The Hydrology of Ecological Devastation: Mountaintop RemovalValley Fill Coal Mining - PowerPoint PPT Presentation

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The Hydrology of Ecological Devastation: Mountaintop RemovalValley Fill Coal Mining

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Title: The Hydrology of Ecological Devastation: Mountaintop RemovalValley Fill Coal Mining


1
The Hydrology of Ecological Devastation
Mountaintop Removal/Valley Fill Coal Mining
2
Background
  • MTR/VF Coal mining flattened over 1 million acres
  • Buried thousands of miles of streams
  • Altered hydrology blamed for destructive and
    deadly flooding
  • Acid mine drainage, sedimentation, etc. causing
    reduction in habitat

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7
Peak Flow Study
  • Wiley and Brogan
  • USGS

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9
Determination of Peak Flow
  • Observed high water marks from July, 2001 flood
  • Estimated Mannings coefficient
  • Calculated peak flow (previous studies avg. 6.7
    error using this method)
  • Calculated flow sensitivity to 10 increase or
    decrease in Mannings coefficient
  • Estimates of flood-recurrence intervals based on
    published flood-frequency equations (Wiley, 2000)
  • Valley-fill site intervals calculated as though
    they were typical streams

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Reasons for Runoff Variability
  • Lesser slope on top of VF causes increased travel
    time
  • Reduced permeability of VF surface decreases
    travel time and increases runoff volume
  • Deforestation results in increase of runoff volume

14
Issues
  • If precipitation across study area were equal,
    than flood-recurrence intervals of unfilled sites
    should be equal Really?
  • How does accuracy of interpretation of high water
    marks affect peak flow estimation
  • Wide range of flood-recurrence intervals for
    valley fill sites mysterious synthetic
    hydrology

15
The Anatomy of a VF
16
Impacts of VF on Headwater Floods in Eastern KY
  • J.D. Phillips
  • UK

17
Relative Runoff and Flow Detention Models
  • Model compared VF hydrology to reference
    condition (unmined forested hillslopes with
    typical Eastern KY soils)
  • Simply alter variables for new condition
  • Output is ratio of situation in question to
    reference situation

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Increasing Surface Runoff
  • Reduce average flow length, L
  • Reduce runoff abstraction, K (infiltration
    excess)
  • Reduce available water capacity, C (saturation
    excess)
  • Increasing slope, S
  • Reducing surface roughness, N

20
More Ratios
  • Infiltration Excess
  • Saturation Excess
  • Runoff from CN

21
Ratios of Variables
  • Minimum is preferred

22
Runoff
23
Runoff Results
  • Tend to indicate that flash flooding would be
    more prevalent downstream of VFs due to
    infiltration excess runoff
  • In general, results suggest that runoff response
    is likely to be increased for VF sites
  • Agree with previous studies that VF streams will
    maintain higher low-flows than unaffected streams
    ecological implications?

24
Precipitation Variability
  • Mine companies claim variable precipitation over
    flooded area
  • Analyzed two floods using radar precipitation
    images
  • Images indicate storm precip totals 2 km pixels
  • Placed random transects over study area (Eastern
    KY)

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Precipitation Contd
  • SPF used to determine spatial dependence in storm
    precipitation patterns
  • SPF indicates probability that different precip
    class will be h pixels apart
  • Essentially SPFltSPF random indicates clustering
    of precip values

27
Precipitation Contd
  • Results indicate that spatial dependence of
    precip for two storms is high

28
The Connection
29
To what extent does the hydrology of a VF effect
ecology?
  • Sponge effect
  • Sustained baseflows during drought and increased
    baseflows year-round

30
Ecological Effect Contd
31
Benthic macroinvertebrate assemblages in streams
with varying flow permanenceJ.W.
FeminellaAuburn U.
32
Findings
  • 75 of species displayed no pattern with respect
    to stream permanence
  • 7 of species found exclusively within
    intermittent streams
  • However, other results indicate that assemblages
    show predictable, but subtle, relationships with
    stream permanence
  • Year to year riffle permanence influence the
    structure of assemblages

33
How much do VF influence stream habitat?
  • Hartman, et al.
  • WVU

34
Findings
  • No evidence for increased sedimentation
    downstream
  • Increases stream conductivity
  • Increases metals in streams (Na, K, Mn, Mg, Ca,
    Ni, and Fe)
  • Significantly lower populations of 6 varieties of
    stream biota
  • However, given the level of disturbance in
    valley fills, it is surprising how little
    differences existed between fills and reference
    stream biota

35
Issues
  • Deep pit mining had occurred in all of watersheds
    that Hartman studied. Reference streams?
  • How does new temperature regime affect stream
    habitat?
  • Fish?
  • Worth studying hydrology of VFs? Too random?
  • Turn off the lights?
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