evaluation of aggregates for the austrian mineral ... · proposal for resource protection zones 5...

1
Higher terrace ne‘ Erlauf: 85 ha, 14,3 Mio m³ (25,7 Mio t) Higher-/ lower terrace at Loosdorf: 4 ha, 0,15 Mio m³ (0,27 Mio t) Lower terrace at Neumarkt/Y: 171 ha, 5,74 Mio m³ (10,3 Mio t) Lowest terrace e‘ Pöchlarn: 162,1 ha, 20,1 Mio m³ (36,2 Mio t) Lower terrace s‘ Pöchlarn: 25,4 ha, 1,5 Mio m³ (2,8 Mio t) Higher terrace ne‘ Erlauf: 85 ha, 14,3 Mio m³ (25,7 Mio t) Higher-/ lower terrace at Loosdorf: 4 ha, 0,15 Mio m³ (0,27 Mio t) Lower terrace at Neumarkt/Y: 171 ha, 5,74 Mio m³ (10,3 Mio t) Lowest terrace e‘ Pöchlarn: 162,1 ha, 20,1 Mio m³ (36,2 Mio t) Lower terrace s‘ Pöchlarn: 25,4 ha, 1,5 Mio m³ (2,8 Mio t) Volume calculation : above water table: area x (HGW-Flurabstand - 2m – 1m cover) above and below: area x (gravel thickness – 1m cover) Weight calculation : volume x 1,8 t/m³ Stratigraphic classification Resource suitability 1 1409 ha Holocene sediments in large valleys 344 ha Lower Terrace 170 ha Higher Terrace, often with fine-grained cover Resource suitability 2 350 ha Holocene sediments in narrow valleys 124 ha “Deckenschotter“ gravel Type of extraction above water table above and below water table below water table after cutting out settlements incl. 300m buffer, water / nature protection zones Areas off-limits settlements incl. 100m buffer, water / nature protection zones Extended buffer around settlements 300m buffer Areas with restriction on mining operations landscape protection areas, Natura 2000 Resource suitability 1 - best suitability 2 Type of extraction above water table above and below water table below water table Resource suitability 1 - best suitability 2 " " " " " " " " " " " " " " " " " extent of groundwater models extent of sediment thickness models Operating status of gravel pits " active not active Evaluation of aggregates for the Austrian Mineral Resources Plan M. Heinrich, S. Pfleiderer, T. Untersweg & L. Weber The aim of the Austrian Mineral Resources Plan is to preserve access to valuable mineral resources for future generations Heinrich 1986 Phase I: Geological assessment Phase II: Balance check with provincial governments 0 1 2 3 4 5 6 7 8 9 Tonnen [t] Geological Survey of Austria www.geologie.ac.at Leopold Weber [email protected] Maria Heinrich [email protected] Sebastian Pfleiderer [email protected] Thomas Untersweg [email protected] Lithological characterisation of aggregates Distribution of gravel pits and extent of models of sediment thickness and groundwater table Suitable resource zones and type of extraction Remaining resource zones after cutting out no-go areas Superposition of areas where legal restrictions preclude or impede mining 5 km 5 km Quality Quantity small but beautiful lots but no good young terraces older terraces, alluvial fans Tertiary inter- bedded layers taluses colluvium, flow earth examples Geology 1 2 3 4 5 1:AMM 2: AM 3: aM 4: Am 5: am Quality Quantity young terraces older terraces, alluvial fans Tertiary inter- bedded layers taluses colluvium, flow earth examples Geology 1 1 2 5 5 1 1 2 2 3 3 2 2 3 3 3 4 3 3 4 4 4 4 4 4 4 5 5 5 5 1:AMM 2: AM 3: aM 4: Am 5: am Quality Quantity Importance Quality Quan t it y 1: major / supra-reg. 2: major / regional 3: medium 4: medium / minor 5: minor 1 2 3 4 5 Importance Geological Potential 1 1 2 3 5 1: major / supra-reg. 1 1 2 3 5 2: major / regional 1 2 3 4 5 3: medium 2 2 4 4 5 4: medium / minor 3 3 4 5 5 5: minor 1 2 3 4 5 Importance Geological Potential Character accessibility groundwater level sediment cover Average annual consumption per capita sand & gravel dimension stone clay concrete industrial minerals coal raw iron Superposition of land use data and restricted areas - water/nature protection Discussion and Negotiation - land for building Proposal for resource protection zones 5 km 5 km Compiled map of unconsolidated sediments 1:50.000 and location of pilot study (District of Melk) Federal Ministry of Economics and Labour Quality lithology e.g.: sandy gravel, sorted, rounded, intercalations of fine- grained material, rarely conglomerate e.g.: concrete (after sieving) usage best actual / supposed possible Quantity extent thickness tonnes / ha Importance use demand supply Lithological classification rubbish, construction waste, rock fragments of varying composition, mine waste swamp, bog, moor mass movement deposits, landslides mostly gravel and sand; well sorted, regionally consolidated layers gravel, rounded; partly sand, mostly well sorted, regionally fine-grained covers (alluvial clay) mostly gravel; variable rounding and sorting, partly sand, regionally fine-grained covers (alluvial clay) mostly gravel; rounded, mostly sandy, mostly sorted, partially consolidated mostly gravel with sand and silt layers; variable rounding and sorting mostly gravel and sand; rounded, sorted, with silt layers and often thick covers of loess and loam, high proportion of silt “Deckenschotter” gravel coarse debris sand (e.g. Linz-, Melk-formation, kaolinitic sand) silt, sand and gravel; often boulders, mostly angular, unsorted silt and sand, frequently interbedded, mostly well sorted predominantly silt predominantly silt, mostly interbedded, partly sand silt, sand and gravel; rounded, interbedded, sorted, containing coal Maps of aggregate occurrence and uniform legend + quality + quantity Resource regions Evaluation of geological potential in foreland / mountain regions + usage Assessment of importance + character Definition of resource zones compilation of unconsolidated sediment occurrence

