Datação da fração humina da matéria orgânica do solo e sua comparação com idades 14C de carvões fósseis

The radiocarbon dating of the soil organic matter (SOM) is a polemic subject, due mainly to the complexity of the formation of the soils and to the variable contamination from several sources. Soil samples from 4 different Brazilian localities were submitted to physical and chemical pre-treatment for the extraction of humin fraction, which is the most stable organic compound and theoretically the oldest and representative of the age of the SOM. The radiocarbon dating obtained from the total SOM and their humin fractions are compared to the 14C ages from buried charcoals at similar depths. The radiocarbon ages obtained from such charcoals are, in most of the cases, concordant within the experimental errors of those obtained on humin fractions, or are in average 10% higher, with one exception. Thus, the ages on humin fractions could be assumed as the minimum ages for the associated soils, while the results obtained on total SOM, even at depths until 200 cm, exhibit pronounced contamination effect by modern carbon, rejuvenating their ages.

Persistência e lixiviação do herbicida simazina em solo barrento cultivado com milho

Foram determinadas, em experimento de campo, a persistência e a lixiviação do herbicida simazina na dose de 3 kg/ ha i. a. em um solo podzol vermelho-amarelo de textura barrenta plantado com milho, por meio do monitoramento de seus resíduos, durante um ano após a sua aplicação, em 14 de janeiro de 1992. O experimento foi conduzido na Estação Experimental do Instituto Biológico, Campinas, SP, utilizando-se o método de cromatografia gasosa para a determinação analítica de resíduos. Empregou-se o fatorial 8 X 5, "épocas de amostragem do solo" X "profundidades de amostragem", quatro repetições para os procedimentos experimentais no campo, reduzidas para duas nas de terminações analíticas. Os resultados demonstraram que a maior concentração do herbicida localizou-se na camada superficial do solo (0-10 cm de profundidade), onde persistiu até 360 dias após o tratamento na concentração de 0,08 mg/kg de solo. A curva de persistência do produto, para a profundidade de 010 cm , foi representada por uma equação exponencial do terceiro grau. Foram encontrados resíduos de simazina nas camadas de solo à profundidades de 10 -20, 20 -30 e 30-40 cm até 1 8 3 , 6 5 e 6 5 dias após o tratamento, respectivamente.

Comparative uptake and metabolism of 2-[14C]-2,4-dichlorophenoxyacetic acid in callus cultures of monocot (Dioscorea spp.) and dicot (Nicotiana tabacum L.) plants

(Comparative uptake and metabolism of 2-[14C]-2,4-dichlorophenoxyacetic acid in callus cultures of monocot (Dioscorea spp.) and dicot (Nicotiana tabacum L.) plants). The uptake and metabolism of 2-[14C]-2,4-dichlorophenoxyacetic acid (2,4-D) were investigated in leaf calluses of Nicotiana tabacum, tuber calluses of Dioscorea opposita and calluses derived from zygotic embryos, leaves and petioles of Dioscorea composita. Striking similarities were evident in the patterns of 2,4-D metabolites and their chemical characteristics in the three callus types of D. composita compared, but significant differences were detected among the patterns of rnetabolites in the three species studied. Preliminary investigations on the stability of various metabolites (separated using TLC) by hydrolysis showed that sugar esters appeared to be the major metabolites in tobacco whilst in yams (D. opposita) glycosides were shown to be the main ones, which indicated a similarity between plants of Gramineae and Dioscoreaceae in terms of 2,4-D metabolism. Release of 2,4-D from tobacco callus cells upon their transfer to 2,4-D-free medium was detected and the implications of this are discussed in relation to the cultural conditions necessary to induce morphogenesis in vitro.

CO2:n adsorptio Loviisan voimalaitoksen päästöilmasta 14C-päästöjen määrittämiseksi

