A well-known method is C-14 dating. Carbon 14 is a radioactive isotope of carbon that has half-life of 5730 years, meaning that if you start with 1000 g of C-14, after 5730 years you would have 500 g left (the other half has decayed into N-14). C-14 is present in trace amounts in nature and living organisms would therefore maintain a near-constant level of C-14 in their bodies if they consume and interact with their surroundings. Dead organisms, however, can no longer eat and therefore cannot replenish their C-14 levels, and the C-14 levels would begin to fall due to decay. The amount of C-14 in a dead organism can be compared to a reference level to determine how much time has passed since it died by the formula T = -5730*log2(r/R) where T is the time since the organism's death, r is the remaining level of C-14, and R is the reference level of C-14.
All living things contain carbon, which we all accumulate from our food and from the air. That's true for birds, animals, trees, people; if it's alive, it is bringing in carbon from the environment. When we die, or when a tree dies, we stop taking in carbon from the environment.
Carbon is an element which has 6 protons in the nucleus, and some number of neutrons. The most prevalent are 6 or 7 neutrons, making Carbon either a 12 or 13 mass atom.
There are also several radioactive isotopes, the longest-lived version having 8 neutrons. This carbon-14 isotope decays with a half-life of 5,715 years, and turning into nitrogen. When we breathe in, or eat anything, we're adding a tiny bit of carbon-14 to our bodies - but when we die, this stops.
We know the ratio of normal carbon to carbon-14 in the environment. So if we carefully measure the amount of carbon-12 to carbon-14 in an ancient body, or an ancient tree, we can calculate at least approximately how long it has been since any new c-14 was added; that is, how long it has been dead.
1. C-14 and C-12
because g is organic, compound
Carbon 14
it is humus
organic matter important to plant growth is humus.
decayed organic matter.
The isotope of carbon is used to date the ancient fossils. Since every living creature had organic matter and carbon is an integral part of that organic matter, it is conventional to use carbon isotope.
Weathering and erosion produce ever smaller rock particles which, when mixed with dust and decayed organic matter over time, result in different types of soil.
Humus
That would be necromass.
decayed organic matter
decayed organic matter
Decayed organic matter
decayed organic matter
Decayed plant and animal matter.
it is humus
decayed plants and animals
Living things that have been decayed
It is soil. _________________ Maybe you're speaking of Humus.
organic matter important to plant growth is humus.