Groundwater, its treatment and protection Harri Mattila, 2019 1 - - PowerPoint PPT Presentation

groundwater its treatment and protection
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Groundwater, its treatment and protection Harri Mattila, 2019 1 - - PowerPoint PPT Presentation

Groundwater, its treatment and protection Harri Mattila, 2019 1 7.10.2019 General l Groundwater forms only 0,53 % of all water resources (worldwide). l In Finland, more than 2/3 of all raw water is groundwater or artificial groundwater l


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7.10.2019 1

Groundwater, its treatment and protection

Harri Mattila, 2019

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General

l Groundwater forms only 0,53 % of all water

resources (worldwide).

l In Finland, more than 2/3 of all raw water is

groundwater or artificial groundwater

l Advantages of groundwater when compared

to surface water:

  • No need for disinfection (in normal situations)
  • Temperature is rather constant (and low)
  • Little or no chemicals involved in treatment
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The hydrological cycle

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Various groundwater formations

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Observation tube (well)

l Usually PVC pipe l DN > 50 mm l Screen in the depth

  • f the groundwater

layer

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An example of groundwater depth variations (Tuusula, Finland)

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The need for groundwater treatment

l optimum situation: no treatment l most common reason is prevention of corrosion l Fe or Mn l organic material l fluoride l salts l radon l arsenic

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pH -value

l Depends on soil around the

groundwater well

l Sometimes rain water can be acidic l pH of groundwater in Finland is

normally between 5 - 7

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Nitrate compounds

l ammonium, nitrate, nitrite, nitrogen l Very rarely in Finnish groundwaters l Usually means pollution by agriculture

  • r industry

l Sometimes also because of wastewater in

groundwater!

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Sulfate

l Can be diluted in groundwater for

example from minerals rich of sulphur beacause of high pH.

l Important factor in corrosion l limit 50 mg/l

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Iron and manganese

l Most common problems in groundwater

(in Finland)

l No health hazard – technical and/or

aesthetical problems

l Fe < 0,2 mg/, Mn < 0,05 mg/l l Causing also sedimentation in networks

and that’s why harmful

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Chloride

l Normally because of nearby sea but also

because of deicing in winter

l In nature < 10 mg/l, taste limit 200 – 300

mg/l, recommended maximum 250 mg/l, target 25 mg/l

l Very important factor in corrosion

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Hardnes

l Ca- ja Mg –salts l 1 mmol/l = 5,6 º dH l Should be 3 – 5 º dH l The most interesting parameter to

customers due to washing machines

l sometimes high also in Finland, even >10

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Aluminium

l Can be diluted from from the soil (like

Fe and Mn), specially when the soil in acidic

l The maximum limit allowed 0,2 mg/l

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Arsenic

l carcinogenic, max allowed 0,01 mg/l l Mainly in deep boreholes l In Finland about 7% of all the deep

wells are contaminated

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Boron

l Max allowed 1,0 mg/l l Is indicating pollution by wastewater l Appears very seldom

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Fluoride

l WHO: max allowed 1,5 mg/l (note,

drinking water should have 0,5 mg/l)

l Defluoridation is considered as an

expensive task => 1. change the source if possible, 2. dilute water with another

  • ne with little flouride, 3. treatment
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Copper

l Max allowed 2,0 mg/l ( an average /

week)

l Rather seldom in groundwater l Mainly because of corrosion in pipelines

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Bacteria

l E.coli is the most important indicator

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Viruses

l Very difficult to analyze => difficult to

separate/destroy from water

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Dilutants

l Altogether about 70 compounds l Hydrogarbons, alcohols, aethers, esters,

aldehydes, ketones

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MTBE, TAME

l Additives in petrol l Are diluted very easily in water => the

first compounds found in case of pollution

l Easy to detect by smell and taste (0,03

mg/l)

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Pesticides

l Hundreds of compounds l Max allowed 0,0005 mg/l (total) l The smallest amounts which can be

detected are normally 0,00001 – 0,00002 mg/l

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Radioactivity

l Mostly in deep wells (in the rock) l No smell, no colour, no taste ! l Radon is the most common one in

groundwater

l Max allowed 1000 Bq/l)

=> 1. new water source, 2. treatment (aeration, active carbon filtration)

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Uranium

l Lack of knowledege concerning health

effects

l Earlier max by WHO 0,15 mg/l, today

0,002 mg/l

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Corrosion

l pH > 7,5 l alkalinity > 0,6 mmol/l l calsium > 10 mg/l l oxygen > 2 mg/l

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Maps and aerial photographs

l Swamps, springs,

ditches, etc.

l Humidity changes out

  • f photgraphs

l Old maps might give

valuable information

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Geophysical methods

l Seismic sounding l Electrical probing (resistance)

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Drillings

l Manually l Machinery

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Iron and manganese

l Most common quality problem with

ground waters

l Coagulation happens immediately with

  • zygen

l Iron can be removed also biologically

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Removal of Fe and Mg

l In small scales

– aeration – sand filtration – ion exchange processes

l Lime stone filtration l Slow sand filtration

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Slow sand filtration

l Water is filtered slowly through a sand

layer

l Surface load 0,05 – 0,2 m/h l Water per one 1 m2: 50 – 200 l/h l Iron content max 1mg/l l Pretreatment could be done by a filter

containing crushed stone

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Sand filtration

l Aeration needed almost always l Dissolved iron is oxidized => can be

filtered out of water

l Surface load normally 4 – 5 m/h l Small filters require backwashing more

  • ften

l Might be expensive ?

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UV desinfection

l Generally, ground water is

microbiologically clean

l Sometimes we have experienced pollution l UV-desinfiction is applicable method for

ground waters (no turbidity nor colour)

l UV-desinfection is not affecting the taste

  • f water unlike chlorination
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Ground water protection !

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Raato