Efficacy of low-level laser therapy on scar tissue

Background: Physiotherapy has a very important role in the maintenance of the integumentary system integrity. There is very few evidence in humans. Nevertheless, there are some studies about tissue regeneration using low-level laser therapy (LLLT). Aim: To analyze the effectiveness of LLLT on scar tissue. Methods: Seventeen volunteers were stratified by age of their scars, and then randomly assigned to an experimental group (EG) — n = 9 – and a placebo group (PG) – n = 8. Fifteen sessions were conducted to both the groups thrice a week. However, in the PG, the laser device was switched off. Scars’ thickness, length, width, macroscopic aspect, pain threshold, pain perception, and itching were measured. Results: After 5 weeks, there were no statistically significant differences in any variable between both the groups. However, analyzing independently each group, EG showed a significant improvement in macroscopic aspect (p = 0.003) using LLLT. Taking into account the scars’ age, LLLT showed a tendency to decrease older scars’ thickness in EG. Conclusion: The intervention with LLLT appears to have a positive effect on the macroscopic scars’ appearance, and on old scars’ thickness, in the studied sample. However, it cannot be said for sure that LLLT has influence on scar tissue.

Short- and medium-term effects of manual therapy on cervical active range of motion and pressure pain sensitivity in latent myofascial pain of the upper trapezius muscle: a randomized controlled trial

Objective: The purpose of this study was to investigate effects of different manual techniques on cervical ranges of 17 motion and pressure pain sensitivity in subjects with latent trigger point of the upper trapezius muscle. 18 Methods: One hundred seventeen volunteers, with a unilateral latent trigger point on upper trapezius due to computer 19 work, were randomly divided into 5 groups: ischemic compression (IC) group (n = 24); passive stretching group (n = 20 23); muscle energy technique group (n = 23); and 2 control groups, wait-and-see group (n = 25) and placebo group 21 (n = 22). Cervical spine range of movement was measured using a cervical range of motion instrument as well as 22 pressure pain sensitivity by means of an algometer and a visual analog scale. Outcomes were assessed pretreatment, 23 immediately, and 24 hours after the intervention and 1 week later by a blind researcher. A 4 × 5 mixed repeated- 24 measures analysis of variance was used to examine the effects of the intervention and Cohen d coefficient was used. 25 Results: A group-by-time interaction was detected in all variables (P b .01), except contralateral rotation. The 26 immediate effect sizes of the contralateral flexion, ipsilateral rotation, and pressure pain threshold were large for 3 27 experimental groups. Nevertheless, after 24 hours and 1 week, only IC group maintained the effect size. 28 Conclusions: Manual techniques on upper trapezius with latent trigger point seemed to improve the cervical range of 29 motion and the pressure pain sensitivity. These effects persist after 1 week in the IC group. (J Manipulative Physiol 301 Ther 2013;xx:1-10)

Plaster body wrap: effects on abdominal fat

Background Abdominal fat is associated with metabolic disorders, leading to cardiovascular risk factors and numerous diseases. This study aimed to analyze the effect of plaster body wrap in combination with aerobic exercise on abdominal fat. Methods Nineteen female volunteers were randomly divided into intervention group (IG; n = 10) performing aerobic exercise with plaster body wrap, and control group (CG; n = 9) performing only exercise. Subcutaneous and visceral fat were measured using ultrasound; subcutaneous fat was also estimated on analysis of skinfolds and abdominal perimeters. Results At the end of the 10-sessions protocol, the IG demonstrated a significant decrease (p ≤ 0.05) in subcutaneous fat at the left anterior superior iliac spine (ASIS) level and in iliac crest perimeter measurements. A large intervention effect size strength (0.80) was found in subcutaneous fat below the navel and a moderate effect size strength on the vertical abdominal skinfold (0.62) and the perimeter of the most prominent abdominal point (0.57). Comparing the initial and final data of each group, the IG showed a significant decrease in numerous variables including visceral and subcutaneous fat above and below the navel measured by ultrasound (p ≤ 0.05). Conclusion Plaster body wrap in combination with aerobic exercise seems to be effective for abdominal fat reduction.

