Results 211 to 220 of about 201,786 (264)
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Water movement in the rabbit eye
Experimental Eye Research, 1991The intraocular distribution of topically applied D2O was quantified using deuterium nuclear magnetic resonance (NMR) spectroscopy. D2O appeared in all tissues with the highest concentration in the aqueous humor (1.2 M); however, it rapidly dissipated from the eye.
H M, Cheng +6 more
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2018
This chapter examines how the physical properties of water influence and explain the great diversity of swimming performance and mechanisms - from the scale of spermatozoa on up to whales. The key parameters of inertia, viscosity and their manifestation in the critically important Reynolds number are explained and placed in the context of a range of ...
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This chapter examines how the physical properties of water influence and explain the great diversity of swimming performance and mechanisms - from the scale of spermatozoa on up to whales. The key parameters of inertia, viscosity and their manifestation in the critically important Reynolds number are explained and placed in the context of a range of ...
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Ion Transport and Water Movement
Journal of Dental Research, 1987Secretion of water and electrolytes in salivary glands occurs by a dual process involving the formation of a plasma-like, isotonic primary-secretion in salivary acini and its subsequent modification in salivary-ducts by the removal and addition of specific ions.
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Archives of Ophthalmology, 1942
The object of this investigation was to determine the rate at which water enters and leaves the eye and, more particularly, to discover the rate of total water movement between the aqueous and its environment. To accomplish this, it is essential to distinguish one molecule of water from another, for water molecules in the eye are continuously ...
V. E. KINSEY, M. GRANT, D. G. COGAN
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The object of this investigation was to determine the rate at which water enters and leaves the eye and, more particularly, to discover the rate of total water movement between the aqueous and its environment. To accomplish this, it is essential to distinguish one molecule of water from another, for water molecules in the eye are continuously ...
V. E. KINSEY, M. GRANT, D. G. COGAN
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Movement Behaviour Recognition for Water Activities
2017This work describes an analysis process for the movement traces of users during water activities. The data is collected by a mobile phone app that the Navionics company developed to provide to its users sea maps and navigation services. The final objective of the project is to recognize the prevalent activity types of the users (fishing, sailing ...
Nanni M, Trasarti R, Giannotti F
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Southward movement of water - the water ways
2020This thesis explores the acculturation of the Australian landscape by the First Nations people of Australia who named it, mapped it and used tangible and intangible material property in designing their laws and lore to manage the environment. This is taught through song, dance, stories, and paintings. Through the tangible and intangible knowledge there
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[Lithium and body water movement].
Agressologie: revue internationale de physio-biologie et de pharmacologie appliquees aux effets de l'agression, 1982info:eu-repo/semantics ...
Abramow, Maurice, Cogan, Elie
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The occurrence and movement of water
Acta Geophysica, 2007A review is presented of the basic scientific analysis of the behaviour of water at all scales from the molecular (10−8 m) to the catchment scale (105 m). The approach needed to make progress at the various scales is shown to be different and sometimes contradictory.
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AAPG Bulletin, 1936
ABSTRACT The movement of water through formations having capillary openings is generally laminar and obeys Darcy’s law, at least down to very low gradients. About 1,000 samples tested in the Geological Survey laboratory have coefficients of permeability ranging from .001 to 90,000, indicating probable velocities ranging from a ...
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ABSTRACT The movement of water through formations having capillary openings is generally laminar and obeys Darcy’s law, at least down to very low gradients. About 1,000 samples tested in the Geological Survey laboratory have coefficients of permeability ranging from .001 to 90,000, indicating probable velocities ranging from a ...
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1974
Water may enter the rhizosphere† from above as natural or artificial precipitation, or as surface flow; water may enter the rhizosphere from below or from the sides by capillarity or movement along a gradient of potential, or by mass flow along a hydrostatic potential.
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Water may enter the rhizosphere† from above as natural or artificial precipitation, or as surface flow; water may enter the rhizosphere from below or from the sides by capillarity or movement along a gradient of potential, or by mass flow along a hydrostatic potential.
openaire +1 more source