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Page 1: Evaluation of aggregates for the Austrian Mineral ... · Proposal for resource protection zones 5 km 5 km Compiled map of unconsolidated sediments 1:50.000 and location of pilot study

Higher terracene‘ Erlauf: 85 ha,14,3 Mio m³ (25,7 Mio t)

Higher-/ lower terraceat Loosdorf: 4 ha,0,15 Mio m³ (0,27 Mio t)

Lower terraceat Neumarkt/Y: 171 ha,5,74 Mio m³ (10,3 Mio t)

Lowest terracee‘ Pöchlarn: 162,1 ha,20,1 Mio m³ (36,2 Mio t)

Lower terraces‘ Pöchlarn: 25,4 ha,1,5 Mio m³ (2,8 Mio t)

Higher terracene‘ Erlauf: 85 ha,14,3 Mio m³ (25,7 Mio t)

Higher-/ lower terraceat Loosdorf: 4 ha,0,15 Mio m³ (0,27 Mio t)

Lower terraceat Neumarkt/Y: 171 ha,5,74 Mio m³ (10,3 Mio t)

Lowest terracee‘ Pöchlarn: 162,1 ha,20,1 Mio m³ (36,2 Mio t)

Lower terraces‘ Pöchlarn: 25,4 ha,1,5 Mio m³ (2,8 Mio t)

Volume calculation:above water table: area x (HGW-Flurabstand - 2m – 1m cover)above and below: area x (gravel thickness – 1m cover)

Weight calculation: volume x 1,8 t/m³

Stratigraphic classificationResource suitability 11409 ha Holocene sediments in large valleys

344 ha Lower Terrace

170 ha Higher Terrace, often with fine-grained cover

Resource suitability 2

350 ha Holocene sediments in narrow valleys

124 ha “Deckenschotter“ gravel

Type of extractionabove water table

above and belowwater table

below water table

after cutting out settlements incl. 300m buffer, water / nature protection zones Areas off-limitssettlements incl. 100m buffer, water / nature protection zones

Extended buffer around settlements300m buffer

Areas with restriction on mining operationslandscape protection areas, Natura 2000

Resource suitability1 - best suitability

2

Type of extraction

above water tableabove and belowwater tablebelow water table

Resource suitability1 - best suitability2

"