Estudo Estratigráfico e Paleontológico do Jurássico do Algarve Ocidental

Algarve Province, Southern Portugal, corresponds in part to a meso-cenozoic basin running along the coast from Cabo S. Vicente to beyond Spanish border. Structurally it is a big monocline plunging southwards much deformed mainly by two East-West longitudinal flexures. Lithostratigraphical and chronostratigraphical studies dealt specially with Jurassic formations. This and the geological mapping of the post-Hercynian sedimentary formations allow us to define the following units: Triassic-Lower Liassic Arenitos de Silves (Silves sandstones sensu P. Choffat, pro parte) - At their base the Silves sandstones (0-150m) are represented mainly by cross-bedded red sandstones. This unit is Upper Triassic (Keuper) in age, on the evidence of some Brachiopoda. Complexo margo-carbonatado de Silves (Silves marl-limestone complex=Silves sandstones sensu P. Choffat, pro parte) (80-200m) overlies the preceding, it may be reported to the Upper Triassic-Hettangian. It consists of a thick pelite-marl-dolomite-limestone series with many intercalations of greenstones. Since no fossils were found it is not possible to conclude whether it is still Hettangian or if it does correspond, in the whole or in part, already to the Sinemurian. Liassic Dolomitos e calcários dolomíticos de Espiche (Espiche dolomite-rocks and dolomitic-limestones) - The usually massive and finely crystalline or saccharoidal dolomites and dolomitic-limestones are the toughest strata of the Algarve margin giving rise to several hills. Its thickness attains in certain points 60 metres at least. Based on geometry and on lithological similarities with the carbonated complex of the northern basin of Tagus river (Peniche, São Pedro de Muel, Quiaios), this formation can be accepted as Sinemurian in age. As it happens with the carbonated complex, here also the first dolomite beds are non-isochronal throughout the region; upper time-limit of the dolomitic facies is either Lower Carixian, Lower Toarcian or even Lower Dogger. The dolomitization is secondary but not much later than sedimentation. However, between Cabo S. Vicente-Vila do Bispo there is evidence of an even later secondary dolomitization related to the regional fault complex. Calcário dolomítico com nódulos de silex da praia de Belixe (Belixe beach dolomitic-limestone with silex nodules) (50-55m) - Ascribed to Lower or Middle Carixian on the basis of Platypleuroceras sp., Metaderoceras sp. nov. and M. gr. Venarense. Calcário cristalino compacto com Protogrammoceras, Fuciniceras e ? Argutarpites de Belixe (Belixe compact crystalline limestone with Protogrammoceras, Fuciniceras and ? Argutarpites) (30m) - Ascribed to Lower Domerian. Middle and Upper Domerian are indicated but by a single specimen of ? Argutarpites. Calcários margosos e margas com Dactylioceras semicelatum e Harpoceratídeos de Armação Nova (Armação Nova marly limestones and marls with D. semicelatum and Harpoceratidae) (25m) -Ascribed to Lower Toarcian. Middle and Upper Toarcian formations are not known in the Algarve. Dogger Calcários oolíticos, c. corálicos, c. pisolíticos, c. calciclásticos, c. dolomíticos e dolomitos de Almadena (Almadena oolitic-limestones, coral-reef-limestones, pisolite-limestones, limeclastic-limestones, dolomitic-limestones and dolomite-rocks) (more than 50 metres), with lagoonal facies. Ascribed to Aalenian-Bathonian-? Callovian. Margas acinzentadas e calcários detríticos com Zoophycos da praia de Mareta (Mareta beach greyish marls and detritical limestones with Zoophycos) (40m) - Pelagic transreef facies with Upper Bajocian and Bathonian ammonites. Calcários margosos e margas da praia de Mareta (Mareta beach pelagic marly-limestones and marls) (110m) - Ascribed to the Callovian on its ammonites. Malm Near Cabo S. Vicente and Sagres the first Upper Jurassic level consists of a yellowish-brown nodular, compact, locally phosphated and ferruginous, sometimes conglomeratic, marly limestone (0,35-1,50m) containing a rich macrofauna, which includes: 1) Callovian forms unknown at Lower Oxfordian; 2) Upper Callovian forms that still survived in Lower and Middle Oxfordian; 3) Lower Oxfordian forms (Mariae and Cordatum Zones); 4) Lower and Middle Oxfordian forms (Mariae to Plicatilis Zone); 5) Middle Oxfordian forms (plicatilis Zone), and some ones appearing in Middle Oxfordian. This condensed deposit is therefore dated from Middle Oxfordian (Plicatilis Zone). The other Upper Jurassic lithostratigraphical units were also mapped but their detailed study is not presented in this work. Correlations between lithostratigraphical and chronostratigraphical scales from P. Choffat, J. Pratsch, C. Palain and from the author are stated. Further correlations are attempted between zonc scales of