Tämän kandidaatintyön tavoitteena oli selvittää mahdollisuuksia 14C:n kemiallisten muotojen eriyttämiseen käyttäen Loviisan voimalaitoksella olemassa olevaa näytteenkeräyslaitteistoa. Lisäksi tarkoituksena oli selvittää parhaiten tähän käyttötarkoitukseen soveltuva zeoliittityyppiä tyypeistä 4A, 5A ja 13X. Työn kirjallisessa osassa käsitellään ydinvoimalaitoksen C14-päästöjä keskittyen pääosin Loviisan VVER-laitokseen. Adsorption osalta esitellään kaupallisesti käytettyjä adsorptiomateriaaleja ja paneudutaan adsorptioon fysikaalisena ja kemiallisena ilmiönä. Lisäksi esitellään kahden desorptiomenetelmän perusperiaatteet. Kirjallisen osan lopussa kootaan tutkimukseen vaikuttavia tekijöitä ja esitellään aiemmin käytössä ollut näytteenkeräyslaitteisto. Kokeellisessa osassa esitellään työssä käytetyt laitteistot. Lisäksi on kuvattu mittausten suoritus nestetuikelaskurilla. Tämän jälkeen työssä esitellään mittaustuloksien käsittely ja näin saadut tulokset.

Comparison of the efficacy of biodegradable and non-biodegradable scintillation liquids on the counting of tritium- and [14C]-labeled compounds

The widespread use of ³H and 14C in research has generated a large volume of waste mixed with scintillation liquid, requiring an effective control and appropriate storage of liquid radioactive waste. In the present study, we compared the efficacy of three commercially available scintillation liquids, Optiphase HiSafe 3, Ultima-Gold™ AB (biodegradable) and Insta-Gel-XF (non-biodegradable), in terms of [14C]-glucose and [³H]-thymidine counting efficiency. We also analyzed the effect of the relative amount of water (1.6 to 50%), radioisotope concentration (0.1 to 100 nCi/ml), pH (2 to 10) and color of the solutions (samples containing 0.1 to 1.0 mg/ml of Trypan blue) on the counting efficiency in the presence of these scintillation liquids. There were few significant differences in the efficiency of 14C and ³H counting obtained with biodegradable or non-biodegradable scintillation liquids. However, there was an 83 and 94% reduction in the efficiency of 14C and ³H counting, respectively, in samples colored with 1 mg/ml Trypan blue, but not with 0.1 mg/ml, independent of the scintillation liquid used. Considering the low cost of biodegradable scintillation cocktails and their efficacy, these results show that traditional hazardous scintillation fluids may be replaced with the new safe biodegradable fluids without impairment of ³H and 14C counting efficiency. The use of biodegradable scintillation cocktails minimizes both human and environmental exposure to hazardous solvents. In addition, some biodegradable scintillation liquids can be 40% less expensive than the traditional hazardous cocktails.

The effect of nitrate fertilization on the distribution of exported 14c-photosynthate in nodulated soybean (Glycine max (L.) Merr.) plants

Soybean (Glycine ~ (L.) Merr. cv. Harosoy 63) plants inoculated with Rhizobium japonicum were grown in vermiculite in the presence or absence of nitrate fertilization for up to 6 weeks after planting. Overall growth of nodulated plants was enhanced in the presence of nitrate fertilization, while the extent of nodule development was reduced. Although the number of nodules was not affected by nitrate fertilization when plants were grown at a light intensity limiting for photosynthesis, at light intensities approaching or exceeding the light saturation point for photosynthesis, nitrate fertilization resulted in at least a 30% reduction in nodule numbers. The mature, first trifoliate leaf of 21 day old plants was allowed to photoassimi1ate 14C02. One hour after·· the initial exposure to 14C02, the , plants were harvested and the 14C radioactivity was determined in the 80% ethanol-soluble fraction: in. o:rider to assess· "the extent of photoassimilate export and the pattern of distribution of exported 14C. The magnitude of 14C export was not affected by the presence of nitrate fertilization. However, there was a significant effect on the distribution pattern, particularly with regard to the partitioning of 14C-photosynthate between the nodules and the root tissue. In the presence of nitrate fertilization, less than 6% of the exported 14C photosynthate was recovered from the nodules, with much larger amounts (approximately 37%) being recovered from the root tissue. In the absence of nitrate fertilization, recovery of exported 14C-photosynthate from the nodules (19 to 27%) was approximately equal to that from the root tissue (24 to 33%). By initiating- or terminating the applications of nitrate at 14 days of age, it was determined that the period from day 14 to day 21 after planting was particularly significant for the development of nodules initiated earlier. Addition of nitrate fertilization at this time inhibited further nodule development while stimulating plant growth, whereas removal of nitrate fertilization stimulated nodule development. The results obtained are consistent with the hypothesis that nodule development is inhibited by nitrate fertilization through a reduction in the availability of photosynthate to the nodules.

