FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W3021571844> ?p ?o ?g. }

• W3021571844 endingPage "106557" @default.
• W3021571844 startingPage "106557" @default.
• W3021571844 abstract "This study aims to better understand, at a regional scale, the concentration and distribution of selected chemical elements in surface environments and the influence of natural factors (geological background, geomorphology) and anthropogenic factors (mining activities, land-use, agricultural fertilization) on their distribution in the Baoshan area, Yunnan province, southwest China. Mineral resources (such as copper, lead, zinc, mercury, gold, silver) and carbonate and basalt parent materials in this area often lead to elevated potentially toxic metals (PTMs), which are widely distributed where mining activities have rapidly developed since last 20–30 years. This study makes use of 1574 surface soil data and 425 deep soil data from the National Geochemistry Survey of Land Quality project (NGSLQ), and 1585 archived river sediment data which were collected and analyzed for the Regional Geochemistry-National Reconnaissance program (RGNR). These data, once log-ratio (clr) transformed have been studied by compositional data analysis (CoDA), principle components analysis (PCA) and spatial analysis. In the Baoshan area, the concentration of elements As, B, (Br), Co, Cr, Cu, Hg, (I), Mn, (N), Ni, Sb, (Sc), (Se), V, Fe2O3Total and (COrgonic) are enriched compared to the China Soil Geochemical Baselines program (CGB) and RGNR data sets; while elements Sr and Na2O are depleted compared to CGB and RGNR data sets. Influencing factors on surface soil, deep soil and river sediment composition of the study area are revealed. The distribution of most elements in surface soil, deep soil and river sediment are influenced by natural factors such that: Co, Cr, Cu, Ni, Sc, Ti, V, Fe2O3Total and MgO are controlled by the distribution of basic igneous rocks; Ca, Mg, Sr and pH are controlled by the distribution of carbonate rocks and basic igneous rocks; As, Hg, Sb, (Ag), Cd, Pb and Zn are controlled by mineralization; and other elements normally controlled by the distribution of clastic rocks and acid-intermediate rocks; while the organic matter such as Br, N, (P), S, COrgonic and CTotal in soil data set are controlled by geomorphic (altitude and temperature). Anthropogenic factors are also recognized in the soil data set. For example: high pH values in paddy land and grassland, and low pH values in forested land, garden plot and dry cultivated land; in agricultural area fertilization has caused enrichment of the nutrient elements (COrgonic, CTotal, N, P, etc.,) in surface soil; while in areas of mining, surface soils are contaminated by PTMs (incl. Hg, As, Sb, Cu, Pb, Zn and Cd)." @default.
• W3021571844 created "2020-05-13" @default.
• W3021571844 creator A5004668248 @default.
• W3021571844 creator A5046122727 @default.
• W3021571844 creator A5058244415 @default.
• W3021571844 creator A5071038974 @default.
• W3021571844 creator A5073742976 @default.
• W3021571844 creator A5083105570 @default.
• W3021571844 creator A5090170346 @default.
• W3021571844 date "2020-10-01" @default.
• W3021571844 modified "2023-10-01" @default.
• W3021571844 title "A regional soil and river sediment geochemical study in Baoshan area, Yunnan province, southwest China" @default.
• W3021571844 cites W1169224977 @default.
• W3021571844 cites W1895572872 @default.
• W3021571844 cites W1964197427 @default.
• W3021571844 cites W1969742642 @default.
• W3021571844 cites W1969804536 @default.
• W3021571844 cites W1971853600 @default.
• W3021571844 cites W1971871493 @default.
• W3021571844 cites W1972687402 @default.
• W3021571844 cites W1974285157 @default.
• W3021571844 cites W1974921304 @default.
• W3021571844 cites W1977699688 @default.
• W3021571844 cites W1978631402 @default.
• W3021571844 cites W1980240087 @default.
• W3021571844 cites W1980480753 @default.
• W3021571844 cites W1993072786 @default.
• W3021571844 cites W1998146383 @default.
• W3021571844 cites W2009009124 @default.
• W3021571844 cites W2009326065 @default.
• W3021571844 cites W2009735920 @default.
• W3021571844 cites W2016690206 @default.
• W3021571844 cites W2017547066 @default.
• W3021571844 cites W2019281114 @default.
• W3021571844 cites W2027714403 @default.
• W3021571844 cites W2032453821 @default.
• W3021571844 cites W2042055101 @default.
• W3021571844 cites W2046817159 @default.
• W3021571844 cites W2049156425 @default.
• W3021571844 cites W2049443361 @default.
• W3021571844 cites W2054934915 @default.
• W3021571844 cites W2058927331 @default.
• W3021571844 cites W2066440888 @default.
• W3021571844 cites W2066615414 @default.
• W3021571844 cites W2076183751 @default.
• W3021571844 cites W2077698224 @default.
• W3021571844 cites W2078112764 @default.
• W3021571844 cites W2081027781 @default.
• W3021571844 cites W2081984256 @default.
• W3021571844 cites W2082699707 @default.
• W3021571844 cites W2085762065 @default.
• W3021571844 cites W2087760944 @default.
• W3021571844 cites W2088725912 @default.
• W3021571844 cites W2089813368 @default.
• W3021571844 cites W2091702354 @default.
• W3021571844 cites W2093383935 @default.
• W3021571844 cites W2097149005 @default.
• W3021571844 cites W2116035387 @default.
• W3021571844 cites W2123785532 @default.
• W3021571844 cites W2132447898 @default.
• W3021571844 cites W2140628857 @default.
• W3021571844 cites W2143875387 @default.
• W3021571844 cites W2148722605 @default.
• W3021571844 cites W2150494400 @default.
• W3021571844 cites W2160628140 @default.
• W3021571844 cites W2168162834 @default.
• W3021571844 cites W2207209165 @default.
• W3021571844 cites W2377009255 @default.
• W3021571844 cites W2468081463 @default.
• W3021571844 cites W2525110493 @default.
• W3021571844 cites W2554392785 @default.
• W3021571844 cites W2554942105 @default.
• W3021571844 cites W2592476837 @default.
• W3021571844 cites W2622835792 @default.
• W3021571844 cites W2757775548 @default.
• W3021571844 cites W2766679144 @default.
• W3021571844 cites W2780420342 @default.
• W3021571844 cites W2793399348 @default.
• W3021571844 cites W2886341438 @default.
• W3021571844 cites W2905114723 @default.
• W3021571844 cites W2909859221 @default.
• W3021571844 cites W2914545537 @default.
• W3021571844 cites W2924907057 @default.
• W3021571844 cites W2952634005 @default.
• W3021571844 cites W2967407320 @default.
• W3021571844 cites W4242357899 @default.
• W3021571844 doi "https://doi.org/10.1016/j.gexplo.2020.106557" @default.
• W3021571844 hasPublicationYear "2020" @default.
• W3021571844 type Work @default.
• W3021571844 sameAs 3021571844 @default.
• W3021571844 citedByCount "11" @default.
• W3021571844 countsByYear W30215718442020 @default.
• W3021571844 countsByYear W30215718442021 @default.
• W3021571844 countsByYear W30215718442022 @default.
• W3021571844 countsByYear W30215718442023 @default.
• W3021571844 crossrefType "journal-article" @default.
• W3021571844 hasAuthorship W3021571844A5004668248 @default.
• W3021571844 hasAuthorship W3021571844A5046122727 @default.

• next