Carixian-Lower Toarcian and Upper Bajocian-Middle Oxfordian of France, Spain (Asturias, Iberian and Betic Chains), Argel (Orania) and Portugal (northern Tagus basin and Algarve). The study of pyritous fossil assemblages common in Upper Bathonian-Lower Callovian marly levels of the praia da Mareta seems to suggest that these sediments were deposited in a bay or in an almost closed coastal re-entrance virtually without deep water circulation. Although such conditions may occur at any depth one may suppose that these ones actually correspond to an infralittoral neritic environment. The thaphocoenosis collected there are almost entirely composed of nektonic (ammonites, Belemnites) and planktonic (Bositra) faunas. The sedentary (crinoids, brachiopods) or free (sea-urchins, gastropods) epibenthonic forms are very scarce; endobenthonic forms are not known. The palaeontological study of all Nautiloids and Ammonoids of the Liassic and Dogger is presented (except Kosmoceratidae and Perisphinctaceae). Among the thirty one taxa dealt with, one is new (Metaderoceras sp. nov.) and the great majority of the others has been identified for the first time in Algarve. Some others have never been reported before in Portuguese formations. The evolution, during Jurassic times, of the sedimentary basins of the Portuguese plate margin is described. The absence of Cephalopods in the very extensive marly and dolomitic limestones, partly marine, suggests that, during Lower Liassic, palaeogeography underwent no great changes. Dolomitic-limestone with silex nodules from Cabo S. Vicente contain the first ammonites recorded at the base of the Middle Liassic. This facies, although very common in Tethys, is unknown north of the Tagus. The faunal assemblage has a mediterranean to submediterranean character. Comparisons between faunal assemblage" from Algarve with the ones known north of the Tagus show that communications between Boreal Europe and Tethys, virtually non-existent during Lower and Middle Carixian, became very easy during Lower Domerian. In earlier Pliensbachian times two distinct seas were adjacent to the Iberian plate. One, an epicontinental sea with a tethyan fauna, extended southwards from the Meseta margin. Another, was a boreal sea; during its transgressive episodes boreal faunas attained into the basin north of the Tagus. During Middle Carixian and Lower Domerian, owing to simultaneous transgressions, these two seas joined together allowing faunal exchanges along the epicontinental areas which limited the emerging hercynian chains belts. During Liassic, the Algarve belonged undoubtedly to the tethyan submediterranean province. The area north of the Tagus, on the contrary, was a complex realm where subboreal and tethyan affinities alternatively prevailed. In the Algarve the first Middle Jurassic deposits do frequently show lateral thickness reductions as well as unconformities contemporaneous with other generalized disturbances on the sedimentation processes in other parts of Europe. By this time, near Sagres, a barrier reef developed separating lagoonal or ante-reef facies from the transreef pelagic zone. The presence of tethyan fauna, the abundance of Phylloceratidae and the absence of boreal forms allow us to consider the Algarve basin as a submediterranean province. The presence of Callovian pelagic fossiliferous formations in the Loulé area shows that during Middle Jurassic the marl-limestone transreef sedimentation was not confined to the western Algarve. They would extend eastwards where they only can be seen in the core of some anticlines. This is due to the progressive sinking of the meso-cenozoic formations as we proceed towards the South of the Sagres-Algoz-Querença flexure. In the whole of the Peninsule, and as for the Middle Callovian, an important regression can be clearly recognized on the evidence of an erosion surface which strikes obliquely the Middle and Upper Callovian strata. The geographic boundaries of the different faunal provinces are not changed by the presence of many Kosmoceratidae in the phosphate nodules since they are but a minority in comparison with the tethyan forms. An abstract model can be constructed showing that in Western Europe the Kosmoceratidae may have migrated South and westwards through a channel of the sea that linked Paris basin to Poitou and Aquitaine. By migrating between the Iberian meseta and the Armorican massif this fauna reached northern Tagus basin at the beginning of Upper Callovian (Athleta Zone); this south and southwest bound migration would have proceeded, allowing such forms to reach Algarve basin only in latest Callovian times (Lamberti Zone). This migration means that during Middle Jurassic a widely spread North Atlantic sea would exist, flooding the western part of Portugal up to the Poitou.

