Response of microbial functional groups involved in soil N cycle to N, P and NP fertilization in Tibetan alpine meadows

2016 ◽  
Vol 101 ◽  
pp. 195-206 ◽  
Author(s):  
Wenbin Ma ◽  
Shengjing Jiang ◽  
Féline Assemien ◽  
Mingsen Qin ◽  
Beibei Ma ◽  
...  
2005 ◽  
Vol 75 (1) ◽  
pp. 65-80 ◽  
Author(s):  
A. K. Patra ◽  
L. Abbadie ◽  
A. Clays-Josserand ◽  
V. Degrange ◽  
S. J. Grayston ◽  
...  

SOIL ◽  
2015 ◽  
Vol 1 (1) ◽  
pp. 235-256 ◽  
Author(s):  
J. W. van Groenigen ◽  
D. Huygens ◽  
P. Boeckx ◽  
Th. W. Kuyper ◽  
I. M. Lubbers ◽  
...  

Abstract. The study of soil N cycling processes has been, is, and will be at the centre of attention in soil science research. The importance of N as a nutrient for all biota; the ever-increasing rates of its anthropogenic input in terrestrial (agro)ecosystems; its resultant losses to the environment; and the complexity of the biological, physical, and chemical factors that regulate N cycling processes all contribute to the necessity of further understanding, measuring, and altering the soil N cycle. Here, we review important insights with respect to the soil N cycle that have been made over the last decade, and present a personal view on the key challenges of future research. We identify three key challenges with respect to basic N cycling processes producing gaseous emissions: 1. quantifying the importance of nitrifier denitrification and its main controlling factors; 2. characterizing the greenhouse gas mitigation potential and microbiological basis for N2O consumption; 3. characterizing hotspots and hot moments of denitrification Furthermore, we identified a key challenge with respect to modelling: 1. disentangling gross N transformation rates using advanced 15N / 18O tracing models Finally, we propose four key challenges related to how ecological interactions control N cycling processes: 1. linking functional diversity of soil fauna to N cycling processes beyond mineralization; 2. determining the functional relationship between root traits and soil N cycling; 3. characterizing the control that different types of mycorrhizal symbioses exert on N cycling; 4. quantifying the contribution of non-symbiotic pathways to total N fixation fluxes in natural systems We postulate that addressing these challenges will constitute a comprehensive research agenda with respect to the N cycle for the next decade. Such an agenda would help us to meet future challenges on food and energy security, biodiversity conservation, water and air quality, and climate stability.


2013 ◽  
Vol 8 (4) ◽  
pp. 29 ◽  
Author(s):  
Nunzio Fiorentino ◽  
Massimo Fagnano ◽  
Paola Adamo ◽  
Adriana Impagliazzo ◽  
Mauro Mori ◽  
...  

2021 ◽  
Vol 278 ◽  
pp. 116852
Author(s):  
Xin Zhang ◽  
Guangmin Xiao ◽  
Roland Bol ◽  
Ligang Wang ◽  
Yuping Zhuge ◽  
...  

2014 ◽  
Vol 1 (1) ◽  
pp. 623-676 ◽  
Author(s):  
J. W. van Groenigen ◽  
D. Huygens ◽  
P. Boeckx ◽  
T. W. Kuyper ◽  
I. M. Lubbers ◽  
...  

Abstract. The study of soil N cycling processes has been, is, and will be at the center of attention in soil science research. The importance of N as a nutrient for all biota; the ever increasing rates of its anthropogenic input in terrestrial (agro)ecosystems; its resultant losses to the environment; and the complexity of the biological, physical, and chemical factors that regulate N cycling processes all contribute to the necessity of further understanding, measurement and mitigation of the soil N cycle. Here, we review important insights with respect to the soil N cycle that have been made over the last decade, and present a personal view on the key challenges for future research (Fig. 1). We identified four key questions with respect to N cycling processes: 1. How large is the contribution of non-symbiotic N fixation in natural systems? 2. How important is nitrifier denitrification and what are its main controlling factors? 3. What is the greenhouse gas mitigation potential and microbiological basis for N2O consumption? 4. How can we characterize hot-spots and hot-moments of denitrification? Furthermore, we propose three questions about proximal controls on N cycling processes: 1. How does functional diversity of soil fauna affect N cycling beyond mineralization? 2. What is the functional relationship between root traits and soil N cycling? 3. To what extent do different types of mycorrhizal symbioses (differentially) affect N cycling? Finally, we identified a key challenge with respect to modelling: 1. How can advanced 15N/18O tracing models help us to better disentangle gross N transformation rates? We postulate that addressing these questions would constitute a comprehensive research agenda with respect to the N cycle for the next decade. Such an agenda would help us to meet future challenges on food and energy security, biodiversity conservation and climate stability.


Ecosphere ◽  
2018 ◽  
Vol 9 (9) ◽  
pp. e02426 ◽  
Author(s):  
Clément Bardon ◽  
Boris Misery ◽  
Florence Piola ◽  
Franck Poly ◽  
Xavier Le Roux
Keyword(s):  
Soil N ◽  
N Cycle ◽  

2018 ◽  
Vol 426 (1-2) ◽  
pp. 211-225 ◽  
Author(s):  
Qi Liu ◽  
Yanhui Zhang ◽  
Benjuan Liu ◽  
James E. Amonette ◽  
Zhibin Lin ◽  
...  
Keyword(s):  
Soil N ◽  
N Cycle ◽  

2016 ◽  
Vol 95 ◽  
pp. 223-232 ◽  
Author(s):  
R. Liz Hamilton ◽  
Mark Trimmer ◽  
Chris Bradley ◽  
Gilles Pinay
Keyword(s):  
Oil Palm ◽  
Soil N ◽  
N Cycle ◽  

2018 ◽  
Vol 10 (12) ◽  
pp. 4805 ◽  
Author(s):  
Qi-Peng Zhang ◽  
Jian Wang ◽  
Hong-Liang Gu ◽  
Zhi-Gang Zhang ◽  
Qian Wang

Many studies reported the effect on plant functional groups and plant diversity under discontinuous slope gradient. However, studies on the effect of continuous slope gradient on plant functional groups and plant diversity in alpine meadows have rarely been conducted. We studied the effect of a continuous slope gradient on the dominance characteristics of plant functional groups and plant diversity of alpine meadows on the Tibetan plateau—in Hezuo area of Gannan Tibetan Autonomous Prefecture. Altogether, 84 samples of alpine meadows grass and 84 soil samples from seven slope gradients at sunlit slopes were collected. By using analysis of variance (ANOVA) and Pearson correlation coefficient, this study revealed: (1) Continuous slope gradient is an important factor affecting plant communities in alpine meadows, due to the physical and chemical characteristics of the soil and water content. The number of families, genera, and species increased first then decreased at the different slope gradient levels, respectively; (2) there is a close relationship between the soil and plant functional groups, and plant diversity. In other words, the slope determines the functional groups of plants and the soil nutrients; and (3) soil characteristics (pH value, Soil Total Nitrogen, Soil Water Content) are the determining factors of the plant community characteristics at each slope gradient level. To conclude, a continuous slope gradient is an important factor that affects plant communities in alpine meadows.


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