FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2893824264> ?p ?o ?g. }

• W2893824264 endingPage "598" @default.
• W2893824264 startingPage "598" @default.
• W2893824264 abstract "Understanding the association between soil organic carbon (SOC) and texture under different climatic conditions is important for assessing the effects of future climate changes on SOC stocks. In this study, we conducted a climatic gradient experiment covering three climate types (humid, sub-humid, and semi-arid) with a steep rainfall ranging from 345 to 910 mm, and specifically determined SOC dynamics, clay content, and vegetation and soil characteristics. The results showed that, from semi-arid to humid regions, SOC stocks, SOC, and clay content increased synchronously and were closely related in layers of depths of both 0–10 and 10–20 cm. In contrast, under similar climatic conditions, SOC dynamics were mainly affected by vegetation and soil characteristics, especially total nitrogen and total phosphorus dynamics, but not the soil clay content. Therefore, these results suggest that the relationship between SOC stocks and clay content depended on scale sizes. Specifically, on a larger scale with different climatic gradients, the climate may partly determine the changes in SOC and clay dynamics, whereas, at a smaller scale where climate type does not vary considerably, the changes in SOC stocks and clay content may be related to vegetation diversity and soil nutrient dynamics. These results may contribute to future model development and the projection of changes in soil carbon storage." @default.
• W2893824264 created "2018-10-05" @default.
• W2893824264 creator A5008479914 @default.
• W2893824264 creator A5010176677 @default.
• W2893824264 creator A5042282426 @default.
• W2893824264 creator A5043749183 @default.
• W2893824264 creator A5044765535 @default.
• W2893824264 creator A5050009045 @default.
• W2893824264 creator A5061016096 @default.
• W2893824264 creator A5066378778 @default.
• W2893824264 date "2018-09-26" @default.
• W2893824264 modified "2023-10-06" @default.
• W2893824264 title "Relationship between Soil Organic Carbon Stocks and Clay Content under Different Climatic Conditions in Central China" @default.
• W2893824264 cites W1505506133 @default.
• W2893824264 cites W1509114248 @default.
• W2893824264 cites W1635165580 @default.
• W2893824264 cites W1784792506 @default.
• W2893824264 cites W1880854489 @default.
• W2893824264 cites W1929306868 @default.
• W2893824264 cites W1946277022 @default.
• W2893824264 cites W1968092043 @default.
• W2893824264 cites W1971157211 @default.
• W2893824264 cites W1973115799 @default.
• W2893824264 cites W1973123372 @default.
• W2893824264 cites W1976172944 @default.
• W2893824264 cites W1988491595 @default.
• W2893824264 cites W1999537921 @default.
• W2893824264 cites W2000291905 @default.
• W2893824264 cites W20009899 @default.
• W2893824264 cites W2007735691 @default.
• W2893824264 cites W2012456614 @default.
• W2893824264 cites W2015069075 @default.
• W2893824264 cites W2016043919 @default.
• W2893824264 cites W2016680202 @default.
• W2893824264 cites W2020293329 @default.
• W2893824264 cites W2021586624 @default.
• W2893824264 cites W2023900583 @default.
• W2893824264 cites W2024594986 @default.
• W2893824264 cites W2032638770 @default.
• W2893824264 cites W2041076013 @default.
• W2893824264 cites W2043711420 @default.
• W2893824264 cites W2045760167 @default.
• W2893824264 cites W2047438552 @default.
• W2893824264 cites W2050928551 @default.
• W2893824264 cites W2052289430 @default.
• W2893824264 cites W2065784770 @default.
• W2893824264 cites W2069667737 @default.
• W2893824264 cites W2075680945 @default.
• W2893824264 cites W2083355713 @default.
• W2893824264 cites W2083857556 @default.
• W2893824264 cites W2090602773 @default.
• W2893824264 cites W2105427050 @default.
• W2893824264 cites W2131790774 @default.
• W2893824264 cites W2138540827 @default.
• W2893824264 cites W2141706238 @default.
• W2893824264 cites W2143791347 @default.
• W2893824264 cites W2146351313 @default.
• W2893824264 cites W2153944160 @default.
• W2893824264 cites W2167638494 @default.
• W2893824264 cites W2174069807 @default.
• W2893824264 cites W2203137389 @default.
• W2893824264 cites W2396882737 @default.
• W2893824264 cites W2500473094 @default.
• W2893824264 cites W2511521053 @default.
• W2893824264 cites W2548216028 @default.
• W2893824264 cites W2595520191 @default.
• W2893824264 cites W2603868411 @default.
• W2893824264 cites W2610256562 @default.
• W2893824264 cites W2620871096 @default.
• W2893824264 cites W318143065 @default.
• W2893824264 cites W4233132870 @default.
• W2893824264 cites W44923620 @default.
• W2893824264 doi "https://doi.org/10.3390/f9100598" @default.
• W2893824264 hasPublicationYear "2018" @default.
• W2893824264 type Work @default.
• W2893824264 sameAs 2893824264 @default.
• W2893824264 citedByCount "54" @default.
• W2893824264 countsByYear W28938242642019 @default.
• W2893824264 countsByYear W28938242642020 @default.
• W2893824264 countsByYear W28938242642021 @default.
• W2893824264 countsByYear W28938242642022 @default.
• W2893824264 countsByYear W28938242642023 @default.
• W2893824264 crossrefType "journal-article" @default.
• W2893824264 hasAuthorship W2893824264A5008479914 @default.
• W2893824264 hasAuthorship W2893824264A5010176677 @default.
• W2893824264 hasAuthorship W2893824264A5042282426 @default.
• W2893824264 hasAuthorship W2893824264A5043749183 @default.
• W2893824264 hasAuthorship W2893824264A5044765535 @default.
• W2893824264 hasAuthorship W2893824264A5050009045 @default.
• W2893824264 hasAuthorship W2893824264A5061016096 @default.
• W2893824264 hasAuthorship W2893824264A5066378778 @default.
• W2893824264 hasBestOaLocation W28938242641 @default.
• W2893824264 hasConcept C142724271 @default.
• W2893824264 hasConcept C150772632 @default.
• W2893824264 hasConcept C158787203 @default.
• W2893824264 hasConcept C159390177 @default.
• W2893824264 hasConcept C159750122 @default.
• W2893824264 hasConcept C175963888 @default.

• next