When soil bacteria turn ammonium into nitrate, nitrification takes place. The operations carried out by soil microorganisms in the soil are a large part of the carbon cycle and nitrogen cycle's overlap.
Microbes consume nutrients, produce new substances for their own development, and ultimately perish. These cycles are interconnected, and the water cycle is a key catalyst for other biogeochemical cycles. For instance, the leaching of nitrogen and phosphate into rivers, lakes, and seas depends on the flow of water. The ocean serves as a significant carbon storage facility. Wherever carbon is delivered dissolved or suspended in flowing water, the two cycles immediately interact. An essential component is the movement of organic matter and weathering products from the continents to the seas.
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