It's estimated that 0.1 % to 0.3 % of aluminum is absorbed (bioavailable) from the diet, while 0.3 % is
absorbed via water.
Not exact matches
Firstly
water is
absorbed by the root and moves through root hair cells
via the process of osmosis (we will look at this another day!).
Cold, polar
waters constantly
absorb CO2, sink as it becomes more dense, and is transported to the equatorial
waters via the ThermoHaline and outgases in the warmer
waters of the Indian and Pacific Oceans.
Dan H.: «Cold, polar
waters constantly
absorb CO2, sink as it becomes more dense, and is transported to the equatorial
waters via the ThermoHaline and outgases in the warmer
waters of the Indian and Pacific Oceans.»
It also
absorbs light
via photosynthesis, which allows plants to convert energy from the sun into food using carbon dioxide and
water.
A great slimming aid, this formula ensures that minerals are
absorbed cutaneously and
water is purged from fat cells
via osmosis.
This can also be a borehole system usually over a 100m deep and usually two or three or more borehole probes are inserted into these wells and
absorb the energy in the ground transferring it
via the heat pump into the home for use in heating and domestic hot
water.
Heat can be stored as latent heat / potential energy and the most commonly occurring substance on earth that can
absorb, hold and release large quantities of latent heat / potential energy
via phase transitions initiated by a range of naturally occurring thermodynamic processes is
water.
Topics that I work on or plan to work in the future include studies of: + missing aerosol species and sources, such as the primary oceanic aerosols and their importance on the remote marine atmosphere, the in - cloud and aerosol
water aqueous formation of organic aerosols that can lead to brown carbon formation, the primary terrestrial biological particles, and the organic nitrogen + missing aerosol parameterizations, such as the effect of aerosol mixing on cloud condensation nuclei and aerosol absorption, the semi-volatility of primary organic aerosols, the importance of in - canopy processes on natural terrestrial aerosol and aerosol precursor sources, and the mineral dust iron solubility and bioavailability + the change of aerosol burden and its spatiotemporal distribution, especially with regard to its role and importance on gas - phase chemistry
via photolysis rates changes and heterogeneous reactions in the atmosphere, as well as their effect on key gas - phase species like ozone + the physical and optical properties of aerosols, which affect aerosol transport, lifetime, and light scattering and absorption, with the latter being very sensitive to the vertical distribution of
absorbing aerosols + aerosol - cloud interactions, which include cloud activation, the aerosol indirect effect and the impact of clouds on aerosol removal + changes on climate and feedbacks related with all these topics In order to understand the climate system as a whole, improve the aerosol representation in the GISS ModelE2 and contribute to future IPCC climate change assessments and CMIP activities, I am also interested in understanding the importance of natural and anthropogenic aerosol changes in the atmosphere on the terrestrial biosphere, the ocean and climate.