Der Einfluss von Neuropeptid Y auf die Glukoseaufnahme im dorsalen Tectum opticum während visueller Stimulation der Unke Bombina orientalis: Quantitative Analyse mit Hilfe der 14C-2-Desoxiglukose-Technik

(1) Neuropeptid Y (NPY), einer der häufigsten peptidergen Neurotransmitter im zentralen und peripheren Nervensystem der Säuger, ist an der Steuerung zahlreicher physiologischer Prozesse beteiligt. Auch Amphibien weisen eine verstärkte NPY-Immunreaktivität im Zentralnervensystem auf. Im Hinblick auf bereits gewonnene Erkenntnisse sollte in der vorliegenden Arbeit eine Modulierbarkeit retino-tectaler Aktivität durch Neuropeptid Y an der chinesischen Rotbauchunke (Bombina orientalis) überprüft und erstmals mit Hilfe der 14[C]-2-Desoxiglukose-Methode (14C-2DG) (Sokoloff et al. 1977) quantitativ analysiert werden. Als Vergleichstier diente die Agakröte (Bufo marinus). Zur Darstellung eines möglichen Effektes auf das Tectum opticum wurde NPY lokal auf die tectale Oberfläche visuell stimulierter Rotbauchunken appliziert. Mit Hilfe der 14C-2DG-Methode und den daraus autoradiographisch ermittelten Daten konnten die zerebralen Aktivitäten visualisiert, quantitativ ausgewertet und miteinander verglichen werden. In einer weiteren Versuchsreihe wurde hinterfragt, welche inhibitorische Wirkung NPY entwickeln kann, wenn zuvor der retinale Input pharmakologisch durch systemische Gabe von Apomorphin (APO) signifikant erhöht wurde. (2) Die 14C-2DG-Methode erlaubt einen Blick in die funktionale Aktivität des Gehirns und ermöglicht es, regional ablaufende physiologische und biochemische Energiestoffwechselprozesse innerhalb des Gehirns quantitativ zu erfassen. Mit Hilfe der 14C-2DG-Methode werden die neuromodulatorischen Wirkungen von NPY kartiert und analysiert. (3) Versuchstiergruppe 1 – Bombina orientalis – unbehandelt Zur Beurteilung pharmakologischer Effekte durch NPY bzw. APO auf den Hirnmetabolismus war es zunächst erforderlich, die Gehirnaktivitäten pharmakologisch unbeeinflusster Tiere nach visueller Reizgabe zu untersuchen. Im Bereich des medialen Mesencephalon wurden die tectalen 14C-2DG-Konzentrationen über zehn Messreihen pro Einzeltier sowohl an der rechten als auch an der linken tectalen Hälfte auf Höhe des ventrolateralen Tectum opticum ermittelt. Beim rechts-links Vergleich zeigen sich gleich verteilte Strahlungsintensitäten. Basierend auf dieser Aussage konnte NPY unilateral auf die tectale Oberfläche aufgebracht und auf seine Wirkung geprüft werden. (4) Versuchstiergruppe 2 – Bombina orientalis – NPY-Applikation Der unilaterale Einsatz von NPY auf die tectale Oberfläche des Versuchstieres bewirkt, dass die unter dem Einfluss von NPY stehende tectale Hälfte, im Gegensatz zur unbehandelten tectalen Hälfte, einen deutlich niedrigeren 14C-2DG-Gebrauch aufweist. Besonders in den oberen Schichten des Tectum opticum (Layer 9) zeigt die 14C-2DG-Methode qualitativ und quantitativ auswertbare Aktivitätsminderungen an. (5) Verhalten unter NPY: Durchschnittlich nach 10 min Versuchsdauer zeigt Bombina orientalis eine deutliche Abnahme in der Beutefangaktivität, die sich gegen Ende der Versuchszeit noch weiter reduziert. (6) Versuchstiergruppe 3 – Bombina orientalis – APO-Applikation Systemisch verabreichtes APO führt bei Bombina orientalis zu einer Verstärkung des retinalen Ausganges in die retino-tectalen Projektionsfelder. Die neuronalen Aktivitäten im Tectum opticum erhöhen sich unter dem Einfluss von APO im Durchschnitt um 40% im Vergleich zu APO-unbehandelten Tieren. (7) Verhalten unter APO: Bombina orientalis zeigt nach systemischer Applikation von APO keine verstärkten stereotypen Schnappreaktionen. Die Tiere reagieren ausschließlich mit Akinese, d.h. einem Ausfall gerichteter Lokomotionen und Orientierungsbewegungen. (8) Versuchstiergruppe 4 – Bombina orientalis – APO/NPY-Applikation Die durch systemisch verabreichtes APO erhöhten retino-tectalen Aktivitäten im Tectum opticum werden unter dem unilateralen Einsatz von NPY deutlich abgeschwächt. Eindeutig niedrigere 14C-2DG-Aufnahmen sind in den oberen Schichten des Tectum opticum messbar, was die starke Wirkung von NPY quantitativ belegt. (9) Versuchstiergruppe 2 – Bufo marinus – NPY-Applikation Der unilaterale Einsatz von NPY auf die tectale Oberfläche von Bufo marinus zeigt ebenfalls, dass die unter dem Einfluss von NPY stehende tectale Hälfte, im Gegensatz zur unbehandelten tectalen Hälfte, einen deutlich niedrigeren 14C-2DG-Gebrauch aufweist. Bufo marinus zeigt aber aufgrund erweiterter Versuchsbedingungen (On-Off-Beleuchtungswechsel) anders verteilte Strahlungsintensitäten über dem Tectum-Querschnitt als Bombina orientalis. Stärkere [14C]-Akkumulationen zeigen sich in den tieferen zentralen Schichten des Tectum opticum. (10) Versuchstiergruppe 4 – Bufo marinus – APO/NPY-Applikation Auch die durch systemisch verabreichtes APO erhöhten retino-tectalen Aktivitäten im Tectum opticum von Bufo marinus werden unter dem unilateralen Einsatz von NPY deutlich abgeschwächt. (11) Die Ergebnisse der vorliegenden Arbeit leisten einen Beitrag zum Einfluss von NPY auf den retino-tectalen Informationstransfer bei Anuren im Sinne einer praetecto-tectalen inhibitorischen Modulation. Im Einklang mit früheren neuroanatomischen, immuncytochemischen und elektro-physiologischen Befunden liefern diese Ergebnisse erstmals ein biochemisches Korrelat auf der Basis des tectalen Energiestoffwechsels. (12) Es ist hervorzuheben, dass NPY-vermittelte inhibitorische Modulationen visuellen Informationstransfers in der vorliegenden Arbeit an Bombina orientalis nachgewiesen wurden, die phylogenetisch zu den ältesten Anuren (Anamnioten) gehört. Vergleichbares ist an verschiedenen Amnioten – einschließlich Primaten – beschrieben worden, was darauf hinweist, dass solche NPY-vermittelten Prozesse sich innerhalb der Tetrapoden relativ früh herausgebildet haben und in der Evolution konserviert worden sind.

