Biochar restructures plant‐soil‐microbe relationships in a woody cropping system

Author(s):  
Jake A. Nash ◽  
Jessica R. Miesel ◽  
Gregory M. Bonito ◽  
Monique L. Sakalidis ◽  
Han Ren ◽  
...  
2019 ◽  
Vol 108 (1) ◽  
pp. 337-352 ◽  
Author(s):  
Pil U. Rasmussen ◽  
Alison E. Bennett ◽  
Ayco J. M. Tack

Ecohydrology ◽  
2010 ◽  
Vol 4 (6) ◽  
pp. 757-790 ◽  
Author(s):  
Chitsomanus P. Muneepeerakul ◽  
Rachata Muneepeerakul ◽  
Fernando Miralles-Wilhelm ◽  
Andrea Rinaldo ◽  
Ignacio Rodriguez-Iturbe

Author(s):  
Elisabeth Ramm ◽  
Chunyan Liu ◽  
Per Ambus ◽  
Klaus Butterbach-Bahl ◽  
Bin Hu ◽  
...  

Abstract The paradigm that permafrost-affected soils show restricted mineral nitrogen (N) cycling in favor of organic N compounds is based on the observation that net N mineralization rates in these cold climates are negligible. However, we find here that this perception is wrong. By synthesizing published data on N cycling in the plant-soil-microbe system of permafrost ecosystems we show that gross ammonification and nitrification rates in active layers were of similar magnitude and showed a similar dependence on soil organic carbon (SOC) and total nitrogen (TN) concentrations as observed in temperate and tropical systems. Moreover, high protein depolymerization rates and only marginal effects of C:N stoichiometry on gross N turnover provided little evidence for N limitation. Instead, the rather short period when soils are not frozen is the single main factor limiting N turnover. High gross rates of mineral N cycling are thus facilitated by released protection of organic matter in active layers with nitrification gaining particular importance in N-rich soils, such as organic soils without vegetation. Our finding that permafrost-affected soils show vigorous N cycling activity is confirmed by the rich functional microbial community which can be found both in active and permafrost layers. The high rates of N cycling and soil N availability are supported by biological N fixation, while atmospheric N deposition in the Arctic still is marginal except for fire-affected areas. In line with high soil mineral N production, recent plant physiological research indicates a higher importance of mineral plant N nutrition than previously thought. Our synthesis shows that mineral N production and turnover rates in active layers of permafrost-affected soils do not generally differ from those observed in temperate or tropical soils. We therefore suggest to adjust the permafrost N cycle paradigm, assigning a generally important role to mineral N cycling. This new paradigm suggests larger permafrost N climate feedbacks than assumed previously.


Author(s):  
Shamina Imran Pathan ◽  
Maria Teresa Ceccherini ◽  
Francesco Sunseri ◽  
Antonio Lupini
Keyword(s):  

2019 ◽  
Vol 11 (19) ◽  
pp. 5226 ◽  
Author(s):  
Juan Cao ◽  
Ruirui Yan ◽  
Xiaoyong Chen ◽  
Xu Wang ◽  
Qiang Yu ◽  
...  

Grazing affects nutrient cycling processes in grasslands, but little is known by researchers about effects on the nutrient stoichiometry of plant–soil–microbe systems. In this study, the influence of grazing intensity (0, 0.23, 0.34, 0.46, 0.69, and 0.92 AU ha−1) on carbon (C), nitrogen (N) and phosphorus (P) and their stoichiometric ratios in plants, soil, and microbes was investigated in a Hulunber meadow steppe, Northeastern China. The C:N and C:P ratios of shoots decreased with grazing increased. Leaf N:P ratios <10 suggested that the plant communities under grazing were N-limited. Heavy grazing intensities increased the C:N and C:P ratios of microbial biomass, but grazing intensity had no significant effects on the stoichiometry of soil nutrients. The coupling relationship of C:N ratio in plant–soil–microbial systems was tightly significant compared to C:P ratio and N:P ratio according to the correlation results. The finding suggested grazing exacerbated the competition between plants and microorganisms for N and P nutrition by the stoichiometric changes (%) in each grazing level relative to the no grazing treatment. Therefore, for the sustainability of grasslands in Inner Mongolia, N inputs need to be increased and high grazing intensities reduced in meadow steppe ecosystems, and the grazing load should be controlled within G0.46.


2017 ◽  
Vol 418 (1-2) ◽  
pp. 89-114 ◽  
Author(s):  
Judy Simon ◽  
Michael Dannenmann ◽  
Rodica Pena ◽  
Arthur Gessler ◽  
Heinz Rennenberg

2012 ◽  
Vol 3 (3) ◽  
pp. 273-277 ◽  
Author(s):  
Luca Bragazza ◽  
Julien Parisod ◽  
Alexandre Buttler ◽  
Richard D. Bardgett

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