Kingsdale Beck - Geog 2

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  • Kingsdale Beck
    • Method of Presentation
      • Log normal box and whisker plot
        • Site 3.1
          • Range of 16-39,466 cm3
          • Interquartile - 1409.5
        • Site 3.3
          • Range of 0- 5596 cm3
          • Interquartile - 1094 cm3
        • Advantages
          • Able to display a large range of data, avoiding clusters due to data being over 4 orders of magnitude
        • Hypothesis: There is no significance difference between the volumes of bedload in two 3rd order streams
          • Mann-Whitney:120
          • critical value:127
            • Untitled
    • Theory
      • Hjulstrom
        • As the velocity increases it will take away everything smaller than the pick up velocity meaning only larger rocks will remain
        • Smaller bed load particles further downstream will be most likely eroded as the velocity will be a lot higher then upstream
      • Bradshaw
        • where the triangle is wider it is where the characteristic is of a larger quantity or size
        • The particle size links into the velocity and how this increases as you go further downstream
          • Therefore the higher the velocity the more erosion will take place, meaning the bedload will get smaller, as is also suggested
        • Channel bed roughness should also decrease as you go downstream, and therefore also refers to the roundness of the rocks in the channel
          • expected there to be anomalies as we hadn't ensured we differentiated between different rock types and therefore erosional abilities
      • Strahler's stream order
        • Difference between the channel characteristic upstream and further downstream
        • Due to different amount of water that will have come from other channels
    • Risk Assessment
      • Kingsdale Beck
        • High risk
          • Face upstream, work together, work downstream, no deeper than wellies
      • Adders
        • Lower risk
          • Brief to avoid, no sandles
      • Steep slopes
        • On site brief
          • Ensure to take care when walking down slopes and also to make sure rest of group is able to move down
      • Road crossing
        • park on left hand side where possible so that door doesn't open onto road, green cross code
    • Location
      • Yorkshire Dales National Park
      • Source end of River Twiss, meeting the River Doe further downstream to form River Greta in Ingleton
        • Several 1st order streams at the top of the valley near our first site
          • land around here is peaty
        • 5th order stream near the end of the periglacial lake
          • valley sides and valley bottom of the rest of the basin is limestone
            • Yoredale series
              • Alternating layers of gritstone and limestone and some softer layers of shale and coal
      • Temperate West-coast maritime climate
        • On average 200mm of rainfall per year
      • 500m gradient either side of channel with a relatively flat narrow bottom which widens further downstream
    • Sampling Technique
      • Stratified
        • chose whereabouts our sites were going to be to ensure we had different stream orders
      • Systematic sampling
        • sites were equally spaced apart (50m in between each site at each order) in order to ensure show an environmental gradient in each order
          • important as hypothesis was changes downstream
          • 12 sites in order to allow enough levels of significance in spearmans rank
      • 1. Used a 50m tape measure as a transect from one bank to the other
        • 2. Then a random number table to find a measurement along the transect eg. 56.2 = 5.62m
        • 3. repeated this 20 times at each site, then lined them up in size order making it easier
          • Meant we took an unbiased sample, reduced chance we would always take out small rocks
    • Primary data collection
      • Stone roundness
        • Power's scale of roundness index table
          • scale ranges from 1(very angular) to 6(well rounded)
            • minimum of 5 categories to get different categories for chi-squared
      • moderated
        • making sure the same person decided the roundness as it is subjective
        • 10 sites in order to get levels of significance
    • Conclusion
      • Kingsdale Beck isn't a typical river
        • shouldn't be a difference between two 3rd order streams and should be a difference downstream but there isn't
          • therefore even the bedload doesn't represent a typical river
        • couldn't collect velocity and therefore discharge as well
          • impellor wasn't working effectively
          • only measured bedload rather than flow characteristic
            • only one part of Hjulstrom and Bradshaw measured

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