Dissolved Solids, Sediments, & Turbidity

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28 Terms

1
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What is TDS?


total concentration of dissolved substances in water

  • Inorganic salts: sodium, potassium, calcium, magnesium, chlorides, sulfates, silicates, bicarbonates

  • Small amounts of organic matter from natural sources

the "invisible" dissolved content

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What TDS measures?

All dissolved ions and molecules

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What does TDS not include?

suspended particles, bacteria, or anything that can be filtered out

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TDS in freshwater? For drinking water?

20-1000 mg/L

50 mg/L for taste, 500 mg/L EPA recommended

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is TDS unhealthy?

No

indirect indicator of contamination

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How to measure TDS?

Directly: Evaporate a water sample, weigh
the remaining residue

Indirectly: Specific conductance (SpC) is a
proxy for TDS in freshwaters

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Controls on TDS

  • Soil type

  • Geology/weathering

    • Ex. Limestone is relatively easy to mineralize

  • pH/temperature/DO

  • Discharge & Residence time

  • Evaporation

  • Decomposition & DOM

  • Human Activities

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Wentworth Scale

defines grain size class in intervals that
increase by powers of 2

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How does particle size change from upstream to downstream?

Particle size tends to decrease
moving downstream

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Median size (d50)

half of the bed particles are large, half are smaller

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Embeddedness

degree to which particles are buried

<p><span>degree to which particles are buried</span></p>
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Sorting

distribution of particles in the bed
• Well-sorted = discrete patches of the same size
• Poorly sorted = mixed particle sizes

<p><span style="font-size: calc(var(--scale-factor)*24.00px);">distribution of particles in the bed</span><span><br></span><span style="font-size: calc(var(--scale-factor)*24.00px);">• Well-sorted = discrete patches of the same size</span><span><br></span><span style="font-size: calc(var(--scale-factor)*24.00px);">• Poorly sorted = mixed particle sizes</span></p>
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Armoring


finer sediments overlain by larger particles

• Occurs when the bed surface of gravel-bed rivers is coarsened relative to the subsurface
• Dams can exacerbate this process

<p><span style="font-size: calc(var(--scale-factor)*24.00px);"><br>finer sediments overlain by larger particles</span><span><br></span><span style="font-size: calc(var(--scale-factor)*24.02px);">• Occurs when the bed surface of </span><span style="font-size: calc(var(--scale-factor)*24.00px);">gravel-bed rivers is coarsened relative to the subsurface</span><span><br></span><span style="font-size: calc(var(--scale-factor)*24.00px);">• Dams can exacerbate this process</span></p>
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How do sediments move in streams?

Stream load – transport of matter other than water by streamflow

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Dissolved load

mostly dissolved chemicals (TDS!), including
nutrients

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Particulate load

non-dissolved components

Suspended (solid) load, wash load, bed load

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Suspended (solid) load


material in the water column (<0.5 μm)

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wash load

between 0.5 μm and 0.063 mm (largely sand and silt); think about the puff of sand when you step in a stream

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bed load


material that rolls along the bottom (>0.063 mm)

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shear stress

The amount of tractive force (“drag”) applied parallel to a surface
Will determine if a particle enters the stream load

highest in the “thalweg” (mainthread of flow)

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Critical shear stress (τc)

shear stress necessary to mobilize
a given grain size

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Shear increases

with both slope and depth

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main driver of sediment transport?

storms

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Entrainment (erosion)

getting the sediments moving

sand is most easily entrained

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sediment transport (movement)

movement down the channel;
requires a lower velocity

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Deposition (sedimentation)

settling out; as velocities decrease, grains settle out
Heaviest/largest sediments fall out first

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Channel Modifications

erosion

accretion

sediment routing

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Measuring sediments

  • Total suspended solids (TSS) – filtering a water sample until filter clogs

  • Direct turbidity measurement - beam of light is passed through a water sample; measure amount of light scattered (units = NTU)

    • ↑ scattered light with ↑ turbidity

  • Secchi Disk – common in lakes