Optimização das fugas pela boca durante o CPAP nasal: banda submentoniana versus máscara facial

Introdução: O CPAP nasal é o tratamento de eleição para os pacientes com Síndrome da Apneia Obstrutiva do Sono (SAOS). Com a máscara nasal podem ocorrer fugas de ar pela boca, que podem por em causa a aderência do paciente ao tratamento devido muitas vezes ao desconforto que provocam, ao aumento do trabalho respiratório e por afectarem a qualidade do sono. Objectivos: Este estudo tem como principal objectivo verificar a eficácia da banda submentoniana e da máscara facial na correcção das fugas pela boca em pacientes com SAOS. Métodos e Participantes: Uma amostra de conveniência de 15 pacientes (8 homens) com SAOS e a fazerem CPAP com máscara nasal, foi recrutada. Foram divididos em dois grupos A e B, onde no grupo A se colocou a banda submentoniana e no grupo B se alterou a interface para máscara facial. Medidas e Resultados: As variáveis avaliadas neste estudo foram as fugas, o IAH, o percentil 95 da pressão de tratamento, a Sa,O2 e os efeitos adversos das duas intervenções. O nível de fugas reduziu no grupo A de 38±11,27 para 24,55±14,30L/min (p=0,002) e no grupo B de 34,34±16,50 para 18,51±16,22L/min (p=0,008). O IAH aumentou no grupo B de 2,60±2,13 para 4,41±3,88 (p=0,016). Relativamente ao percentil 95 da pressão de tratamento aumentou nos dois grupos (Grupo A de 10,15±2,63 para 12,08±2,45cmH2O (p=0,008) e no Grupo B 10,51±1,88 para 12,64±1,29cmH2O (p=0,008)). A Sa,O2 mínima aumentou e o tempo<90% diminui no grupo A com p=0,008, p=0,031, respectivamente. Quanto ao uso auto-reportado verificaram-se poucos efeitos adversos, salientando-se apenas a facilidade de colocação da banda submentoniana, a secura da boca nos dois grupos, a pressão no queixo provocada pela banda e a dor no dorso do nariz provocada pela máscara facial. Conclusão: Ambas as estratégias provaram ser mais eficazes a reduzir a fuga que a máscara nasal. Foram bem toleradas e com poucos efeitos adversos.

Characterisation of adventitious lung sounds in people with dementia

Introduction: Lower Respiratory Tract Infections (LRTIs) are highly prevalent in institutionalised people with dementia, constituting an important cause of morbidity and mortality. Computerised auscultation of Adventitious Lung Sounds (ALS) has shown to be objective and reliable to assess and monitor respiratory diseases, however its application in people with dementia is unknown. Aim: This study characterised ALS (crackles and wheezes) in institutionalised people with dementia. Methods: An exploratory descriptive study, including 6 long-term care institutions was conducted. The sample included a dementia group (DG) of 30 people with dementia and a match healthy group (HG) of 30 elderly people. Socio-demographic and anthropometric data, cognition, type and severity of dementia, cardio-respiratory parameters, balance, mobility and activities and participation were collected. Lung sounds were recorded with a digital stethoscope following Computerised Respiratory Sound Analysis (CORSA) guidelines. Crackles’ location, number (N), frequency (F), two-cycle duration (2CD), initial deflection width (IDW) and largest deflection width (LDW) and wheezes’ number (N), ratio (R) and frequency (F) were analysed per breathing phase. Statistical analyses were performed using PASW Statistics(v.19). Results: There were no significant differences between the two groups in relation to the mean N of crackles during inspiration and expiration in both trachea and thorax. DG trachea crackles had significant higher F during inspiration and lower IDW, 2CD and LDW during expiration when compared with HG. At the thorax, the LDW during inspiration was also significantly lower in the DG. A significant higher N of inspiratory wheezes was found in the HG. Both groups had a low ratio of high frequency wheezes. Conclusion: Computerised analyses of ALS informed on the respiratory system and function of people with dementia and elderly people. Hence, this could be the step towards prevention, early diagnosis and continuous monitoring of respiratory diseases in people with cognitive impairment.

