FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W4365143927> ?p ?o ?g. }

• W4365143927 endingPage "129513" @default.
• W4365143927 startingPage "129513" @default.
• W4365143927 abstract "Although degradation of phosphorus-containing natural organic matter (NOM) is an important process associated with geogenic phosphorus (P) enrichment, the detailed mechanism underlying the association remains unclear. Herein, we used molecular characteristics of P-containing dissolved organic matter (DOM) coupled with hydrogeochemistry and carbon isotopes to unravel this controlling mechanism. Results indicate that P-containing DOM is indeed an important factor controlling groundwater P enrichment. Further, one-P-atom (1P) and two-P-atom (2P) compounds were widely detected. Compared to 1P compounds, 2P compounds have greater numbers of N/S-containing compounds; smaller proportions of highly unsaturated and aliphatic compounds; larger proportions of polyphenols and polycyclic aromatics; lower H/C and nominal oxidation state of carbon (NOSC) values; and higher m/z, O/C, P/C, N/C, double bond equivalents (DBE), and modified aromaticity index (AImod) values. At the molecular level, P-containing DOM degradation overall results in an increase in H/C and a decrease in O/C, and a processing gradient is observed from 2P to 1P compounds, during which dissolved inorganic phosphorus (DIP) was gradually accumulated and retained, eventually becoming the predominating P pool in groundwater. To our knowledge, this is the first study to reveal geogenic P enrichment from a molecular perspective in groundwater systems worldwide." @default.
• W4365143927 created "2023-04-13" @default.
• W4365143927 creator A5001342446 @default.
• W4365143927 creator A5025546406 @default.
• W4365143927 creator A5045579735 @default.
• W4365143927 creator A5071392824 @default.
• W4365143927 creator A5083417541 @default.
• W4365143927 date "2023-05-01" @default.
• W4365143927 modified "2023-10-18" @default.
• W4365143927 title "Degradation of phosphorus-containing natural organic matter facilitates enrichment of geogenic phosphorus in Quaternary aquifer systems: A molecular perspective" @default.
• W4365143927 cites W1265902443 @default.
• W4365143927 cites W1494699847 @default.
• W4365143927 cites W1963913064 @default.
• W4365143927 cites W1965162447 @default.
• W4365143927 cites W1985016228 @default.
• W4365143927 cites W1985547002 @default.
• W4365143927 cites W1997623549 @default.
• W4365143927 cites W1999115302 @default.
• W4365143927 cites W1999900382 @default.
• W4365143927 cites W2005995746 @default.
• W4365143927 cites W2006694929 @default.
• W4365143927 cites W2027068200 @default.
• W4365143927 cites W2027479037 @default.
• W4365143927 cites W2031349127 @default.
• W4365143927 cites W2031723692 @default.
• W4365143927 cites W2033911809 @default.
• W4365143927 cites W2038982333 @default.
• W4365143927 cites W2039824236 @default.
• W4365143927 cites W2048550424 @default.
• W4365143927 cites W2052827499 @default.
• W4365143927 cites W2057373676 @default.
• W4365143927 cites W2058301964 @default.
• W4365143927 cites W2067369295 @default.
• W4365143927 cites W2074704891 @default.
• W4365143927 cites W2075435443 @default.
• W4365143927 cites W2078976583 @default.
• W4365143927 cites W2078986043 @default.
• W4365143927 cites W2087777284 @default.
• W4365143927 cites W2096033292 @default.
• W4365143927 cites W2101758912 @default.
• W4365143927 cites W2101923056 @default.
• W4365143927 cites W2107083991 @default.
• W4365143927 cites W2116105765 @default.
• W4365143927 cites W2119063929 @default.
• W4365143927 cites W2134341220 @default.
• W4365143927 cites W2156464790 @default.
• W4365143927 cites W2156863678 @default.
• W4365143927 cites W2164087962 @default.
• W4365143927 cites W2169406597 @default.
• W4365143927 cites W2272974840 @default.
• W4365143927 cites W2311522546 @default.
• W4365143927 cites W2328275042 @default.
• W4365143927 cites W2515236609 @default.
• W4365143927 cites W2554469697 @default.
• W4365143927 cites W2604787889 @default.
• W4365143927 cites W2610606104 @default.
• W4365143927 cites W2613422064 @default.
• W4365143927 cites W2735182719 @default.
• W4365143927 cites W2756390103 @default.
• W4365143927 cites W2788076750 @default.
• W4365143927 cites W2788166803 @default.
• W4365143927 cites W2804083434 @default.
• W4365143927 cites W2883522803 @default.
• W4365143927 cites W2905244135 @default.
• W4365143927 cites W2947574879 @default.
• W4365143927 cites W2965329238 @default.
• W4365143927 cites W2965935386 @default.
• W4365143927 cites W2968536698 @default.
• W4365143927 cites W2981088070 @default.
• W4365143927 cites W3002944674 @default.
• W4365143927 cites W3015607646 @default.
• W4365143927 cites W3015710173 @default.
• W4365143927 cites W3015889645 @default.
• W4365143927 cites W3022956552 @default.
• W4365143927 cites W3027974487 @default.
• W4365143927 cites W3032425706 @default.
• W4365143927 cites W3109561698 @default.
• W4365143927 cites W3112140407 @default.
• W4365143927 cites W3118530283 @default.
• W4365143927 cites W3132467928 @default.
• W4365143927 cites W3138862059 @default.
• W4365143927 cites W3145350805 @default.
• W4365143927 cites W3153415560 @default.
• W4365143927 cites W3173021124 @default.
• W4365143927 cites W3182279934 @default.
• W4365143927 cites W3202426557 @default.
• W4365143927 cites W3206587600 @default.
• W4365143927 cites W4200262712 @default.
• W4365143927 cites W4206543129 @default.
• W4365143927 cites W4207041485 @default.
• W4365143927 cites W4224241643 @default.
• W4365143927 cites W4224307644 @default.
• W4365143927 cites W4225152458 @default.
• W4365143927 cites W4280639127 @default.
• W4365143927 cites W4285004928 @default.
• W4365143927 cites W4312054179 @default.
• W4365143927 cites W4321596661 @default.
• W4365143927 doi "https://doi.org/10.1016/j.jhydrol.2023.129513" @default.

• next