describe the oceans solubility pump and the oceans biological pump using the pools of carbon (DIC, PIC, POC, DOC) and the processes. how are the two linked? where does the ocean \"take up\" C and where is it released from the ocean? Solution The oceans play an important role in regulating the amount of fever to in atmosphere because 02 can move quickly into and out of the oceans. It is estimated that approximately 93% of Co2is found in oceans. In oceans the solubility pump is physicochemical process which transports dissolved inorganic carbon to the interior. The solubility pump is driven by to principal factors. First one 4more C02 can dissolve into cold polar waters thane warm waters. As major ocean currents more from tropics to the poles they are cold and take more carbon dioxide from the atmosphere secondly the higher latitude zones also places where deep waters are formed as the water gets cold they become denser and sink into oceans interior absoring the Co2 accumulated on the surface. Bioloical pump: in this process carbon dioxide moves away from the surface ocean. Microscopic Marine animals called zooplankyon eat the phytoplankton and provide the basis for the food web for all animal life in the ocean. Although most of the fever to taken up by phytoplankton is recycled near the surface 30% sinks into the deeper waters before converted by Marine bacteria only 0.1 % reaches the sea floor as sediment. Carbon is cycled through the ocean biological processes of photosynthesis respiration and decomposition of aquatic plants. As the oceanic plants don\'t have large Woody stems the decomposition after quickly then on land Judo this very little carbon is stored in the ocean prove biological processes the total amount of carbonn update and carbon loss from the ocean depends on the balance of organic and inorganic processes. Carbon dioxide is soluble in water it reacts with water to form several ionic and nonionic compounds called dissolved inorganic carbon(DIC) for example aquous carbon dioxide ,carbonic acid, bicarbonate and carbonate. Carbon enters the ocean by dissolving in the water it also enters through rivers and other water bodies it is converted by organisms into organic carbon by photosynthesis and the food chain also helps in this process if circulates in the layout for longer periods before getting deposited as sediments. Oceanic absorption of Co2 is considered as very important form of carbon sequestration limiting the rate of carbon dioxide in the atmosphere. Dissolved organic carbon DOC in Marine systems is one of the cycled reservoir of organic matter on earth and it makes up 20% of all organic carbon in general these compounds are formed do the decomposition processes of organisms in the Marine system. It is defined as the organic matter that is able to pass through a filter range in size between 0.7 and 0.22 um. Particulate organic carbon POC is the carbon that is too large and is tilted out of your sample. Dissolved and parti.

1. describe the oceans solubility pump and the oceans biological pump using the pools of carbon
(DIC, PIC, POC, DOC) and the processes. how are the two linked? where does the ocean "take
up" C and where is it released from the ocean?
Solution
The oceans play an important role in regulating the amount of fever to in atmosphere because 02
can move quickly into and out of the oceans. It is estimated that approximately 93% of Co2is
found in oceans.
In oceans the solubility pump is physicochemical process which transports dissolved inorganic
carbon to the interior.
The solubility pump is driven by to principal factors. First one 4more C02 can dissolve into cold
polar waters thane warm waters. As major ocean currents more from tropics to the poles they are
cold and take more carbon dioxide from the atmosphere secondly the higher latitude zones also
places where deep waters are formed as the water gets cold they become denser and sink into
oceans interior absoring the Co2 accumulated on the surface.
Bioloical pump: in this process carbon dioxide moves away from the surface ocean.
Microscopic Marine animals called zooplankyon eat the phytoplankton and provide the basis for
the food web for all animal life in the ocean.
Although most of the fever to taken up by phytoplankton is recycled near the surface 30% sinks
into the deeper waters before converted by Marine bacteria only 0.1 % reaches the sea floor as
sediment.
Carbon is cycled through the ocean biological processes of photosynthesis respiration and
decomposition of aquatic plants. As the oceanic plants don't have large Woody stems the
decomposition after quickly then on land Judo this very little carbon is stored in the ocean prove
biological processes the total amount of carbonn update and carbon loss from the ocean depends
on the balance of organic and inorganic processes.
Carbon dioxide is soluble in water it reacts with water to form several ionic and nonionic
compounds called dissolved inorganic carbon(DIC) for example aquous carbon dioxide ,carbonic
acid, bicarbonate and carbonate.
Carbon enters the ocean by dissolving in the water it also enters through rivers and other water
bodies it is converted by organisms into organic carbon by photosynthesis and the food chain
also helps in this process if circulates in the layout for longer periods before getting deposited as
sediments.
Oceanic absorption of Co2 is considered as very important form of carbon sequestration limiting

2. the rate of carbon dioxide in the atmosphere.
Dissolved organic carbon DOC in Marine systems is one of the cycled reservoir of organic
matter on earth and it makes up 20% of all organic carbon in general these compounds are
formed do the decomposition processes of organisms in the Marine system. It is defined as the
organic matter that is able to pass through a filter range in size between 0.7 and 0.22 um.
Particulate organic carbon POC is the carbon that is too large and is tilted out of your sample.
Dissolved and particulate organic carbon or important components in the carbon cycle and serve
the primary food source for the aquatic food chains .moreover organic carbon and dissolved
particulate matter also affect the penetration of light in the aquatic systems which is very
important for the phototrophs.