueiro-anão-precoce 'CCP 76', conduziu-se um ensaio na área experimental do Departamento de Irrigação e Drenagem da Universidade Federal do Ceará em Fortaleza, Ceará, no período de abril a junho de 1995. Utilizou-se como substrato à camada arável (0-30cm) de um Podzólico Vermelho-Amarelo Distrófico, textura média. Para o plantio, utilizaram-se sementes oriundas de um único genótipo de cajueiro- anão-precoce progênie 'CCP 76'. Os tratamentos constaram da aplicação de quatro doses de matéria orgânica (0; 100; 200 e 300 cm³/2,5 Kg solo) e quatro doses da mistura mineral (0; 1,92; 3,34 e 6,18 g) contendo uréia, superfosfato triplo, cloreto de potássio, gesso, calcário e fritas tipo MIB-3. O delineamento experimental utilizado foi o inteiramente casualizado, com 16 tratamentos, em 4 repetições, seguindo o modelo fatorial 4². Foram realizadas as seguintes determinações: altura de planta (cm), diâmetro do caule (mm), número de folha/planta, comprimento da raiz principal (cm), peso da matéria seca da parte aérea e do sistema radicular (g/planta). Os resultados enfatizam que a aplicação de doses combinadas de matéria orgânica e fertilizante mineral promoveu acréscimos significativos sobre a altura da planta, peso da matéria seca da parte aérea e número de folhas.

CIANAMIDA HIDROGENADA, THIDIAZURON E ÓLEO MINERAL NA QUEBRA DA DORMÊNCIA E NA PRODUÇÃO DO PESSEGUEIRO cv. CHIRIPÁ

Este trabalho foi realizado no ano de 1999, na Estação Experimental Agronômica da Universidade Federal do Rio Grande do Sul, localizada no município de Eldorado do Sul, Estado do Rio Grande do Sul, latitude 30°05'52" S, longitude 51°39'08" W e altitude de 46 metros. Foram testados os efeitos da Cianamida Hidrogenada (C.H.) e Óleo Mineral (O.M.) em mistura, Óleo Mineral (O.M.) e Thidiazuron (TDZ) com Óleo Mineral (O.M.), sobre brotação, frutificação, produção e antecipação de colheita. Os tratamentos foram aplicados quando as plantas estavam no estádio fenológico A. Foram testados os seguintes tratamentos: C.H. 0,5%, 1,0% e 1,5% + O.M 1,0%, O.M. 1,0% e 2,0%, TDZ 200 e 400 ppm + O.M. 2,0% e testemunha (sem pulverização). Os tratamentos não anteciparam a brotação das gemas vegetativas. O tratamento C.H. 1,5% com O.M. 1,0% proporcionou produção suficiente para viabilizar o cultivo do "Chiripá" em condições de inverno ameno, mas não houve diferenças significativas no peso médio dos frutos. O TDZ, nas dosagens testadas, não se mostrou eficiente na quebra de dormência desta cultivar. Não houve efeito na antecipação da colheita.

Composição mineral da folha em abacaxizeiro: efeito da parte da folha analisada

A padronização da amostragem para a análise foliar em abacaxizeiros é importante para a obtenção de resultados confiáveis. Neste aspecto, este trabalho visa a esclarecer a variação da composição mineral da folha de abacaxi, em plantas desenvolvidas em solo arenoso, sem irrigação. As folhas foram coletadas, limpas e divididas em 4 porções: aclorofilada, basal, mediana e apical. Após a secagem, as amostras foram pesadas, submetidas à digestão e analisadas pela metodologia adequada a cada nutriente. Uma grande variação no teor dos nutrientes foi encontrada ao longo da folha de abacaxi. Uma comparação confiável pode ser estabelecida entre as análises feitas com a folha inteira e a porção clorofilada da folha; o mesmo já não pode ser dito para a porção aclorofilada. Assim, este trabalho vem confirmar a necessidade da padronização da amostragem.

Efeito da aplicação de cianamida hidrogenada e óleo mineral na quebra de dormência e producão do pessegueiro-'Flamecrest'

Com o objetivo de aumentar a produção e qualidade de frutos do pessegueiro- 'Flamecrest', de alta exigência em frio, realizou-se um experimento no Município de Farroupilha-RS, no ano de 2000, com o uso de cianamida hidrogenada e óleo mineral. Estudou-se o efeito de duas diferentes épocas de aplicação dos tratamentos (15-7 e 2-8) sobre a brotação, floração, frutificação, produção e antecipação de colheita. Foram testados os efeitos dos seguintes tratamentos: cianamida hidrogenada (C.H.) 1,22; 2,45; 3,675 e 4,90 g de i.a.L-1 com óleo mineral (O.M.) 10 g de i.a.L-1; O.M. 10 g de i.a.L-1 isolado e testemunha (sem pulverização). Os tratamentos não anteciparam a brotação das gemas floríferas, porém C.H. 2,45 e 4,90 g de i.a.L-1 com O.M. a 10 g de i.a.L-1 proporcionaram plantas com maior brotação das gemas vegetativas. Não houve efeito marcante dos tratamentos sobre a floração e a porcentagem de frutos vingados nas duas épocas. O número de frutos raleados por planta foi superior para os tratamentos com C.H. 2,45 e 4,90 g de i.a.L-1 com O.M. 10 g de i.a.L-1 quando aplicados na segunda época. Já, para o número e massa total dos frutos colhidos, destacaram-se, na primeira época (15-7), os tratamentos com C.H. 1,22 e 3,675 g de i.a.L-1 + O.M. 10 g de i.a.L-1 e, na segunda época (2-8), os tratamentos com C.H. 2,45 e 4,90 g de i.a.L-1 + O.M. 10 g de i.a.L-1. Os tratamentos da segunda época resultaram em produções médias superiores à primeira. A massa média dos frutos não foi alterada de forma clara pelos tratamentos, assim como o teor de sólidos solúveis totais e a resistência de polpa.