Pollen-based reconstructions of biome distributions for Australia, Southeast Asia and the Pacific (SEAPAC region) at 0,6000 and 18,000 14C yr B.P.

Aim  This paper documents reconstructions of the vegetation patterns in Australia, Southeast Asia and the Pacific (SEAPAC region) in the mid-Holocene and at the last glacial maximum (LGM). Methods  Vegetation patterns were reconstructed from pollen data using an objective biomization scheme based on plant functional types. The biomization scheme was first tested using 535 modern pollen samples from 377 sites, and then applied unchanged to fossil pollen samples dating to 6000 ± 500 or 18,000 ± 1000 14C yr bp. Results  1. Tests using surface pollen sample sites showed that the biomization scheme is capable of reproducing the modern broad-scale patterns of vegetation distribution. The north–south gradient in temperature, reflected in transitions from cool evergreen needleleaf forest in the extreme south through temperate rain forest or wet sclerophyll forest (WSFW) and into tropical forests, is well reconstructed. The transitions from xerophytic through sclerophyll woodlands and open forests to closed-canopy forests, which reflect the gradient in plant available moisture from the continental interior towards the coast, are reconstructed with less geographical precision but nevertheless the broad-scale pattern emerges. 2. Differences between the modern and mid-Holocene vegetation patterns in mainland Australia are comparatively small and reflect changes in moisture availability rather than temperature. In south-eastern Australia some sites show a shift towards more moisture-stressed vegetation in the mid-Holocene with xerophytic woods/scrub and temperate sclerophyll woodland and shrubland at sites characterized today by WSFW or warm-temperate rain forest (WTRF). However, sites in the Snowy Mountains, on the Southern Tablelands and east of the Great Dividing Range have more moisture-demanding vegetation in the mid-Holocene than today. South-western Australia was slightly drier than today. The single site in north-western Australia also shows conditions drier than today in the mid-Holocene. Changes in the tropics are also comparatively small, but the presence of WTRF and tropical deciduous broadleaf forest and woodland in the mid-Holocene, in sites occupied today by cool-temperate rain forest, indicate warmer conditions. 3. Expansion of xerophytic vegetation in the south and tropical deciduous broadleaf forest and woodland in the north indicate drier conditions across mainland Australia at the LGM. None of these changes are informative about the degree of cooling. However the evidence from the tropics, showing lowering of the treeline and forest belts, indicates that conditions were between 1 and 9 °C (depending on elevation) colder. The encroachment of tropical deciduous broadleaf forest and woodland into lowland evergreen broadleaf forest implies greater aridity. Main conclusions  This study provides the first continental-scale reconstruction of mid-Holocene and LGM vegetation patterns from Australia, Southeast Asia and the Pacific (SEAPAC region) using an objective biomization scheme. These data will provide a benchmark for evaluation of palaeoclimate simulations within the framework of the Palaeoclimate Modelling Intercomparison Project.

