Effects of Maitland manual therapy on the treatment of pain syndromes of the cervical spine

Introduction: The aim of this study was evaluate the effect of Maitland's manual therapy on selected motor function parameters in cervical spine pain syndromes.Material and Methods: 30 subjects were enrolled, in the age from 27 to 66, including 15 men and 15 women with chronic functional cervical spine syndrome who had a 10-day physiotherapy cycle that did not produce the expected results. The study included: pain assessment in the Dziak scale, measurements of mobility of the cervical spine and shoulder joints, functional evaluation by Hautanta, De`Klein, Jackson, and palpation of muscle irritation.Results: A comparison of average pain scores before and after therapy indicated that the pain level after treatment decreased (p <0.05), but only in some patients (n = 23). The mean values of cervical vertebrae before and after therapy vary from the dependence on the investigated movement. There is an increase in the range of rotation, straightening and bending to the right in men and women (p <0.05), the range of bending forward and bending left only in women (p <0.05). There was no change in parenchymal mobility in parenchymal tumors (p> 0.05). There has been a decrease in positive clinical trials and muscle irritation after therapy.Conclusions: Maitland manual therapy is effective in the treatment of cervical spine pain syndromes. The technique results in a significant increase in the mobility of the cervical spine as well as an improvement in the functional state of the cervical segment without affecting the mobility of the shoulder ridge. There was a decrease in palpate tenderness of the soft tissue studied

The Ponto-Caspian basin as a final trap for southeastern Scandinavian Ice-Sheet meltwater

This paper provides new data on the evolution of the Caspian Sea and Black Sea from the Last Glacial Maximum until ca. 12 cal kyr BP. We present new analyses (clay mineralogy, grain-size, Nd isotopes and pollen) applied to sediments from the river terraces in the lower Volga, from the middle Caspian Sea and from the western part of the Black Sea. The results show that during the last deglaciation, the Ponto-Caspian basin collected meltwater and fine-grained sediment from the southern margin of the Scandinavian Ice Sheet (SIS) via the Dniepr and Volga Rivers. It induced the deposition of characteristic red-brownish/chocolate-coloured illite-rich sediments (Red Layers in the Black Sea and Chocolate Clays in the Caspian Sea) that originated from the Baltic Shield area according to Nd data. This general evolution, common to both seas was nevertheless differentiated over time due to the specificities of their catchment areas and due to the movement of the southern margin of the SIS. Our results indicate that in the eastern part of the East European Plain, the meltwater from the SIS margin supplied the Caspian Sea during the deglaciation until ∼13.8 cal kyr BP, and possibly from the LGM. That led to the Early Khvalynian transgressive stage(s) and Chocolate Clays deposition in the now-emerged northern flat part of the Caspian Sea (river terraces in the modern lower Volga) and in its middle basin. In the western part of the East European Plain, our results confirm the release of meltwater from the SIS margin into the Black Sea that occurred between 17.2 and 15.7 cal kyr BP, as previously proposed. Indeed, recent findings concerning the evolution of the southern margin of the SIS and the Black Sea, show that during the last deglaciation, occurred a westward release of meltwater into the North Atlantic (between ca. 20 and 16.7 cal kyr BP), and a southward one into the Black Sea (between 17.2 and 15.7 cal kyr BP). After the Red Layers/Chocolate Clays deposition in both seas and until 12 cal kyr BP, smectite became the dominant clay mineral. The East European Plain is clearly identified as the source for smectite in the Caspian Sea sediments. In the Black Sea, smectite originated either from the East European Plain or from the Danube River catchment. Previous studies consider smectite as being only of Anatolian origin. However, our results highlight both, the European source for smectite and the impact of this source on the depositional environment of the Black Sea during considered period

Stratigraphy and conditions of accumulation of the Younger Loesses (Vistulian) in the Holy Cross Mountains area, Poland

