Explore: Uranium Cycle (biogeochemistry)

Andrews, Jeffrey A. (2000). "Soil respiration and the global carbon cycle". Biogeochemistry. 48 (1): 7–20. Bibcode:2000Biogc..48....7S. doi:10.1023/A:1006247623877

decay of uranium and thorium. In crustal rocks, it is present as the lead sulfide mineral galena. Natural sources of lead in the lead cycle include wind

The deep water cycle, or geologic water cycle, involves exchange of water with the mantle, with water carried down by subducting oceanic plates and returning

differs from biogeochemistry in that the focus is on processes and organisms over space and time rather than on global chemical cycles. Geobiological

June 2010). "The Growing Human Footprint on Coastal and Open-Ocean Biogeochemistry". Science. 328 (5985): 1512–1516. Bibcode:2010Sci...328.1512D. doi:10

The fluorine cycle is the series of biogeochemical processes through which fluorine moves through the lithosphere, hydrosphere, atmosphere, and biosphere

Trace metal stable isotope biogeochemistry is the study of the distribution and relative abundances of trace metal isotopes in order to better understand

Biophysical Journal, Volume 108, Jan 2015 Newsome, The biogeochemistry and bioremediation of uranium and other priority radionuclides, Chemical Geology,

003. ISSN 0926-9851. Taghipour, B; Hemmati, M (2013). "Geobotany and biogeochemistry of Sungun copper deposit, northern Iran; an implication to mineral

Radiometric dating Isotope-ratio mass spectrometry Sulfur isotope biogeochemistry Urey–Bigeleisen–Mayer equation Drever, James (2002). The Geochemistry