Transfer and Recycling of Nutrients

Transfer and Recycling of Nutrients

Nutrient Cycles Overview

  • Nutrient cycles are essential for life on Earth, continually transforming and redistributively elements such as carbon, nitrogen, and phosphorus.
  • Nutrient cycles are also known as biogeochemical cycles, highlighting their combination of biological, geological, and chemical aspects.

The Carbon Cycle

  • The carbon cycle describes the movement of carbon between living organisms and the environment.
  • Carbon is taken up by plants through photosynthesis, converted into carbohydrates and other forms of stored energy.
  • Animals consume plants and other animals, taking in this carbon and releasing it via respiration.
  • Decomposition of organic matter also releases carbon back into the atmosphere, some can store it long term as fossil fuels.
  • Human activities, particularly burning of fossil fuels and deforestation, can disrupt the natural balance of the carbon cycle, leading to increases in atmospheric carbon dioxide.

The Nitrogen Cycle

  • The nitrogen cycle outlines how nitrogen transforms and circulates within ecosystems.
  • Nitrogen is needed for the creation of proteins and nucleic acids, but atmospheric nitrogen cannot be directly used by most organisms.
  • Bacteria in the soil or associated with plant roots can fix nitrogen, converting it into ammonium or nitrate ions that plants can use.
  • Nitrogen is passed up the food chain when animals eat plants or other animals.
  • Bacteria and fungi in the soil can also break down dead organic matter, returning nitrogen to the soil as ammonia in a process called ammonification.
  • Other types of bacteria in the soil convert ammonia back to nitrates (nitrification) or return it to the atmosphere as nitrogen gas (denitrification).

The Phosphorus Cycle

  • The phosphorus cycle describes the movement of phosphorus through the environment.
  • Unlike carbon and nitrogen, phosphorus rarely exists in a gaseous form and is mainly cycling between rocks, water, and living organisms.
  • Phosphorus in rocks can be released slowly over time through weathering, becoming accessible to plants.
  • Animals obtain phosphorus by consuming plants or other animals, while decomposition returns phosphorus to the soil.
  • Phosphorus can be washed into rivers and eventually into oceans, where it may eventually create new sedimentary rocks, starting the cycle again.
  • Overuse of phosphorus in agriculture can disrupt natural cycles, leading to eutrophication of water bodies.

Recycling of Nutrients

  • Dead plants, animals, and waste products return nutrients back into the ecosystem, a process known as nutrient recycling.
  • Decomposers, including bacteria, fungi, and certain types of animals, play a crucial role in nutrient recycling by breaking down organic material.
  • Humans can assist in nutrient recycling through practices like composting, where organic waste is collected and decomposed to produce a rich soil amendment.