The paper presents results of studies focused on occurrence and correlation of four main horizons of Younger Loesses: Lowest Younger Loess (LMn – after Maruszczak, 2001), Lower Younger Loess (LMd), Middle Younger Loess (LMs), and Upper Younger Loess (LMg) recorded in five sections (Politów, Wąchock, Nietulisko Małe, Komorniki and Bodzechów) in the Holy Cross Mountains area. All analysed loesses were accumulated during the Vistulian Glaciation (Weichselian). The horizons were distinguished based on separating interstadial tundra soils, coupled with thermoluminescence dating, and correlated with marine oxygen-isotope stages MIS 5d−2. The Lowermost Younger Loess (LMn) covers the Nietulisko I soil complex (Jersak, 1973), developed on deposits of the Odranian Glaciation (MIS 6) and representing a forest soil of the Eemian Interglacial (MIS 5e) and the Brørup warming (MIS 5c). A thin horizon of the Oldest Younger Loess and a thin sandy horizon, both probably corresponding to the Herning cooling phase (MIS 5d) at the boundary with the Eemian Interglacial, were distinguished within this complex. Based on previously performed grain-size and heavy mineral analysis of the Upper Younger Loess (LMg) and a topographic position of the loesses in four loessy islands of diverse regional extent, accumulation of this loess in the Holy Cross Mountains area is found to have been stimulated by the western winds. The proposed model of loess accumulation takes into account the influence of the topography of the area and its geological structure

Pleistocene deposits in the western part of the Holy Cross Mountains

The paper presents characteristics of the Pleistocene sediments in the western part of the Holy Cross Mountains. They are subdivided into four complexes and their stratigraphic setting is referred to the updated scheme for the Pleistocene of Poland. The Preglacial Complex includes fluvial sediments characteristic for its lack of Scandinavian material. Sediments of three main glaciations (Nidanian, Sanian 1 and Sanian 2) within the South Polish Complex, are referred also as the South Polish Glaciations. The oldest of these glaciations (Nidanian) is separated from the middle glaciation (Sanian 1) by sediments of the Podlasian Interglacial, represented by clay at the Kozi Grzbiet Cave that contains faunal remains and record of the Brunhes/Matuyama palaeomagnetic boundary. During the middle (Sanian 1) and youngest glaciation (Sanian 2), the Holy Cross Mountains were almost completely covered by the Scandinavian ice sheet, forming glacial deposits separated by fluvial series of the Ferdynandovian Interglacial. The Middle Polish Complex begins with sediments of the Mazovian Interglacial, represented by a pollen record from the Zakrucze site. They are followed by deposits of periglacial and fluvial origin of the Liwiecian Glaciation, Zbójnian Interglacial, Krznanian Glaciation and Lublinian Interglacial. The following glaciation (Odranian) is represented by the youngest glacial deposits that document presence of the Scandinavian ice-sheet in the westernmost part of the Holy Cross Mountains. The North Polish Complex is composed of a climatic warming (Eemian Interglacial) and cooling (Vistulian Glaciation), and is represented by valley and periglacial deposits. The last cooling of the Pleistocene is recorded in faunal remains in the Raj Cave

The rodman system of wear the trolley wires railway traction

W artykule przedstawiono konfigurację stanowiska do pomiarów zużycia przewodów jezdnych trakcji kolejowej. Zaproponowano sposób pomiaru. Przedstawiono budowę cyfrowego systemu odczytu położenia spełniającego wymagania techniki pomiaru.In the paper, the configurations of the station to measurement of wear the trolley wires railway traction is shown. The means of measurement is proposed. It is the construction of digital read-out system of position fulfilling the technique measurement requirements

Applied linear encoders in the engineering industry

W referacie przedstawiono krótką informację o rozwoju czujników pomiarowych położenia jakimi są liniały. Omówiono zasadę działania oraz budowę najczęściej stosowanych rodzajów liniałów w przemyśle maszynowym. Na podsumowanie podano podstawowe parametry eksploatacyjne liniałów oraz zalecenia ich montażu.The paper presents brief information about the development of position sensors such as linear encoders. Discusses the principles of operation and construction of the most commonly used types linear encoders in the engineering industry. At the summary provides basic operational performance linear encoders and recommendations of their assembly

Modułowy cyfrowy układ sterowania i pomiaru położenia

The article presents a modular digital system of the control and position measurement. It shows the structure of modules with photoelectric and capacitative linear encoders, and a universal solution for the control and position measurement.W artykule przedstawiono modułowy cyfrowy system sterowania i pomiaru położenia. Przedstawiono struktury modułów z fotoelektrycznym i pojemnościowym liniowym enkoderem, a także uniwersalne rozwiązanie sterowania i pomiaru położenia