Temat: anoxia - Katalog OPAC zbiorów

Skocz do pozycji: 1.

Tytuł:: Brewing Heterogeneous Devices for Monitoring Cerebrovascular Oxygenation
Autorzy:: Geetha, G.
Geethalakshmi, S. N.
Mathivadhani, D.
Powiązania:: https://bibliotekanauki.pl/articles/1193588.pdf
Data publikacji:: 2016
Wydawca:: Przedsiębiorstwo Wydawnictw Naukowych Darwin / Scientific Publishing House DARWIN
Tematy:: Anoxia
Hypoxia
Internet of Things (IoT)
Pbto2
Traumatic Brain Injury (TBI)
Wearable devices
Opis:: Technologies encumbering Wireless Sensor Network with its effulgence and ubiquity in Sensing plays a dominant role in Health care industry and Health monitoring System. Impeccable blending of Actuators and networking them for a viable communication across varied platforms paves gateway for triumphant IoT solution. IoT plays a predominant role in revitalizing the healthcare sector with appendages of several smart devices deliberated to facilitate medicos, surgeons and subjects to monitor each and every aspect of their health. Customary health checkups allow patients to distinguish health issues sooner and get treatment accordingly. IoT offers a cost effective solution adjunct with a timely intervention.
Źródło:: World Scientific News; 2016, 41; 275-280
2392-2192
Pojawia się w:: World Scientific News
Dostawca treści:: Biblioteka Nauki

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Skocz do pozycji: 2.

Tytuł:: From carbonate platform to euxinic sea – the collapse of an Early/Middle Devonian reef, Cantabrian Mountains (Spain)
Autorzy:: van Loevezijn, G. B. S.
Raven, J. G. M.
Powiązania:: https://bibliotekanauki.pl/articles/94474.pdf
Data publikacji:: 2017
Wydawca:: Uniwersytet im. Adama Mickiewicza w Poznaniu
Tematy:: Anoxia
Basal Choteč Event
Cantabria
carbon isotopes
Eifelian
Emsian
anoksja
Kantabria
izotopy węgla
eifel
ems
Opis:: The Santa Lucía Formation represents the major phase in Devonian reef development of the Cantabrian Zone (Cantabrian Mountains, northwest Spain). In the present study the transition from the carbonate platform deposits of the Santa Lucía Formation to the overlying euxinic basinal deposits of the Huergas Formation is described. These transitional strata are connected to the Basal Choteč Event and represent a condensed sedimentation of micritic dark-grey and black limestones with an upward increase of dark shale intercalations with iron mineralisation surfaces and storm-induced brachiopod coquinas. The transitional beds are grouped into a new unit, the Cabornera Bed, which consists of lime-stone, limestone-shale and shale facies associations, representing a sediment-starved euxinic offshore area just below the storm wave base. Four stages in reef decline can be recognised: a reef stage, an oxygen-depleted, nutrient-rich stage, a siliciclastic-influx stage and a pelagic-siliciclastic stage. Additional geochemical and geophysical investigations are needed to verify the results presented herein.
Źródło:: Geologos; 2017, 23, 3; 143--161
1426-8981
2080-6574
Pojawia się w:: Geologos
Dostawca treści:: Biblioteka Nauki

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