Pollen-based reconstructions of Japanese biomes at 0, 6000 and 18,000 14C yr bp

A biomization method, which objectively assigns individual pollen assemblages to biomes ( Prentice et al., 1996 ), was tested using modern pollen data from Japan and applied to fossil pollen data to reconstruct palaeovegetation patterns 6000 and 18,000 14C yr bp Biomization started with the assignment of 135 pollen taxa to plant functional types (PFTs), and nine possible biomes were defined by specific combinations of PFTs. Biomes were correctly assigned to 54% of the 94 modern sites. Incorrect assignments occur near the altitudinal limits of individual biomes, where pollen transport from lower altitudes blurs the local pollen signals or continuous changes in species composition characterizes the range limits of biomes. As a result, the reconstructed changes in the altitudinal limits of biomes at 6000 and 18,000 14C yr bp are likely to be conservative estimates of the actual changes. The biome distribution at 6000 14C yr bp was rather similar to today, suggesting that changes in the bioclimate of Japan have been small since the mid-Holocene. At 18,000 14C yr bp the Japanese lowlands were covered by taiga and cool mixed forests. The southward expansion of these forests and the absence of broadleaved evergreen/warm mixed forests reflect a pronounced year-round cooling.

Pollen-based biomes for Beringia 18,000, 6000 and 0 14C yr B.P.

The objective biomization method developed by Prentice et al. (1996) for Europe was extended using modern pollen samples from Beringia and then applied to fossil pollen data to reconstruct palaeovegetation patterns at 6000 and 18,000 14C yr bp. The predicted modern distribution of tundra, taiga and cool conifer forests in Alaska and north-western Canada generally corresponds well to actual vegetation patterns, although sites in regions characterized today by a mosaic of forest and tundra vegetation tend to be preferentially assigned to tundra. Siberian larch forests are delimited less well, probably due to the extreme under-representation of Larix in pollen spectra. The biome distribution across Beringia at 6000 14C yr bp was broadly similar to today, with little change in the northern forest limit, except for a possible northward advance in the Mackenzie delta region. The western forest limit in Alaska was probably east of its modern position. At 18,000 14C yr bp the whole of Beringia was covered by tundra. However, the importance of the various plant functional types varied from site to site, supporting the idea that the vegetation cover was a mosaic of different tundra types.

Inverse modeling of the 14C bomb pulse in stalagmites to constrain the dynamics of soil carbon cycling at selected European cave sites

