A study on the Soil Carbon Cycle in Temperate Deciduous and Evergreen Coniferous Forests

2006 ◽  
Vol 4 (3) ◽  
pp. 157-168
Author(s):  
Youn-Kyung MIN ◽  
Eun-Hye LEE ◽  
JaeSeok LEE
Forests ◽  
2021 ◽  
Vol 12 (1) ◽  
pp. 89
Author(s):  
Hong Wei ◽  
Xiuling Man

The change of litter input can affect soil respiration (Rs) by influencing the availability of soil organic carbon and nutrients, regulating soil microenvironments, thus resulting in a profound influence on soil carbon cycle of the forest ecosystem. We conducted an aboveground litterfall manipulation experiment in different-aged Betula platyphylla forests (25-, 40- and 61-year-old) of the permafrost region, located in the northeast of China, during May to October in 2018, with each stand treated with doubling litter (litter addition, DL), litter exclusion (no-litter, NL) and control litter (CK). Our results indicated that Rs decreased under NL treatment compared with CK treatment. The effect size lessened with the increase in the stand age; the greatest reduction was found for young Betula platyphylla forest (24.46% for 25-year-old stand) and tended to stabilize with the growth of forest with the reduction of 15.65% and 15.23% for 40-and 61- year-old stands, respectively. Meanwhile, under DL treatment, Rs increased by 27.38%, 23.83% and 23.58% on 25-, 40- and 61-year-old stands, respectively. Our results also showed that the increase caused by DL treatment was larger than the reduction caused by NL treatment, leading to a priming effect, especially on 40- and 61-year-old stands. The change in litter input was the principal factor affecting the change of Rs under litter manipulation. The soil temperature was also a main factor affecting the contribution rate of litter to Rs of different-aged stands, which had a significant positive exponential correlation with Rs. This suggests that there is a significant relationship between litter and Rs, which consequently influences the soil carbon cycle in Betula platyphylla forests of the permafrost region, Northeast China. Our finding indicated the increased litter enhanced the Rs in Betula platyphylla forest, which may consequently increase the carbon emission in a warming climate in the future. It is of great importance for future forest management in the permafrost region, Northeast China.


2009 ◽  
Vol 97 (5) ◽  
pp. 840-850 ◽  
Author(s):  
F. Stuart Chapin III ◽  
Jack McFarland ◽  
A. David McGuire ◽  
Eugenie S. Euskirchen ◽  
Roger W. Ruess ◽  
...  

2018 ◽  
Vol 30 (5) ◽  
pp. 1260-1270 ◽  
Author(s):  
SHEN Ruichang ◽  
◽  
LAN Zhichun ◽  
FANG Changming ◽  
CHEN Jiakuan
Keyword(s):  

2020 ◽  
Author(s):  
Minttu Havu ◽  
Liisa Kulmala ◽  
Anu Riikonen ◽  
Leena Järvi

<p>A <span>high proportion of anthropogenic carbon dioxide emissions </span><span>originate from</span><span> urban areas, which has led cities to become interested in reducing their own emissions and </span><span>determining</span><span> how much carbon could be sequestered by their own vegetation and soil. </span><span>The challenge with the latter is that our current knowledge on carbon storage is based on data and models from natural and forest ecosystems, whereas</span><span> the response of vegetation and soil to environmental factors most probably is altered in urban green space where the soil conditions, water availability </span><span>and</span><span> temperature are highly variable.</span> <span>T</span><span>herefore</span><span>, </span><span>ecosystem models </span><span>are required to </span><span>correctly account for urban vegetation</span> <span>and soil </span><span>to understand </span><span>and quantify</span><span> the biogenic carbon cycle in urban areas. </span></p><p><span>I</span><span>n this study, urban land surface model SUEWS </span><span>(</span><span>the </span><span>Surface Urban Energy and Water Balance Scheme</span><span>)</span> <span>and </span><span>t</span><span>he soil carbon decomposition model Yasso</span><span>15</span> <span>are used to simulate urban carbon cycle on two street</span><span>s</span> <span>in Helsinki, Finland for years 2003-2016. </span><span>Curbside trees (<em>Alnus glutinosa </em>and<em> Tilia </em></span><em><span>x Vulgaris</span></em><span>) were planted while the two test streets were constructed in 2002. Thereafter</span><span>, carbon and water fluxes </span><span>and </span><span>pools</span> <span>with detailed street tree soil composition</span><span>s</span> <span>were</span><span> monitored in</span><span> 2002-2014. </span><span>SUEWS creates a local spatially variable temperature and specific humidity environment which is used in the model runs. </span><span>The modelled evaporation i</span><span>s</span><span> evaluated against sap flow measurements and modelled soil moisture against soil moisture observations. </span><span>The </span><span>Yasso</span><span>15</span><span> model i</span><span>s</span><span> evaluated against loss-on-ignition based soil carbon measurements </span><span>as </span><span>it has not been </span><span>previously </span><span>evaluated </span><span>in urban soils. </span><span>T</span><span>he </span><span>modelled</span><span> carbon dioxide flux combined with the </span><span>changes in the</span><span> soil carbon stock is used t</span><span>o estimate the carbon cycle of ur</span><span>ban street </span><span>trees and soils.</span></p>


1994 ◽  
Vol 74 (3-4) ◽  
pp. 183-204 ◽  
Author(s):  
Naohiro Goto ◽  
Akiyoshi Sakoda ◽  
Motoyuki Suzuki

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