scholarly journals Oil Residues Accelerate Coastal Wetland Losses

Eos ◽  
2016 ◽  
Author(s):  
Elizabeth Jacobsen

Coastal wetland loss after an oil spill can be more extensive than after a hurricane.

1997 ◽  
Vol 1997 (1) ◽  
pp. 789-793
Author(s):  
Eric F. Heinitz ◽  
Melany Lee

ABSTRACT The Ilwaco tire fire oil spill occurred when oil generated by the pyrolysis of rubber tire chips began seeping from a hillside into an adjacent coastal wetland. The tire chips were used as road fill material to repair a section of State Route 100 damaged by a landslide. This paper discusses not only the complexities of the response to the oil spill, but also the elaborate cofferdam system and containment berm constructed to control and contain the continual flow of oil from the site until mitigation measures could be taken to eliminate the source. Because exposure to oxygen could potentially increase the risk of a tire fire, several in-situ cooling methods were evaluated. The unique properties of this oil, the environmental effects and restoration concerns, the excavation methods, and disposal problems are all discussed. This is one of two sites in the state of Washington where a road fill, constructed of shredded tire chips, has begun burning. A comparison between these two sites, along with some assumptions as to the causes and possible preventative measures, will be briefly discussed.


Water ◽  
2019 ◽  
Vol 11 (10) ◽  
pp. 2054 ◽  
Author(s):  
Rivera-Monroy ◽  
Elliton ◽  
Narra ◽  
Meselhe ◽  
Zhao ◽  
...  

Coastal Louisiana hosts 37% of the coastal wetland area in the conterminous US, including one of the deltaic coastal regions more susceptible to the synergy of human and natural impacts causing wetland loss. As a result of the construction of flood protection infrastructure, dredging of channels across wetlands for oil/gas exploration and maritime transport activities, coastal Louisiana has lost approximately 4900 km2 of wetland area since the early 1930s. Despite the economic relevance of both wetland biomass and net primary productivity (NPP) as ecosystem services, there is a lack of vegetation simulation models to forecast the trends of those functional attributes at the landscape level as hydrological restoration projects are implemented. Here, we review the availability of peer-reviewed biomass and NPP wetland data (below and aboveground) published during the period 1976–2015 for use in the development, calibration and validation of high spatial resolution (<200 m × 200 m) vegetation process-based ecological models. We discuss and list the knowledge gaps for those species that represent vegetation community associations of ecological importance, including the long-term research issues associated to limited number of paired belowground biomass and productivity studies across hydrological basins currently undergoing different freshwater diversions management regimes and hydrological restoration priorities.


The Holocene ◽  
2020 ◽  
Vol 30 (5) ◽  
pp. 646-656
Author(s):  
Yikai Li ◽  
Yu Ye ◽  
Xiuqi Fang ◽  
Chengpeng Zhang ◽  
Zhilong Zhao

The Dongting Plain is an area characterized by wetland losses because of long-term polder construction. The study of historical polder expansion provides an opportunity to better understand the loss of wetlands covered by polders. To reconstruct the polder expansion over time, the polder patches extracted though remote sensing were marked with the names obtained from maps and the times of construction obtained from local gazetteers, and shown in the chronological order of turning points. Then, the distribution and changes in the wetlands covered by polders during 1368–1980 were reconstructed. The following are the major findings: (1) the current polders (2010s) accumulated over many centuries. There were 5.7% of the current polder area in 1644, 14.0% in 1735, 23.4% in 1850, 55.0% in 1911, 73.6% in 1949, and 100% in 1980; (2) the wetlands were mostly lost in the northern part of the region and declined rapidly over the past two centuries. The wetland area in 1850 was 6635 km2, which in 1911, 1949 and 1980 were 73.9%, 62.7% and 40.6% of that in 1850, respectively; (3) there were differences in the rate of wetland loss. The fastest time of wetland area disappearance was in 1949–1980, and 45.8 km2 of the wetlands had been lost each year; and (4) there was a spatial difference in wetland losses caused by polder expansion. In the northern part of the area, the wetland loss was mainly in 1851–1980, and the polders constructed in this period covered 89.5% of the polder area. In contrast, in the southern part of the area, the change in the wetland area was relatively small in each period, and the polder constructed before and after 1850 covered 48.3% and 52.7% of the polder area, respectively.


Author(s):  
M.D. Thompson ◽  
L.D. McGinnis ◽  
P.L. Wilkey ◽  
S.F. Miller
Keyword(s):  

2018 ◽  
Vol 213 ◽  
pp. 294-304 ◽  
Author(s):  
John W. Day ◽  
Ronald D. DeLaune ◽  
John R. White ◽  
Robert R. Lane ◽  
Rachael G. Hunter ◽  
...  

2019 ◽  
Vol 6 ◽  
Author(s):  
Rachel K. Gittman ◽  
Christopher J. Baillie ◽  
Katie K. Arkema ◽  
Richard O. Bennett ◽  
Jeff Benoit ◽  
...  
Keyword(s):  

2013 ◽  
Vol 14 (3) ◽  
pp. 1175-1188 ◽  
Author(s):  
Yangfan Li ◽  
Yalou Shi ◽  
Xiaodong Zhu ◽  
Huhua Cao ◽  
Tao Yu

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