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Dissolved and particulate organic carbon are important components in the carbon cycle and serve as a primary food sources for aquatic food webs. In addition, DOC alters aquatic ecosystem chemistries by contributing to acidification in low-alkalinity, weakly buffered, freshwater systems.
Dissolved organic nitrogen (DON) is the important and active component of dissolved organic matter (DOM) in lake sediments, and approximately 1272% of DON can be used as a nitrogen source by bacteria and algae [2]; thus, its availability and mobility have an important role in the dynamic processes of nitrogen
Dissolved organic matter (DOM) in marine sediment pore waters plays an important role in sediment carbon and nitrogen remineralization and may also be involved in sediment carbon preservation.
Nitrate (NO3) is the most common form of inorganic nitrogen in unpolluted waters. Nitrate moves readily through soils and into ground water, where concentrations can be much higher than in surface waters. Ammonia (NH3) is formed when organic nitrogen is broken down by bacteria.
On the other hand, inorganic nitrogen is immediately available to plants, as they can directly uptake the ammonium or nitrate ions through their roots. This readily available form of nitrogen is particularly important during periods of rapid plant growth or when there is a deficiency of organic matter in the soil.
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Nitrogen is a nutrient of great environmental concern, because when in excess it is responsible for eutrophication. All living organisms need nutrients to grow and the nutrients need to be in the water to support the food chain.
What is it: The concentration of dissolved inorganic nitrogen ( DIN = ammonia + nitrate + nitrite) in winter is used as an index of nutrient enrichment in marine waters, as DIN usually limits algal growth in seawater.

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