FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W4382794133> ?p ?o ?g. }

• W4382794133 endingPage "e00678" @default.
• W4382794133 startingPage "e00678" @default.
• W4382794133 abstract "Soil organic matter (SOM) plays an important role in soil functions that are crucial for sustainable agriculture. Understanding how agricultural management and soil properties affect SOM in different soil depths would aid in maintaining and increasing SOM throughout the soil profile. We sampled a 24 year-old cultivation field experiment with organic and conventional cropping systems, and an adjacent unmanaged meadow to 70 cm soil depth to assess the total organic carbon (OC) stocks and the distribution of OC into mineral-associated (MAOM), particulate (POM) and dissolved (DOM) organic matter. We found that >83% of the soil OC was in the MAOM fraction, and that the distribution of OC across the MAOM, POM and DOM within a soil depth was not strongly affected by soil management. Largest OC stocks (169 t ha−1) together with the largest plant root biomass was found in the unmanaged meadow, which highlights the potential of deep-rooting plants in sequestering OC into the soil. The OC saturation state of the soil was assessed based on the clay to OC ratio and Hassink's Equation (Hassink 1997). Hassink's Equation seemed to underestimate the MAOM accrual capacity of these soils and thus overestimated soil OC saturation state, whereas the clay to OC ratio indicated potential for OC accrual in all soil depths, except for the meadow topsoil. These varying results suggest that the applied metric should be soil type and -depth specific. We also determined the contribution of clay content and aluminum and iron oxides in explaining the amount of total OC, MAOM-C and POM-C. In contrast to the aluminum and iron oxides, clay was not well correlated to any of the OC fractions below the 20 cm depth, suggesting that estimating the OC accrual potential of the deeper soil should not be based on the soil texture alone. Our results indicate that aluminum and iron oxides can play an important role in transporting and stabilizing of OC in the soil profile." @default.
• W4382794133 created "2023-07-02" @default.
• W4382794133 creator A5015109819 @default.
• W4382794133 creator A5017167010 @default.
• W4382794133 creator A5051748218 @default.
• W4382794133 creator A5052002505 @default.
• W4382794133 creator A5053391921 @default.
• W4382794133 creator A5063014136 @default.
• W4382794133 creator A5076940449 @default.
• W4382794133 creator A5092375311 @default.
• W4382794133 date "2023-09-01" @default.
• W4382794133 modified "2023-10-15" @default.
• W4382794133 title "Assessing the effect of arable management practices on carbon storage and fractions after 24 years in boreal conditions of Finland" @default.
• W4382794133 cites W1854601995 @default.
• W4382794133 cites W1984412649 @default.
• W4382794133 cites W1995548542 @default.
• W4382794133 cites W1997095959 @default.
• W4382794133 cites W2004724527 @default.
• W4382794133 cites W2005742515 @default.
• W4382794133 cites W2006371148 @default.
• W4382794133 cites W2016748612 @default.
• W4382794133 cites W2022246075 @default.
• W4382794133 cites W2024143738 @default.
• W4382794133 cites W2027841418 @default.
• W4382794133 cites W2032333242 @default.
• W4382794133 cites W2036677268 @default.
• W4382794133 cites W2044716830 @default.
• W4382794133 cites W2050109729 @default.
• W4382794133 cites W2052944181 @default.
• W4382794133 cites W2053043516 @default.
• W4382794133 cites W2065492690 @default.
• W4382794133 cites W2065793428 @default.
• W4382794133 cites W2067019078 @default.
• W4382794133 cites W2080666601 @default.
• W4382794133 cites W2083039584 @default.
• W4382794133 cites W2083469864 @default.
• W4382794133 cites W2098056980 @default.
• W4382794133 cites W2108744281 @default.
• W4382794133 cites W2118355172 @default.
• W4382794133 cites W2121124271 @default.
• W4382794133 cites W2130931170 @default.
• W4382794133 cites W2133491912 @default.
• W4382794133 cites W2136596893 @default.
• W4382794133 cites W2141706238 @default.
• W4382794133 cites W2149454849 @default.
• W4382794133 cites W2151452399 @default.
• W4382794133 cites W2160917602 @default.
• W4382794133 cites W2163103579 @default.
• W4382794133 cites W2168708206 @default.
• W4382794133 cites W2170062386 @default.
• W4382794133 cites W2328487243 @default.
• W4382794133 cites W2508157630 @default.
• W4382794133 cites W2557800876 @default.
• W4382794133 cites W2604924672 @default.
• W4382794133 cites W2612845390 @default.
• W4382794133 cites W2742336425 @default.
• W4382794133 cites W2769855170 @default.
• W4382794133 cites W2787390971 @default.
• W4382794133 cites W2799618837 @default.
• W4382794133 cites W2883893555 @default.
• W4382794133 cites W2884069169 @default.
• W4382794133 cites W2968761745 @default.
• W4382794133 cites W2977539872 @default.
• W4382794133 cites W2985814312 @default.
• W4382794133 cites W2997398790 @default.
• W4382794133 cites W2998870886 @default.
• W4382794133 cites W3016568429 @default.
• W4382794133 cites W3017347101 @default.
• W4382794133 cites W3029923327 @default.
• W4382794133 cites W3031544283 @default.
• W4382794133 cites W3035753901 @default.
• W4382794133 cites W3036384722 @default.
• W4382794133 cites W3055516953 @default.
• W4382794133 cites W3084241901 @default.
• W4382794133 cites W3105485802 @default.
• W4382794133 cites W3135555326 @default.
• W4382794133 cites W3158251375 @default.
• W4382794133 cites W3159388573 @default.
• W4382794133 cites W3186189556 @default.
• W4382794133 cites W3202416625 @default.
• W4382794133 cites W3207827237 @default.
• W4382794133 cites W4221102947 @default.
• W4382794133 cites W4280505419 @default.
• W4382794133 cites W4282582837 @default.
• W4382794133 cites W4283743401 @default.
• W4382794133 cites W4284883654 @default.
• W4382794133 cites W4289782010 @default.
• W4382794133 cites W44923620 @default.
• W4382794133 doi "https://doi.org/10.1016/j.geodrs.2023.e00678" @default.
• W4382794133 hasPublicationYear "2023" @default.
• W4382794133 type Work @default.
• W4382794133 citedByCount "0" @default.
• W4382794133 crossrefType "journal-article" @default.
• W4382794133 hasAuthorship W4382794133A5015109819 @default.
• W4382794133 hasAuthorship W4382794133A5017167010 @default.
• W4382794133 hasAuthorship W4382794133A5051748218 @default.
• W4382794133 hasAuthorship W4382794133A5052002505 @default.
• W4382794133 hasAuthorship W4382794133A5053391921 @default.

• next