LIVESTOCK EXCLUSION AND BELOWGROUND ECOSYSTEM RESPONSES IN RIPARIAN MEADOWS OF EASTERN OREGON

2004 ◽  
Vol 14 (6) ◽  
pp. 1671-1679 ◽  
Author(s):  
J. Boone Kauffman ◽  
Andrea S. Thorpe ◽  
E. N. Jack Brookshire
2021 ◽  
Author(s):  
Florian Schneider ◽  
Christopher Poeplau ◽  
Axel Don

2020 ◽  
Vol 30 (12) ◽  
pp. 2284-2297
Author(s):  
Tatenda Dalu ◽  
Terence A. Bellingan ◽  
Jeanne Gouws ◽  
N. Dean Impson ◽  
Martine S. Jordaan ◽  
...  

2009 ◽  
Vol 15 (7) ◽  
pp. 1652-1663 ◽  
Author(s):  
U. KOKFELT ◽  
P. ROSÉN ◽  
K. SCHONING ◽  
T. R. CHRISTENSEN ◽  
J. FÖRSTER ◽  
...  

2013 ◽  
Vol 120 (1-2) ◽  
pp. 477-489 ◽  
Author(s):  
Hae-Kyung Park ◽  
Kang-Hyun Cho ◽  
Doo Hee Won ◽  
Jangho Lee ◽  
Dong-Soo Kong ◽  
...  

2008 ◽  
Vol 6 (5) ◽  
pp. 264-272 ◽  
Author(s):  
Nancy B Grimm ◽  
David Foster ◽  
Peter Groffman ◽  
J Morgan Grove ◽  
Charles S Hopkinson ◽  
...  
Keyword(s):  

2015 ◽  
Vol 12 (9) ◽  
pp. 2791-2808 ◽  
Author(s):  
J. Tang ◽  
P. A. Miller ◽  
A. Persson ◽  
D. Olefeldt ◽  
P. Pilesjö ◽  
...  

Abstract. A large amount of organic carbon is stored in high-latitude soils. A substantial proportion of this carbon stock is vulnerable and may decompose rapidly due to temperature increases that are already greater than the global average. It is therefore crucial to quantify and understand carbon exchange between the atmosphere and subarctic/arctic ecosystems. In this paper, we combine an Arctic-enabled version of the process-based dynamic ecosystem model, LPJ-GUESS (version LPJG-WHyMe-TFM) with comprehensive observations of terrestrial and aquatic carbon fluxes to simulate long-term carbon exchange in a subarctic catchment at 50 m resolution. Integrating the observed carbon fluxes from aquatic systems with the modeled terrestrial carbon fluxes across the whole catchment, we estimate that the area is a carbon sink at present and will become an even stronger carbon sink by 2080, which is mainly a result of a projected densification of birch forest and its encroachment into tundra heath. However, the magnitudes of the modeled sinks are very dependent on future atmospheric CO2 concentrations. Furthermore, comparisons of global warming potentials between two simulations with and without CO2 increase since 1960 reveal that the increased methane emission from the peatland could double the warming effects of the whole catchment by 2080 in the absence of CO2 fertilization of the vegetation. This is the first process-based model study of the temporal evolution of a catchment-level carbon budget at high spatial resolution, including both terrestrial and aquatic carbon. Though this study also highlights some limitations in modeling subarctic ecosystem responses to climate change, such as aquatic system flux dynamics, nutrient limitation, herbivory and other disturbances, and peatland expansion, our study provides one process-based approach to resolve the complexity of carbon cycling in subarctic ecosystems while simultaneously pointing out the key model developments for capturing complex subarctic processes.


1987 ◽  
Vol 67 (4) ◽  
pp. 747-763 ◽  
Author(s):  
M. A. NAETH ◽  
A. W. BAILEY ◽  
W. B. McGILL

A study was conducted in Solonetzic mixed prairie of southern Alberta to evaluate and determine the longevity of selected ecosystem responses to pipeline installation. Five adjacent natural gas pipelines on a series of rights-of-way (ROW) were studied at three sites. The lines, which were installed in 1957, 1963, 1968, 1972 and 1981, had diameters of 86, 86, 91, 107 and 107 cm, respectively. Soils were analyzed for particle size distribution, bulk density, pH, electrical conductivity, ion composition, and organic matter content. It was concluded that pipeline construction in Solonetzic mixed prairie range-land initially tended to improve surface soil chemical and physical properties compared to blowouts, but reduced soil quality in vegetated native prairie. Surface bulk density increased to 1.3–1.6 Mg m−3 from an undisturbed density of 0.9–1.0 Mg m−3. Increased densities were evident to 55 cm in all 1981 transects except the trench where subsurface densities were reduced. Chemical changes were associated with reduced organic matter and increased salts at the surface. On the basis of differences between the various ages of pipelines (1981, youngest; 1957, oldest) there was evidence for greater amelioration of chemical changes than of physical disturbances over time. The time needed to restore half the lost organic matter was estimated to be approximately 50 y. Key words: Pipeline, Solonetzic soil, rangeland (native), soil chemistry, bulk density, reclamation


Ecosystems ◽  
2011 ◽  
Vol 14 (8) ◽  
pp. 1217-1231 ◽  
Author(s):  
Jay B. Norton ◽  
Laura J. Jungst ◽  
Urszula Norton ◽  
Hayley R. Olsen ◽  
Kenneth W. Tate ◽  
...  

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