Efeito hipotensivo de uma sessão de exercício aeróbio em idosos hipertensos

Introdução: As doenças cardiovasculares, entre elas, a hipertensão arterial constituem um dos problemas de saúde de maior prevalência, principalmente na população idosa. Alguns estudos têm apontado o exercício físico aeróbio como uma medida não farmacológica, eficaz, para a prevenção/controlo da hipertensão arterial. Objetivo: Este estudo avaliou o efeito agudo hipotensivo de uma sessão isolada de exercício físico aeróbio num grupo de idosos hipertensos. Metodologia: A amostra foi composta por 20 idosos, de ambos os géneros, hipertensos, pertencentes a três centros de convívio distintos. Os indivíduos foram divididos aleatoriamente em dois grupos, o grupo que fez a sessão de exercício (n=10, idade 81,2 ± 4,71 anos) e o grupo de controlo (n=10, idade 81,2 ± 3,12 anos). O grupo de exercício participou numa sessão de exercício físico aeróbio que teve 35 minutos de duração, sendo constituída por 5 minutos de aquecimento seguidos por duas frações de marcha a uma intensidade de 40-60% da frequência cardíaca (FC) de reserva, cada uma delas com a duração de 10 minutos, separadas por um intervalo de recuperação de 5 minutos, terminando com 5 minutos de retorno à calma. O grupo controlo permaneceu 35 minutos em repouso sentado. Todos indivíduos foram sujeitos à avaliação da pressão arterial (PA) e FC, antes, no intervalo, no término, 20 e 40 minutos após a sessão de exercício/35 minutos de repouso. Resultados: Observou-se que no grupo que fez o exercício físico a PA sistólica medida aos 40 minutos (123,04 ± 23,07 mmHg) após a sessão de exercício foi significativamente inferior aos restantes momentos de avaliação, incluindo o valor observado em repouso (135,57 ± 19,43 mmHg). A PA diastólica medida também aos 40 minutos (61,94 ± 7,49 mmHg) após a sessão foi inferior à obtida ao intervalo da sessão (72,40 ± 8,51 mmHg). A FC foi significativamente superior ao intervalo e no término da sessão comparativamente a todos os outros momentos de avaliação. Quanto ao grupo controlo não se verificaram diferenças significativas em nenhum dos parâmetros avaliados. Conclusão: Uma sessão isolada de exercício aeróbio de curta promove a ocorrência do fenómeno hipotensão pós-exercício em idosos hipertensos.

Clay body wrap with microcurrent: Effects in central adiposity

Introduction: Increased fat mass is becoming more prevalent in women and its accumulation in the abdominal region can lead to numerous health risks such as diabetes mellitus. The clay body wrap using compounds such as green clay, green tea and magnesium sulfate, in addition to microcurrent, may reduce abdominal fat mass and minimize or prevent numerous health problems. Objective: This study aims at measuring the influence of the clay body wrap with microcurrent and aerobic exercise on abdominal fat. Methods: Nineteen female patients, randomized into intervention (n = 10) and control (n = 9) groups, were evaluated using ultrasound for visceral and subcutaneous abdominal fat, calipers and abdominal region perimeter for subcutaneous fat and bioimpedance for weight, fat mass percentage and muscular mass. During 10 sessions (5 weeks, twice a week) both groups performed aerobic exercise in a cycloergometer and a clay body wrap with microcurrent was applied to the intervention group. Results: When comparing both groups after 5 weeks of protocol, there was a significant decrease in the subcutane- ous fat around left anterior superior iliac spine in the intervention group (ρ = 0.026 for a confidence interval 95%). When comparing initial and final abdominal fat in the intervention group, measured by ultrasound (subcutaneous and visceral fat) and by skinfold (subcutaneous fat), we detected a significant abdominal fat reduction. Conclusion: This study demonstrated that the clay body wrap used with microcurrent and aerobic exercise can have a positive effect on central fat reduction.