"

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"

"

"

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"

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"

"

"

"

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extent of groundwater modelsextent of sediment thickness models

Operating status of gravel pits" active

not active

Evaluation of aggregates for the Austrian Mineral Resources PlanM. Heinrich, S. Pfleiderer, T. Untersweg & L. Weber

The aim of the Austrian Mineral Resources Plan is to preserve access to valuable mineral resources for

future generations

Heinrich 1986

Phase I: Geological assessment

Phase II: Balance check with provincial governments

Durchschnittlicher jährlicher Pro-Kopf-Verbrauch

0 1 2 3 4 5 6 7 8 9

Roheisen

Kohle

Industrieminerale

Zement

Tone

Natursteine

Kies & Sand

Tonnen [t]

Geological Survey of Austria www.geologie.ac.at

Leopold Weber [email protected]

Maria Heinrich [email protected] Pfleiderer [email protected] Untersweg [email protected]

Lithological characterisation of aggregates

Distribution of gravel pitsand extent of models ofsediment thickness and

groundwater table

Suitable resource zones and type of extraction

Remaining resource zones after cutting out no-go areas

Superposition of areas wherelegal restrictions preclude

or impede mining

5 km

5 km

5 km

Qu

ality

Quantity

small butbeautiful

lots but no good

young terraces

older terraces,alluvial fans

Tertiary inter-bedded layers

taluses

colluvium, flow earth

examplesGeology

112551

122332

233343

344444

445555

1:AMM2: AM3: aM4: Am5: amQuality

Quantity

young terraces

older terraces,alluvial fans

Tertiary inter-bedded layers

taluses

colluvium, flow earth

examplesGeology

112551

122332

233343

344444

445555

1:AMM2: AM3: aM4: Am5: amQuality

Quantity

Imp

ort

an

ce

Qu

ality

Quantity

112351: major / supra-reg.

112352: major /regional

123453: medium

224454: medium/ minor

334555: minor12345Importance

GeologicalPotential

112351: major / supra-reg.

112352: major /regional

123453: medium

224454: medium/ minor

334555: minor12345Importance

GeologicalPotential

Character

accessibility groundwaterlevel

sedimentcover

Average annual consumption per capita

sand & gravel

dimension stone

clay

concrete

industrial minerals

coal

raw iron

Superposition of land use data and restricted areas

- water/nature protection

Discussion and Negotiation

- land for building

Proposal for resource protection zones

5 km

5 km

Compiled map of unconsolidated sediments 1:50.000 and location of pilot study (District of Melk)

Federal Ministry ofEconomics and Labour

Quality

lithology

e.g.: sandy gravel,sorted, rounded,intercalations of fine-grained material,rarely conglomerate

e.g.: concrete(after sieving)

usagebest actual / supposed possible

Quantity

extent thickness

tonnes / ha

Importance

use demand

supply

Lithological classificationrubbish, construction waste, rock fragmentsof varying composition, mine waste

swamp, bog, moor

mass movement deposits, landslides

mostly gravel and sand; well sorted, regionally consolidated layers

gravel, rounded; partly sand, mostly well sorted,regionally fine-grained covers (alluvial clay)

mostly gravel; variable rounding and sorting, partlysand, regionally fine-grained covers (alluvial clay)

mostly gravel; rounded, mostly sandy, mostly sorted, partially consolidated

mostly gravel with sand and silt layers; variable rounding and sorting

mostly gravel and sand; rounded, sorted,with silt layers and often thick covers of loess and loam, high proportion of silt

“Deckenschotter” gravel

coarse debris

sand (e.g. Linz-, Melk-formation, kaolinitic sand)

silt, sand and gravel; often boulders, mostlyangular, unsorted

silt and sand, frequently interbedded, mostly well sorted

predominantly silt

predominantly silt, mostly interbedded, partly sand

silt, sand and gravel; rounded, interbedded, sorted, containing coal

Maps of aggregate occurrence and uniform legend

+ quality + quantity

Resource regions

Evaluation of geological potential inforeland / mountain regions

+ usage

Assessment of importance

+ character

Definition of resource zones

compilation of unconsolidated sediment occurrence