Sediment dynamics in most large river basins are influenced by a variety of different natural and anthropogenic pressures, and disentangling these cumulative effects remains a challenge. This study determined the contemporary and historical sources of fine-grained (<?63-μm) sediment in a large, regulated river basin and linked changes in sources to activities in the basin. The river has seen declines in chinook salmon, sockeye salmon, and the endangered Nechako white sturgeon populations, and sediment (both fine-grained and sands) transport and deposition have been identified as potential causes of these declines.
Materials and methods
Samples of suspended sediment and potential source materials were collected from numerous sites distributed throughout the upper Nechako River Basin in British Columbia, Canada. A floodplain sediment core was also collected in order to reconstruct sediment sources over the last ~?70 years. Discriminating fingerprint properties were used within the MixSIAR model to apportion sources among sub-basins and land-use types. Results were compared to records of precipitation and Nechako River discharge trends, and to changes in landscape development.
Results and discussion
Contributions from the erosion of channel banks dominated the suspended sediment load at most sites. Changes in sediment sources during the 2015 field season reflected snowmelt and patterns of water release from the Nechako Reservoir that affected the sediment-carrying capacity of tributaries and the Nechako River main stem. Spatial variations in 2015 also reflected the distribution of land use (e.g., forested or agricultural land) as well as topography (e.g., slope steepness). Over the last ~?70 years, variations in sediment sources and the characteristics of the sediment (e.g., organic matter content and particle size composition) were linked to the construction of the Kenney Dam (operational in 1954) and the impacts of deforestation by the forestry and agricultural industries. Superimposed on these have been wildfires and a major mountain pine beetle infestation leading to higher erosion rates in the affected areas.
Conclusions
The sediment source fingerprinting technique, in combination with historical information on the hydrometeorology and the land use and river management in the basin, has provided valuable information with which to understand sediment dynamics in the Nechako River Basin. Such an approach can help to disentangle how large river systems respond to a combination of natural and anthropogenic pressures.
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Analytical studies of flow from irrigation sources into regions of root water uptake typically require the root distribution and the local water extraction rate as data of the problem. In reality, these are strongly influenced by local soil water content and, hence, position relative to the source. This work introduces a model with moisture-dependent root water extraction rate, so that the spatial distribution of uptake is no longer a datum, but emerges as part of the solution. For a diversity of conditions we obtain simple steady solutions describing the interactions between continuous sources and regions of wetting and water extraction. It is shown that as the uptake rate increases, the region decreases markedly in size and becomes more symmetrical in the vertical; for sources at depths that are small relative to the sorptive length, interaction with the surface becomes important; surface evaporation losses significantly reduce the region and increase asymmetry; with non-evaporating surfaces, the region is larger and more symmetrical. The dimensionless coefficient β, proportional to the ratio of the local extraction rate to the Kirchhoff potential, determines behaviour. Estimating β under controlled and field conditions is discussed. 相似文献
Paranasal meningioma was diagnosed in a 5-year-old Appaloosa gelding. The mass occupied the right maxillary, frontal, and sphenopalatine sinuses but did not invade the calvarium. The diagnosis was based on histologic evaluation, positive immunohistochemical staining for vimentin and cytokeratin, and ultrastructural features including the presence of interdigitating spindle cells with numerous desmosomes. 相似文献
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