Independência e auto-suficiência: a política externa da República Popular da China entre 1957 e 1965

Dissertação apresentada para cumprimento dos requisitos necessários à obtenção do grau de Mestre em Ciência Política e Relações Internacionais

Flora medicinal y sus conocimientos asociados : lineamientos para una reglamentación

En este texto se presenta un espacio de intercambio de conocimientos desde una perspectiva científica, técnica y jurídica, para contribuir a la protección de los recursos naturales. Debido a la importancia de establecer mecanismos para proteger la biodiversidad y posibilitar la preservación de los conocimientos asociados especialmente al uso de la flora medicinal, la Línea de Investigación en Política y Legislación, del Grupo de Estudios en Sistemas Tradicionales de Salud de la Facultad de Medicina, y la Línea de Derecho Ambiental y Grupos Étnicos, del Grupo de Derechos Humanos de Jurisprudencia de la Universidad del Rosario, desarrollaron este libro a través del cual la Universidad se propone profundizar en el panorama actual de la reglamentación y política –Internacional, nacional y local—respecto a la flora medicinal y al patrimonio cultural inmaterial asociado a esta.

La influencia del derecho universal a la libre autodeterminación de los pueblos en la construcción de las Relaciones Bilaterales entre Palestina e Israel (1993-2004)

Esta monografía se enfoca en el papel que ha tenido el derecho a la libre autodeterminación de los pueblos en la construcción de las relaciones bilaterales entre Palestina e Israel, en uno de los periodos tal vez más fructíferos de la historia de las dos naciones, comprendido entre 1993 y 2004. Por medio del análisis de ciertos eventos históricos y manifestaciones del derecho a la libre autodeterminación de los pueblos durante del periodo de estudio seleccionado, se busca explicar cómo éstos han repercutido en la relación de ambos pueblos. Este análisis hace uso del enfoque constructivista de Alexander Wendt como herramienta que permite una aproximación teórica que considera, que la construcción de relaciones entre los diferentes agentes del Sistema Internacional son las ideas y creencias compartidas y no únicamente las capacidades materiales.

Lalia.

El documento muestra la vida de los refugiados saharauis en Argel a través de los ojos de una niña.

Los moros en El Quijote

Resumen tomado de la publicaci??n

4 Villas in Algiers (1992)

Cuatro casas mono-familiares para la Embajada de España en Argel

Argelia y los estudios árabes en Alicante (I): Míkel de Epalza

En el presente estudio deseamos presentar los trabajos elaborados por Míkel de Epalza en torno a Argelia, y en especial sobre el estudio de la historia argelina y española. De igual modo, este trabajo busca ser un modesto homenaje a todos los investigadores que han trabajado sobre nuestra historia común, argelinos, españoles y de cualquier otro origen, y en especial a quienes publicaron sus investigaciones en Argelia tras su independencia en 1962, que Míkel de Epalza ya estudiara hasta la fecha del año 1973, y cuyo elenco y conclusiones publicó como un libro titulado de Écrits relatifs à l’histoire de l’Espagne publiés en Algérie de 1962 à 1973. Las líneas esenciales de este estudio nacen de nuestro trabajo junto a Míkel de Epalza durante largos años y de la ponencia que presentamos al Congreso que en homenaje a Mouloud Kassem se celebró en Argel, entre el 27-29 de marzo de 2005. Lo que presentamos aquí es una redacción más completa y específica sobre la labor y los trabajos que Míkel de Epalza dedicó al estudio de Argelia, que busca dar a conocer tanto su personalidad como algunos de los estudios bibliográficos que sobre Argelia y España se han realizado en los últimos 50 años. Deseamos que sirva este estudio como homenaje a la labor aperturista de Mouloud Kassem, así como a la memoria de su predecesor en el Ministerio de Asuntos Religiosos, el Ministro Ahmad Taoufc Al-Madani, autor de una obra fundamental titulada Harb thalâthumi’a sana bayna Al-Jazâ’ir wa-Isbâniyâ (1492-1792), a quien Míkel dedicó un estudio en 2001.