The decomposition of soil organic matter (SOM) is temperature dependent, but its response to a future warmer climate remains equivocal. Enhanced rates of decomposition of SOM under increased global temperatures might cause higher CO2 emissions to the atmosphere, and could therefore constitute a strong positive feedback. The magnitude of this feedback however remains poorly understood, primarily because of the difficulty in quantifying the temperature sensitivity of stored, recalcitrant carbon that comprises the bulk (>90%) of SOM in most soils. In this study we investigated the effects of climatic conditions on soil carbon dynamics using the attenuation of the 14C ‘bomb’ pulse as recorded in selected modern European speleothems. These new data were combined with published results to further examine soil carbon dynamics, and to explore the sensitivity of labile and recalcitrant organic matter decomposition to different climatic conditions. Temporal changes in 14C activity inferred from each speleothem was modelled using a three pool soil carbon inverse model (applying a Monte Carlo method) to constrain soil carbon turnover rates at each site. Speleothems from sites that are characterised by semi-arid conditions, sparse vegetation, thin soil cover and high mean annual air temperatures (MAATs), exhibit weak attenuation of atmospheric 14C ‘bomb’ peak (a low damping effect, D in the range: 55–77%) and low modelled mean respired carbon ages (MRCA), indicating that decomposition is dominated by young, recently fixed soil carbon. By contrast, humid and high MAAT sites that are characterised by a thick soil cover and dense, well developed vegetation, display the highest damping effect (D = c. 90%), and the highest MRCA values (in the range from 350 ± 126 years to 571 ± 128 years). This suggests that carbon incorporated into these stalagmites originates predominantly from decomposition of old, recalcitrant organic matter. SOM turnover rates cannot be ascribed to a single climate variable, e.g. (MAAT) but instead reflect a complex interplay of climate (e.g. MAAT and moisture budget) and vegetation development.

Degradação de 14C-atrazina em solo sob condições semicontroladas

Coordenação de Aperfeiçoamento de Pessoal de Nível Superior (CAPES)

Efeito da idade sobre a fertilidade de éguas inseminadas com sêmen diluído, resfriado a 14ºC e transportado

Para estudar o efeito da idade sobre características ovulatórias e de fertilidade, 147 ciclos estrais de 99 éguas foram agrupados em classes por idade (1 - 3-6 anos; 2 - 7-10 anos; 3 - 11-14 anos; e 4 - 15-19 anos), de acordo com o ano do nascimento. As éguas foram inseminadas com sêmen diluído, resfriado e transportado de apenas um garanhão, três vezes por semana (segundas, quartas e sextas-feiras).O controle folicular, por meio da palpação retal, e a rufiação foram realizados diariamente, durante todo o período experimental. Utilizou-se, para o transporte, o sêmen diluído no diluidor de leite desnatado-glicose no conteiner Celle modificado, sendo a dose inseminante de 400 x 10(6) espermatozóides móveis, no momento da diluição final, pré-resfriamento. O tempo médio da coleta do sêmen à inseminação artificial foi de 3,5 horas e a temperatura final do sêmen, no momento da inseminação, de 14ºC. Não houve influência da idade sobre a velocidade de crescimento folicular e o tamanho do folículo ovulatório. A fertilidade decaiu após os 15 anos de idade, traduzida pela diminuição da taxa de concepção/ciclo e eficiência de prenhez, entretanto, não foram observadas características indicativas de senescência até os 19 anos de idade.

Efeito do número de inseminações artificiais sobre a fertilidade de éguas inseminadas com sêmen diluído, resfriado a 14ºC e transportado

Estudou-se o efeito do número de inseminações sobre a fertilidade de éguas inseminadas, três vezes/semana (segundas, quartas e sextas-feiras), com sêmen diluído, resfriado e transportado, de apenas um garanhão. As éguas foram inseminadas a partir da detecção, pela palpação retal, de um folículo de 3,0 a 3,5 cm de diâmetro, em um dos ovários, até a ovulação. Utilizaram-se para o transporte o sêmen diluído no diluidor leite desnatado-glicose e o conteiner Celle modificado, sendo a dose inseminante de 400 x 10(6) espermatozóides móveis, no momento da diluição final, pré-resfriamento. de acordo com o número de inseminações artificiais (IA) utilizadas/ciclo, os resultados de 148 ciclos, de 100 éguas, foram agrupados em: 1 IA, 2IA, 3 IA e 4 ou mais IA. A eficiência de prenhez foi de 4,29; 5,04; 5,67; e 3,43, para 1, 2, 3 e 4 ou mais IA, respectivamente. As características foliculares diferiram em relação à freqüência de inseminações com os maiores valores observados no grupo de éguas inseminadas quatro ou mais vezes. Concluiu-se que menor velocidade de crescimento folicular e maior diâmetro do folículo ovulatório estiveram associados a maior número de inseminações artificiais/ciclo. Na presença de uma concentração espermática adequada, o número de inseminações/ciclo não exerceu influência sobre a fertilidade.