Here, we report surface water dissolved inorganic carbon (DIC) and sedimentary
organic carbon concentrations and their isotopic compositions in the rapidly urbanized Jiaozhou Bay in northeast China as well as carbonate parameters in effluents of three large WWTPs around the bay.
«Microbial cell and
organic carbon concentrations in this accreted ice are significantly higher than those in the overlying ice, which implies that the subglacial environment is the source,» says Christner.
When he tested soils from the experimental plots, he saw soil
organic carbon concentrations rise gradually with increases in nitrogen fertilization at soil depths from 0 to 6 inches, although not at deeper ones.
But unexpectedly in this case, «we didn't see improvement in soil aggregate stability even though soil
organic carbon concentration increased,» Blanco says, noting that soil particles usually bind together more strongly in aggregates as soil organic carbon concentrations rise.
Not exact matches
Matyas Ripszam has also examined the effects of higher temperature and different
concentration of
organic carbon content on the distribution of pollutants in modelled real - life marine ecosystems, so called mesocosms.
According to Matyas Ripszam, Umeå University, this change will have high impact on the
organic pollutants on the
organic pollutants in the northern Baltic Sea, since this
carbon can interact with the pollutants and decrease their
concentration in the water.
Xiao used battery powered aerosol monitors to measure indoor
concentrations of fine particulate matter, or particles 2.5 micrometers in diameter or smaller, which consists mainly of black
carbon and
organic carbon.
The team's findings provide one possible mechanism for an observed increase in the
concentration of dissolved
organic carbon in the surface waters of North America and Europe during the last few decades, and have implications for management of water quality in coastal zones worldwide.
Without a regular input of
organic matter, soil microbial diversity decreases and the
carbon concentration is lowered.
This in turn triggered decreases in marine phosphate
concentrations, productivity,
organic carbon burial and ultimately oxygen.
As a result, the
concentration of this greenhouse gas is reduced and other sources of
organic carbon that are usually applied as biotechnological substrates, such as agricultural products, are no longer required.
That deep water is not only rich in nutrients, it also has relatively high
concentrations of
carbon dioxide, both because it is cold (cold water can absorb and hold more
carbon dioxide than warm water) and because the decomposition of
organic matter that sinks into the depths releases
carbon dioxide.
These highly sensitive artificial sense organs can reliably detect gases of all kinds, from toxic
carbon monoxide to carcinogenic
organic compounds, and can determine their
concentrations quantitatively.
It is a true multi-talent: Its calcium carbonate platelets carry
organic material from the surface to the deep ocean, which regulates
carbon dioxide
concentrations in the atmosphere.
Based on accumulating measurements of microbes in the subglacial environment, he calculates that the
concentration of cell and
organic carbon in the Earth's ice sheets, or «cryosphere», may be hundreds of times higher than what is found in all the planet's freshwater systems.
Indoor air quality is defined by the
concentrations of various pollutants, including
carbon dioxide (CO2), volatile
organic compounds (VOCs), moulds, dusts and airborne fungi.
A rapid depletion in 13C between about 17,500 and 14,000 years ago, simultaneous with a time when the CO2
concentration rose substantially, is consistent with release of CO2 from an isolated deep - ocean source that accumulated
carbon due to the sinking of
organic material from the surface.
The soils may have similarly held
organic matter and experienced a
carbon loss from the permafrost which would have contributed to past changes in atmospheric CO2
concentrations.
Many previous studies have measured
concentrations of
carbon in the soil from
organic sources, and here Papanicolaou et al. contribute new results that account for the uneven slope of the ground, focusing on land that is constantly disturbed by human activities.
Black
carbon (BC) and
organic carbon (OC)
concentrations in the Zuoqiupu ice core for the monsoon (June - Sept) and non-monsoon (Oct - May) seasons, and the annual mean.
These characteristics included morphometric, geographic, and historical properties of study reservoirs (i.e., depth, residence time, volume, surface area, age, and latitude), biologically significant water column solute
concentrations (i.e., NO3 — , total phosphorus, and dissolved
organic carbon), and metrics of ecosystem primary productivity (i.e., trophic status and mean or modeled surface water chlorophyll a
concentrations; see the supplemental materials for a complete list of the tested variables).
The simulated global mean
organic carbon (OC)
concentrations increase with altitude up to a mean pressure level of about 800 - 900 hPa, and then decrease with altitude (see Fig. 4).
However, the extent of black -
carbon - induced warming is dependent on the
concentration of sulphate and
organic aerosols — which reflect solar radiation and cool the surface — and the origin of the black
carbon3, 4.
On the other hand,
organic eutrophication (without fertilizers) does tend to cause an increase in respiration, increasing the
carbon dioxide
concentration and lowering the pH again.
TA, total alkalinity; DIC, dissolved inorganic
carbon; pCO2,
carbon dioxide
concentration; HCO3 −, bicarbonate
concentration; CO32 −, carbonate
concentration; POC, particulate
organic carbon content per cell; PP, primary production per cell; PIC, particulate inorganic
carbon content per cell; CR, calcification rate per cell; Chl a, chlorophyll a content per cell.
He is an
organic geochemist with specific expertise in geomicrobiology and palaeoclimate reconstruction, with an emphasis on developing and applying molecular proxies for ancient
carbon dioxide
concentrations and temperatures.
They found that such water supplies had higher
concentrations of both
organic carbon and potentially harmful disinfection byproducts.
From 1991, when the experiment began, the plots subjected to 5C warming lost about 17 % of the
carbon that had been stored in the top 60 cm of the soil, where the greatest
concentration of
organic matter is to be found.