FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W4285189084> ?p ?o ?g. }

• W4285189084 endingPage "254" @default.
• W4285189084 startingPage "209" @default.
• W4285189084 abstract "Arsenic, lead, fluorine, nitrogen, and carbon are common in the near-surface environment, but their concentrations in water, solids, and biota are highly variable. The distribution of As, Pb, F, N, and C in the environment is dependent on source, mineralogy, speciation, biological interactions, and geochemical controls. The As minerals interact with environment, and this renders either their dissolution or the formation of secondary minerals, or both. The distribution of the environmental arsenic is determined by the biogeochemical transformations with respect to the redox conditions, the pH, the availability of ions, the adsorption–desorption, dissolution, and the biological activity. The biological transformation and cycling of As can lead to oxidation or reduction of species that mobilize As. Besides, a significant proportion of As can also be remobilized from the soils through the process of anion exchange. Large variations can be observed on all spatial scales influenced by a variety of natural processes including nongeological influences such as climate and vegetation. Continental weathering of bedrocks contributes natural Pb to sediments, while mining and refining of Pb-bearing ores, which are subsequently used for industrial Pb applications, supply anthropogenic Pb to the environment. Lead geochemistry of rivers and costal environments plays a significant role in the biogeochemical cycling of Pb and pollutant delivery at the land–sea interface. Fluorine is ubiquitous in the environment with most deriving from natural sources, these being normal weathering processes resulting in F release from rocks and minerals, volcanic activity, and marine aerosol emission, together with biomass burning, being in part natural. However, there are several sources of anthropogenically derived F, which in some areas represent a threat to the biosphere. Together with carbon, oxygen, and hydrogen, nitrogen is one of the four most common elements in living cells and an essential constituent of proteins and nucleic acids, the two groups of substances that can be said to support life. The important nitrogen pools are soil organic matter, rocks (in fact the largest single pool), sediments, coal deposits, organic matter in ocean water, and nitrate in ocean water. The next most common gaseous form of nitrogen in the atmosphere after molecular nitrogen is dinitrogen oxide. The geochemistry of carbon is the transformations involving the element carbon within the systems of the earth. Carbon is important in the formation of organic mineral deposits, such as coal, petroleum, or natural gas. Most carbon is cycled through the atmosphere into living organisms and then respires back into the atmosphere. Carbon can form a huge variety of stable compound. It is an essential component of living matter. Carbon makes up only 0.08% of the combination of the lithosphere, hydrosphere, and atmosphere." @default.
• W4285189084 created "2022-07-14" @default.
• W4285189084 creator A5018152460 @default.
• W4285189084 date "2022-01-01" @default.
• W4285189084 modified "2023-09-24" @default.
• W4285189084 title "Geochemical Characteristics of Mineral Elements: Arsenic, Fluorine, Lead, Nitrogen, and Carbon" @default.
• W4285189084 cites W1503587868 @default.
• W4285189084 cites W1547515890 @default.
• W4285189084 cites W1587556598 @default.
• W4285189084 cites W1777939053 @default.
• W4285189084 cites W18275426 @default.
• W4285189084 cites W1831110431 @default.
• W4285189084 cites W1965375933 @default.
• W4285189084 cites W1967060945 @default.
• W4285189084 cites W1968763984 @default.
• W4285189084 cites W1969200105 @default.
• W4285189084 cites W1973295190 @default.
• W4285189084 cites W1975696034 @default.
• W4285189084 cites W1978895830 @default.
• W4285189084 cites W1982705178 @default.
• W4285189084 cites W1984580491 @default.
• W4285189084 cites W1985879113 @default.
• W4285189084 cites W1985986887 @default.
• W4285189084 cites W1986051618 @default.
• W4285189084 cites W1992323416 @default.
• W4285189084 cites W1998592288 @default.
• W4285189084 cites W2004386304 @default.
• W4285189084 cites W2004421695 @default.
• W4285189084 cites W2008104453 @default.
• W4285189084 cites W2009842135 @default.
• W4285189084 cites W2013310435 @default.
• W4285189084 cites W2013789293 @default.
• W4285189084 cites W2014016443 @default.
• W4285189084 cites W2017737086 @default.
• W4285189084 cites W2019185666 @default.
• W4285189084 cites W2020456104 @default.
• W4285189084 cites W2023128965 @default.
• W4285189084 cites W2025360735 @default.
• W4285189084 cites W2027530170 @default.
• W4285189084 cites W2031651844 @default.
• W4285189084 cites W2032170210 @default.
• W4285189084 cites W2032279745 @default.
• W4285189084 cites W2035697154 @default.
• W4285189084 cites W2040053099 @default.
• W4285189084 cites W2040372491 @default.
• W4285189084 cites W2041602982 @default.
• W4285189084 cites W2042676639 @default.
• W4285189084 cites W2042804530 @default.
• W4285189084 cites W2043313216 @default.
• W4285189084 cites W2045823138 @default.
• W4285189084 cites W2048547517 @default.
• W4285189084 cites W2050238167 @default.
• W4285189084 cites W2051601909 @default.
• W4285189084 cites W2059589790 @default.
• W4285189084 cites W2059981268 @default.
• W4285189084 cites W2070572356 @default.
• W4285189084 cites W2071959266 @default.
• W4285189084 cites W2072344106 @default.
• W4285189084 cites W2072463777 @default.
• W4285189084 cites W2073181949 @default.
• W4285189084 cites W2076942437 @default.
• W4285189084 cites W2078904194 @default.
• W4285189084 cites W2079193024 @default.
• W4285189084 cites W2079393793 @default.
• W4285189084 cites W2088904784 @default.
• W4285189084 cites W2091202236 @default.
• W4285189084 cites W2093447185 @default.
• W4285189084 cites W2093750105 @default.
• W4285189084 cites W2094165588 @default.
• W4285189084 cites W2095028285 @default.
• W4285189084 cites W2095684149 @default.
• W4285189084 cites W2097612426 @default.
• W4285189084 cites W2126398167 @default.
• W4285189084 cites W2126473104 @default.
• W4285189084 cites W2140056228 @default.
• W4285189084 cites W2140450505 @default.
• W4285189084 cites W2145039095 @default.
• W4285189084 cites W2149602337 @default.
• W4285189084 cites W2149658002 @default.
• W4285189084 cites W2153880563 @default.
• W4285189084 cites W2155665127 @default.
• W4285189084 cites W2159572730 @default.
• W4285189084 cites W2170133849 @default.
• W4285189084 cites W2228338508 @default.
• W4285189084 cites W2279972399 @default.
• W4285189084 cites W2324096461 @default.
• W4285189084 cites W2327884380 @default.
• W4285189084 cites W2330391579 @default.
• W4285189084 cites W2331316276 @default.
• W4285189084 cites W2409706137 @default.
• W4285189084 cites W2465494516 @default.
• W4285189084 cites W2552245604 @default.
• W4285189084 cites W2579437818 @default.
• W4285189084 cites W2604879868 @default.
• W4285189084 cites W2643580206 @default.
• W4285189084 cites W2660177118 @default.
• W4285189084 cites W2767247167 @default.
• W4285189084 cites W2791510185 @default.

• next