Soil parent material and stand development stage effects on labile soil C and N pools in Chinese fir plantations

Geoderma ◽  
2019 ◽  
Vol 338 ◽  
pp. 247-258 ◽  
Author(s):  
Yun Zhang ◽  
Mulualem Tigabu ◽  
Zhigang Yi ◽  
Huitong Li ◽  
Zheng Zhuang ◽  
...  
Pedosphere ◽  
2006 ◽  
Vol 16 (1) ◽  
pp. 56-63 ◽  
Author(s):  
Jian-Fen GUO ◽  
Yu-Sheng YANG ◽  
Guang-Shui CHEN ◽  
Jin-Sheng XIE ◽  
Peng LIN

2007 ◽  
Vol 120 (2-4) ◽  
pp. 250-258 ◽  
Author(s):  
I.K. Okore ◽  
H. Tijani-Eniola ◽  
A.A. Agboola ◽  
E.A. Aiyelari

2004 ◽  
Vol 34 (3) ◽  
pp. 509-518 ◽  
Author(s):  
J Bauhus ◽  
T Vor ◽  
N Bartsch ◽  
A Cowling

Despite the importance of gaps in the dynamics and management of many forest types, very little is known about the medium- to long-term soil C and N dynamics associated with this disturbance. This study was designed to test the hypothesis that gap creation and lime application, a routine measure in many European forests to ameliorate soil acidity, lead to accelerated litter decomposition and thus a reduction in the forest floor and soil C and N pools. Four gaps were created in 1989 in a mature European beech (Fagus sylvatica L.) forest on acid soil with a moder humus, and lime (3 t dolomite·ha–1) was applied to two of these and surrounding areas. Litter and fine-root decomposition was measured in 1992–1993 and 1996–1998 using litterbags. Forest floor (L, F, and H layers) and mineral soil (0–40 cm) C and N pools were determined in 1989 and 1997. Eight years following silvicultural treatments, there was no change in C and N over the entire forest soil profile including forest floor. Reductions in the F and H layers in limed gaps were compensated for by increases in soil C and N in the surface (0–10 cm) mineral soil. Decomposition of F litter was significantly accelerated in limed gaps, leading to the development of a mull–moder, whereas gap creation alone had no effect on mass loss of F material in litterbags. Gap size disturbances in this acid beech forest appear to have minimal influences on soil C and N stocks. However, when combined with liming, changes in the humus form and vertical distribution of soil C and N may occur.


2013 ◽  
Vol 13 (4) ◽  
pp. 641-653 ◽  
Author(s):  
María Almagro ◽  
José Ignacio Querejeta ◽  
Carolina Boix-Fayos ◽  
María Martínez-Mena

2014 ◽  
Vol 312 ◽  
pp. 161-169 ◽  
Author(s):  
Yongfu Li ◽  
Jiaojiao Zhang ◽  
Scott X. Chang ◽  
Peikun Jiang ◽  
Guomo Zhou ◽  
...  

Biology ◽  
2021 ◽  
Vol 10 (1) ◽  
pp. 23 ◽  
Author(s):  
Eren Taskin ◽  
Roberta Boselli ◽  
Andrea Fiorini ◽  
Chiara Misci ◽  
Federico Ardenti ◽  
...  

Combining no-till and cover crops (NT + CC) as an alternative to conventional tillage (CT) is generating interest to build-up farming systems’ resilience while promoting climate change adaptation in agriculture. Our field study aimed to assess the impact of long-term NT + CC management and short-term water stress on soil microbial communities, enzymatic activities, and the distribution of C and N within soil aggregates. High-throughput sequencing (HTS) revealed the positive impact of NT + CC on microbial biodiversity, especially under water stress conditions, with the presence of important rhizobacteria (e.g., Bradyrhizobium spp.). An alteration index based on soil enzymes confirmed soil depletion under CT. C and N pools within aggregates showed an enrichment under NT + CC mostly due to C and N-rich large macroaggregates (LM), accounting for 44% and 33% of the total soil C and N. Within LM, C and N pools were associated to microaggregates within macroaggregates (mM), which are beneficial for long-term C and N stabilization in soils. Water stress had detrimental effects on aggregate formation and limited C and N inclusion within aggregates. The microbiological and physicochemical parameters correlation supported the hypothesis that long-term NT + CC is a promising alternative to CT, due to the contribution to soil C and N stabilization while enhancing the biodiversity and enzymes.


2006 ◽  
Vol 38 (7) ◽  
pp. 1943-1955 ◽  
Author(s):  
Thomas L. Thompson ◽  
Eli Zaady ◽  
Pang Huancheng ◽  
Thomas B. Wilson ◽  
Dean A. Martens
Keyword(s):  
Soil C ◽  
C And N ◽  

Ecology ◽  
2005 ◽  
Vol 86 (2) ◽  
pp. 419-430 ◽  
Author(s):  
Anita C. Risch ◽  
Martin F. Jurgensen ◽  
Martin Schütz ◽  
Deborah S. Page-Dumroese

Ecosystems ◽  
2020 ◽  
Author(s):  
T. Persson ◽  
S. Andersson ◽  
J. Bergholm ◽  
T. Grönqvist ◽  
L. Högbom ◽  
...  

Abstract Liming can counteract acidification in forest soils, but the effects on soil C and N pools and fluxes over long periods are less well understood. Replicated plots in an acidic and N-rich 40-year-old Norway spruce (Picea abies) forest in SW Sweden (Hasslöv) were treated with 0, 3.45 and 8.75 Mg ha−1 of dolomitic lime (D0, D2 and D3) in 1984. Between 1984 and 2016, soil organic C to 30 cm depth increased by 28 Mg ha−1 (30% increase) in D0 and decreased by 9 Mg ha−1 (9.4% decrease) in D3. The change in D2 was not significant (+ 2 Mg ha−1). Soil N pools changed proportionally to those in soil C pools. The C and N changes occurred almost exclusively in the top organic layer. Non-burrowing earthworms responded positively to liming and stimulated heterotrophic respiration in this layer in both D2 and D3. Burrowing earthworms in D3 further accelerated C and N turnover and loss of soil. The high soil C and N loss at our relatively N-rich site differs from studies of N-poor sites showing no C and N loss. Earthworms need both high pH and N-rich food to reach high abundance and biomass. This can explain why liming of N-rich soils often results in decreasing C and N pools, whereas liming of N-poor soils with few earthworms will not show any change in soil C and N. Extractable nitrate N was always higher in D3 than in D2 and D0. After 6 years (1990), potential nitrification was much higher in D3 (197 kg N ha−1) than in D0 (36 kg N ha−1), but this difference decreased during the following years, when also the unlimed organic layers showed high nitrification potential. Our experiment finds that high-dose liming of acidic N-rich forest soils produces an initial pulse of soil heterotrophic respiration and increases in earthworm biomass, which together cause long-term declines in soil C and N pools.


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