Приклади вживання Biogeochemical cycles Англійська мовою та їх переклад на Українською
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Biological and biogeochemical cycles.
Land plants are key components of the water cycle and several other biogeochemical cycles.
Biogeochemical cycles of natural and disturbed peatland ecosystems, their role in the global cycle of carbon and greenhouse gases.
Which of the following are involved in biogeochemical cycles?
In contrast to the purely geological processes, biogeochemical cycles involving living matter are much higher intensity, speed, and a number of agents involved in the trafficking.
Studying the role of microorganisms in biogeochemical cycles.
As microbes are responsible for many biogeochemical cycles and are crucial to the continued function of the biosphere, Woese's efforts to clarify the evolution and diversity of microbes provided an invaluable service to ecologists and conservationists.
The most well-known and important biogeochemical cycles, for example.
Thanks to its ability to break down the dead matter of animals and plants,fungi play an important role in biogeochemical cycles.
The most well-known and important biogeochemical cycles are shown below:.
However, the processes that move them through the soil or ocean are very slow,making the phosphorus cycle overall one of the slowest biogeochemical cycles.[2][8].
What would be the consequences for the biogeochemical cycles of the planet?
Phosphates move quickly through plants and animals; however, the processes that move them through the soil or ocean are very slow,making the phosphorus cycle overall one of the slowest biogeochemical cycles.
Safety of GMOs to the environment, including effects on biochemical and biogeochemical cycles in the process of decomposition of organic material in soil.
Phosphates move quickly through plants and animals; however, the processes that move them through the soil or ocean are very slow,making the phosphorus cycle overall one of the slowest biogeochemical cycles.[2][7].
Unlike many other biogeochemical cycles, the atmosphere does not play a significant role in the movement of phosphorus, because phosphorus and phosphorus-based compounds are usually solids at the typical ranges of temperature and pressure found on Earth.
These more or less circular paths are known as biogeochemical cycles.
You will learn how climate change, global alterations of land use,disrupted water- and biogeochemical cycles, pollution, biological invasions and loss of biodiversity are threatening the viability of our planet, for us humans, and many organisms in natural ecosystems.
A first step towards improving the scientific basis for these strategies is a better understanding of land, oceans, atmosphere and their interlocking water,nutrient and biogeochemical cycles and energy flows which all form part of the Earth system.
Prof Peter Cox, professor of climate system dynamics at the University of Exeterand a lead author on the“global carbon and other biogeochemical cycles and feedbacks” chapter of the forthcoming sixth assessment report(AR6) of the Intergovernmental Panel on Climate Change(IPCC).
The primary biogeochemical cycle is the carbon cycle. .
Soil microorganisms act as both sinks and sources of available P in the biogeochemical cycle.
The phosphorus cycle is the biogeochemical cycle that describes the movement of phosphorus through the lithosphere, hydrosphere, and biosphere.
Available phosphorus is found in a biogeochemical cycle in the upper soil profile, while phosphorus found at lower depths is primarily involved in geochemical reactions with secondary minerals.
The nitrogen cycle is the biogeochemical cycle through which nitrogen is converted into multiple chemical forms as it circulates among the atmosphere, terrestrial, and marine ecosystems.
The nitrogen cycle is the biogeochemical cycle by which nitrogen is converted into various chemical forms as it circulates among atmosphere and land(terrestrial) and marine ecosystems.
Soil microorganisms act as both sinks and sources of available P in the biogeochemical cycle.[1] Locally, transformations of P are chemical, biological and microbiological: the major long-term transfers in the global cycle, however, are driven by tectonic movements in geologic time.
Marine processes exert massive influences on the Earth's climate and the pattern of biogeochemical cycling.