Rangeland application of biochar and rotational grazing interact to influence soil and plant nutrient dynamics

Geoderma ◽  
2022 ◽  
Vol 408 ◽  
pp. 115572
Author(s):  
Si Gao ◽  
Thomas H. DeLuca
2020 ◽  
Vol 16 (1) ◽  
pp. 20190441 ◽  
Author(s):  
Michael B. Bonsall ◽  
Cynthia A. Froyd ◽  
Elizabeth S. Jeffers

Ecosystem dynamics are driven by both biotic and abiotic processes, and perturbations can push ecosystems into novel dynamical regimes. Plant–plant, plant–soil and mycorrhizal associations all affect plant ecosystem dynamics; however, the direction and magnitude of these effects vary by context and their contribution to ecosystem resilience over long time periods remains unknown. Here, using a mathematical framework, we investigate the effects of plant feedbacks and mycorrhiza on plant–nutrient interactions. We show evidence for strong nutrient controlled feedbacks, moderation by mycorrhiza and influence on ecological resilience. We use this model to investigate the resilience of a longitudinal palaeoecological birch– δ 15 N interaction to plant–soil feedbacks and mycorrhizal associations. The birch– δ 15 N system demonstrated high levels of resilience. Mycorrhiza were predicted to increase resilience by supporting plant–nitrogen uptake and immobilizing excess nitrogen; in contrast, long-term enrichment in available nitrogen by plant–soil feedbacks is expected to decrease ecological resilience.


1982 ◽  
Vol 60 (8) ◽  
pp. 1561-1568 ◽  
Author(s):  
Håkan Staaf ◽  
Björn Berg

Plant nutrient dynamics in decomposing needle litter were measured during a 5-year period in a Scots pine forest in central Sweden. As seen over the whole 5-year period, the nutrients were retained (to a litter weight loss of about 75%) in the order Mn < Ca < K < Mg < S < N < P. During the first 1.5 years there was a net increase of N and P whereafter a net release took place. A similar but less pronounced development could be seen for S, whereas Ca, K, Mn, and Mg were released from the start of the incubation. It is suggested that P was the most limiting element for microbial activity during this first phase. There appeared to be only little initial leaching from the litter and the different behaviours of the elements could largely be explained by their concentration in litter in relation to the needs of microorganisms and to their solubility. K and Mg were the elements that were released at rates most similar to organic matter weight loss.


2019 ◽  
Vol 514-515 ◽  
pp. 87-94 ◽  
Author(s):  
E.M. van Egmond ◽  
P.M. van Bodegom ◽  
J.R. van Hal ◽  
R.S.P. van Logtestijn ◽  
R.A. Broekman ◽  
...  

2012 ◽  
Vol 15 (2) ◽  
pp. 355-370 ◽  
Author(s):  
Marian M. Chau ◽  
Lawrence R. Walker ◽  
Klaus Mehltreter

2013 ◽  
Vol 105 (2) ◽  
pp. 527-538 ◽  
Author(s):  
K. Djaman ◽  
S. Irmak ◽  
D. L. Martin ◽  
R. B. Ferguson ◽  
M. L. Bernards

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