FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W3208233735> ?p ?o ?g. }

• W3208233735 endingPage "105811" @default.
• W3208233735 startingPage "105811" @default.
• W3208233735 abstract "Alpine marsh wetlands in the Qinghai-Tibetan Plateau are ecological hotspots for global carbon (C) cycling in Central Asia; however, the soil C sinks are increasingly limited by marsh degradation. To assess the physical mechanisms by which changes in the soil C sequestration occur, the distribution and functional groups of soil organic C (SOC) in aggregates along a marsh degradation gradient on the Zoige Plateau in China were investigated using soil samples collected from differently degraded marshes. Our results showed that, beyond the state of light degradation, the large aggregate content decreased significantly by 31.1–55.2%, while the micro-aggregate content increased significantly by 23.1–93.1%. The SOC content in the aggregates decreased significantly by 39.1–84.8% and the dominant aggregate size for SOC preservation decreased to small or micro-aggregate. Marsh degradation also decreased the relative ratio of aliphatic-C while increasing that of alcohol and phenolic-C, and polysaccharide-C. Index I (relative decomposition of SOC in aggregates) was 73.5–429.0% higher for degraded marshes than for relatively pristine marsh (RPM), while Index Ⅱ (relative recalcitrance of SOC in aggregates) was 13.8–79.5% lower in comparison. Therefore, we concluded that marsh degradation probably reduces the organic C sequestration capacity of soil by increasing the decomposition of SOC in aggregates after both the dominant aggregate size for SOC preservation and aggregate stability decreased. This result represents the physical mechanism by which the decrease in SOC content occurs in response to marsh degradation in alpine regions." @default.
• W3208233735 created "2021-11-08" @default.
• W3208233735 creator A5001073522 @default.
• W3208233735 creator A5012285321 @default.
• W3208233735 creator A5013994054 @default.
• W3208233735 creator A5019301540 @default.
• W3208233735 creator A5023652915 @default.
• W3208233735 creator A5025068726 @default.
• W3208233735 creator A5034294824 @default.
• W3208233735 creator A5042627775 @default.
• W3208233735 creator A5046971352 @default.
• W3208233735 creator A5065702785 @default.
• W3208233735 creator A5088178128 @default.
• W3208233735 date "2022-02-01" @default.
• W3208233735 modified "2023-10-11" @default.
• W3208233735 title "Distribution and functional groups of soil aggregate-associated organic carbon along a marsh degradation gradient on the Zoige Plateau, China" @default.
• W3208233735 cites W1834026011 @default.
• W3208233735 cites W1897334513 @default.
• W3208233735 cites W1963551755 @default.
• W3208233735 cites W1970917249 @default.
• W3208233735 cites W1981306206 @default.
• W3208233735 cites W1982281110 @default.
• W3208233735 cites W1997247670 @default.
• W3208233735 cites W2002879827 @default.
• W3208233735 cites W2004320529 @default.
• W3208233735 cites W2006415937 @default.
• W3208233735 cites W2010398974 @default.
• W3208233735 cites W2015831987 @default.
• W3208233735 cites W2016936138 @default.
• W3208233735 cites W2023109102 @default.
• W3208233735 cites W2024893881 @default.
• W3208233735 cites W2025565779 @default.
• W3208233735 cites W2030676847 @default.
• W3208233735 cites W2034992241 @default.
• W3208233735 cites W2055185339 @default.
• W3208233735 cites W2064882470 @default.
• W3208233735 cites W2065739302 @default.
• W3208233735 cites W2066459710 @default.
• W3208233735 cites W2069711718 @default.
• W3208233735 cites W2072404034 @default.
• W3208233735 cites W2072627116 @default.
• W3208233735 cites W2088732854 @default.
• W3208233735 cites W2091283551 @default.
• W3208233735 cites W2091595754 @default.
• W3208233735 cites W2106186009 @default.
• W3208233735 cites W2112754872 @default.
• W3208233735 cites W2139405554 @default.
• W3208233735 cites W2288048810 @default.
• W3208233735 cites W2401255309 @default.
• W3208233735 cites W2511810226 @default.
• W3208233735 cites W2523419460 @default.
• W3208233735 cites W2533694640 @default.
• W3208233735 cites W2555748705 @default.
• W3208233735 cites W2561029067 @default.
• W3208233735 cites W2609242197 @default.
• W3208233735 cites W2609362419 @default.
• W3208233735 cites W2613408791 @default.
• W3208233735 cites W2619904803 @default.
• W3208233735 cites W2727623211 @default.
• W3208233735 cites W2735488265 @default.
• W3208233735 cites W2743628685 @default.
• W3208233735 cites W2748177257 @default.
• W3208233735 cites W2766220902 @default.
• W3208233735 cites W2786240385 @default.
• W3208233735 cites W2791069628 @default.
• W3208233735 cites W2792773138 @default.
• W3208233735 cites W2940448630 @default.
• W3208233735 cites W2943749046 @default.
• W3208233735 cites W2946348327 @default.
• W3208233735 cites W2947827378 @default.
• W3208233735 cites W2949485741 @default.
• W3208233735 cites W2971696808 @default.
• W3208233735 cites W2981445342 @default.
• W3208233735 cites W2998285560 @default.
• W3208233735 cites W3020390489 @default.
• W3208233735 cites W3023032364 @default.
• W3208233735 cites W3040526967 @default.
• W3208233735 cites W3095631716 @default.
• W3208233735 cites W3096852434 @default.
• W3208233735 doi "https://doi.org/10.1016/j.catena.2021.105811" @default.
• W3208233735 hasPublicationYear "2022" @default.
• W3208233735 type Work @default.
• W3208233735 sameAs 3208233735 @default.
• W3208233735 citedByCount "9" @default.
• W3208233735 countsByYear W32082337352022 @default.
• W3208233735 countsByYear W32082337352023 @default.
• W3208233735 crossrefType "journal-article" @default.
• W3208233735 hasAuthorship W3208233735A5001073522 @default.
• W3208233735 hasAuthorship W3208233735A5012285321 @default.
• W3208233735 hasAuthorship W3208233735A5013994054 @default.
• W3208233735 hasAuthorship W3208233735A5019301540 @default.
• W3208233735 hasAuthorship W3208233735A5023652915 @default.
• W3208233735 hasAuthorship W3208233735A5025068726 @default.
• W3208233735 hasAuthorship W3208233735A5034294824 @default.
• W3208233735 hasAuthorship W3208233735A5042627775 @default.
• W3208233735 hasAuthorship W3208233735A5046971352 @default.
• W3208233735 hasAuthorship W3208233735A5065702785 @default.
• W3208233735 hasAuthorship W3208233735A5088178128 @default.

• next