نتایج جستجو برای: soil c dynamics

تعداد نتایج: 1626374  

2015
Francisco J. Calderón Joseph Benjamin Merle F. Vigil

In order to properly determine the value of charring crop residues, the C use efficiency and effects on crop performance of biochar needs to be compared to the un-charred crop residues. In this study we compared the addition of corn stalks to soil, with equivalent additions of charred (300 °C and 500 °C) corn residues. Two experiments were conducted: a long term laboratory mineralization, and a...

2016
Charles Pepe-Ranney Ashley N. Campbell Chantal N. Koechli Sean Berthrong Daniel H. Buckley

We explored microbial contributions to decomposition using a sophisticated approach to DNA Stable Isotope Probing (SIP). Our experiment evaluated the dynamics and ecological characteristics of functionally defined microbial groups that metabolize labile and structural C in soils. We added to soil a complex amendment representing plant derived organic matter substituted with either (13)C-xylose ...

Journal: :Environmental science & technology 2010
Eva-Maria Burkhardt Denise M Akob Sebastian Bischoff Jana Sitte Joel E Kostka Dipanjan Banerjee Andreas C Scheinost Kirsten Küsel

Understanding the dynamics of metals and radionuclides in soil environments is necessary for evaluating risks to pristine sites. An iron-rich creek soil of a former uranium-mining district (Ronneburg, Germany) showed high porewater concentrations of heavy metals and radionuclides. Thus, this study aims to (i) evaluate metal dynamics during terminal electron accepting processes (TEAPs) and (ii) ...

2006
T. C. Kaspar T. B. Parkin

Winter cover crops have the potential to increase soil organic C in the corn (Zea mays L.)–soybean [Glycine max (L.) Merr.] rotation in the upper Midwest. Management effects on soil C, however, are often difficult to measure because of the spatial variation of soil C across the landscape. The objective of this study was to determine the effect of oat (Avena sativa L.), rye (Secale cereale L.), ...

2009
Xiaojuan Yang Victoria Wittig Atul K. Jain Wilfred Post

[1] A comprehensive model of terrestrial N dynamics has been developed and coupled with the geographically explicit terrestrial C cycle component of the Integrated Science Assessment Model (ISAM). The coupled C-N cycle model represents all the major processes in the N cycle and all major interactions between C and N that affect plant productivity and soil and litter decomposition. Observations ...

2015
C. D. Koven E. A. G. Schuur C. Schädel T. J. Bohn E. J. Burke G. Chen X. Chen P. Ciais G. Grosse J. W. Harden D. J. Hayes G. Hugelius E. E. Jafarov G. Krinner P. Kuhry D. M. Lawrence A. H. MacDougall S. S. Marchenko A. D. McGuire S. M. Natali D. J. Nicolsky D. Olefeldt S. Peng V. E. Romanovsky K. M. Schaefer J. Strauss C. C. Treat M. Turetsky

We present an approach to estimate the feedback from large-scale thawing of permafrost soils using a simplified, data-constrained model that combines three elements: soil carbon (C) maps and profiles to identify the distribution and type of C in permafrost soils; incubation experiments to quantify the rates of C lost after thaw; and models of soil thermal dynamics in response to climate warming...

2016
Arezoo Taghizadeh-Toosi Bent T. Christensen Margaret Glendining Jørgen E. Olesen

World soil carbon (C) stocks are third only to those in the ocean and earth crust, and represent twice the amount currently present in the atmosphere. Therefore, any small change in the amount of soil organic C (SOC) may affect carbon dioxide (CO2) concentrations in the atmosphere. Dynamic models of SOC help reveal the interaction among soil carbon systems, climate and land management, and they...

2002
D. Solomon F. Fritzsche J. Lehmann W. Zech

requires analytical methods that can (i) accurately monitor changes in the amount, nature, and dynamics of We used natural 13C abundance coupled with particle-size fractionSOM pools in natural and human-influenced systems ation to evaluate soil organic carbon (SOC) dynamics following deforand (ii) estimate C fluxes between the soils and atmoestation and subsequent cultivation in the subhumid Et...

2017
Wentao Luo Mai-He Li Jordi Sardans Xiao-Tao Lü Chao Wang Josep Peñuelas Zhengwen Wang Xing-Guo Han Yong Jiang

Plant carbon (C) and nitrogen (N) stoichiometry play an important role in the maintenance of ecosystem structure and function. To decipher the influence of changing environment on plant C and N stoichiometry at the subcontinental scale, we studied the shoot and root C and N stoichiometry in two widely distributed and dominant genera along a 2,200-km climatic gradient in China's grasslands. Rela...

2015
Wei Zhang Chao Liang Jenny Kao-Kniffin Hongbo He Hongtu Xie Hong Zhang Xudong Zhang

Newly synthesized amino acids are the principle compounds created after inorganic nitrogen (N) is rapidly immobilized into microbial tissues. However, little is known about the mineralization kinetics of these newly synthesized amino acids compared to the amino acids originally present in the soil, and how substrate availability controls their mineralization. With 15N isotope tracing, the newly...

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