Sentences with phrase «of absorption varies»

The amount of absorption varies with wavelength and depends directly on the composition and physical conditions of the atmosphere.

Not exact matches

(The absorption rate varies depending on the brand of flour.)

POCKET DIAPERS - Pocket Diapers are the kind of cloth diapering system to buy if you need ONE cloth diaper to meet varying levels of absorption.

Although the level of caffeine absorption varies greatly from one person to another, this substance has a lengthy half - life in newborns.

Their videos (use the link below) capture varying scales of water nucleation occurring in the nano - structures and the absorption of the majority of an impacting rain droplet with little or no splashing.

The researchers examined the impact of mineral dust on monsoon strength by creating seven high - resolution computer simulations that varied the heat absorption of the mineral dust.

The FORTIS spectrographic element splits the light captured by the telescope into segments of varying wavelength intensity, which help scientists discern hydrogen emission and absorption.

Subsequently, the article presents a parameter variation study centered around these ideal and realistic cases that demonstrates the varying impact of each phenomenon (light absorption, charge transport, catalysis) on overall device efficiency and efficiency limits.

This is because the Atwater system fails to take into account that not all the energy in foods is complete digested or absorbed, and today we know that absorption varies based on the type of food and the individual who is consuming it.

In addition, absorption of vitamin A varies according to the food.

These supplements provide different amounts of elemental magnesium (the constituent that matters) and also vary significantly in their bioavailability (absorption).

«There are varying studies on the absorption rates of vitamins and minerals, with many showing that the compressed pill form of vitamins have very poor absorption rates.

The book contains the History of Essential Oils, Olfactory Process, the Limbic System, Absorption through the skin, The Lymphatic System, Methods of extraction, Essential Oil Production and Adulteration, Effective application, Safety Guidelines and Contra - Indications, Glossary of Therapeutic Action, Carrier / Base Oils, Varied Applications, Classification of Plants, Therapeutic Grade essential oils, Chemistry of essential oils, Chemical constituents of some commonly used essential oils, Essential Oil Monographs, Anise to Ylang Ylang, Common conditions aided by Aromatherapy, Compresses, Poultices, Pregnancy, Children / Babies, Fragrant way to Beauty, The Aromatherapy Massage, and finishes with the Aromatherapy Consultation.This book is $ 50.00 when bought separately and independent of a course tuition.

The advantages of transdermal absorption are varied including more rapid entry into the bloodstream, bypassing the digestive tract, and increased absorption and bioavailability.

Thus meaning an isocaloric diet comprising of the exact same foods: raw vs cooked, would vary in calorie absorption.

Digestion / absorption is an efficient process whose duration varies according to the size of the dose (our digestive system is way smarter than we give it credit for).

Absorption of magnesium from different kinds of magnesium supplements varies.

I am learning that coconut flours vary significantly in their rate of absorption from brand to brand.

So the intensity of radiation (at some frequency and polarization) changes over distance, such that, in the direction the intensity is going, it is always approaching the blackbody value (Planck function) for the local temperature; it approaches this quickly if the absorption cross section density is high; if the cross section density is very high and the temperature doesn't vary much over distance, the intensity may be nearly equal to the Planck function for that location; otherwise its value is a weighted average of the Planck function of local temperature extending back over the path in the direction it came from.

The ability of a band to shape the temperature profile of the whole atmosphere should tend to be maximum at intermediate optical thicknesses (for a given band width), because at small optical thicknesses, the amounts of emission and absorption within any layer will be small relative to what happens in other bands, while at large optical thicknesses, the net fluxes will tend to go to zero (except near TOA and, absent convection, the surface) and will be insensitive to changes in the temperature profile (except near TOA), thus allowing other bands greater control over the temperature profile (depending on wavelength — greater influence for bands with larger bandwidths at wavelengths closer to the peak wavelength — which will depend on temperature and thus vary with height.

In that case it does not matter how the water is heated but simply the temperature of the layer of surface water down to a few multiples of the inverse of the IR absorption coefficient which is I think varies from around a few cm to less than 1 mm with increasing wavelength.

Precise attribution is difficult because there is significant overlapping absorption with varying degrees of saturation, and there is the need to take into account the vertical structure and time - spatial distribution of absorbers, requiring a good climate GCM with good radiative transfer.

The places where one has largest absorption and emissions of CO2 such cities are rarely measured accurately - the reason is CO2 varies a lot, and second there is so much CO2 [comparably], one doesn't need precise instrument to detect it.

In particular, the absorption and radiation properties of CO2 vary greatly.

Finally, the 4 W m − 2 CO2 forcing avoids the uncertainty in the exact magnitude of a doubled CO2 forcing [1,48] estimate of 3.7 W m − 2 for doubled CO2, whereas Hansen et al. [66] obtain 4.1 W m − 2, as well as problems associated with the fact that a doubled CO2 forcing varies as the CO2 amount changes (the assumption that each CO2 doubling has the same forcing is meant to approximate the effect of CO2 absorption line saturation, but actually the forcing per doubling increases as CO2 increases [66,85]-RRB-.

A possible mechanism responsible for this linkage begins with the absorption of varying amounts of solar energy by the tropical oceans which creates ocean temperature anomalies.

CO; 2 Observations of the Infrared Radiative Properties of the Ocean «[I] t is necessary to understand the physical variables contributing to sea surface emitted and reflected radiation to space.The emissivity of the ocean surface varies with view angle and sea state, the reflection of sky radiation also depends on view angle and sea state, and the absorption of atmospheric constituents such as water vapor, aerosols, and subdivisible clouds affect transmittance.»

How much does potential surface area for CO2 absorption vary with a one percent change in the number and nature of water droplets in the atmosphere?

The rate of absorption is a very intricately varying function of the wavelength of the light.

The absorption rate I report here is for all of Coral Springs, however, keep in mind that absorption rates can vary by neighborhood and will vary by city also.

The absorption rate I report here is for all of Coral Springs, however, keep in mind that absorption rates can vary by neighborhood and will vary by city.