acid sulfate soils - maryborough area · 25 42 25 36 25 30 25 24 25 18 152 36 152 42 152 48 152 54...

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25 42 25 36 25 30 25 24 25 18 152 36 152 42 152 48 152 54 152 36 152 42 152 48 152 54 25 42 25 36 25 30 25 24 25 18 71 60 000m N 72 05 000m N 65 70 75 80 85 90 95 00 71 60 000m N 72 05 000m N 65 70 75 80 85 90 95 00 4 60 000m E 4 95 000m E 65 70 75 80 85 90 4 60 000m E 4 95 000m E 65 70 75 80 85 90 Toogoom Pialba Urangan Maaroom Torbanlea TORBANLEA - PIALBA ROAD BRUCE HIGHWAY BOONOOROO ROAD MARYBOROUGH HERVEY BAY Dundowran S us an R i v e r Mary R iv e r Granville Tinana MARYBOROUGH TUAN FOREST ROAD Bingham Walligan Takura Hervey Bay G r e a t S andy S t r a i t Owanyilla Boonooroo Tuan Mungar BRUCE HIGHWAY Oakhurst Mary River Tinana Creek Sugar Mill HERVEY BAY (CITY) MARYBOROUGH (CITY) WOOCOO TIARO TIARO 26 00 25 30 25 00 152 30 153 00 152 30 153 00 26 00 25 30 0 15 15 km km SCALE Point Vernon Tawan Toolara Forest Coonarr Burrum Heads Buxton Horton Toogoom Colton Mount Benargie Sunny Glen Bauple Mount Urah Woolooga Woodgate HERVEY BAY LOCALITY MAP Study Area Maryborough - Hervey Bay Study Maryborough - Tiaro Study Urangan Pialba Hervey Bay Torquay Pialba South Bingham Lynwood Isis Junction Takura Howard Burrum Torbanlea Duckinwilla Aldershot Mount Doongul Oakhurst Maryborough Yengarie Childers Cordalba G R E A T S A N D Y S T R AI T Maaroom Boonooroo Tuan Tinnanbar Tin Can Bay Toolara Brooweena Pilerwa Aramara Blackmount Tiaro Netherby Gundiah Gootchie Gunalda Grout Mountain NA NA LP a0S2 LP NA a1S2 S2 LP A0S1 S2 NA LP NA LP LP NA S2 NA NA NA NA NA NA NA LP NA NA NA NA NA A0S2 NA NA NA a0S3/S4 NA NA S0 A0S2 S0 A0S2 LP A0S2 NA LP A0S1 S0 LP a0S1 LP a1S2 LP a1S2 A0S2 S0 a1S2 A0S2 A0S0 LP A0S1 A0S0 A0S1 NA NA A0S2 A0S1 NA S0 LP NA NA NA LP NA A0S1 LP LP A0S1 LP A0S2 A0S1 S0 LP A1S2 A0S1 NA A0S1 A0S1 LP LP S0 NA LP S0 A0S1 NA LP A0S1 S0 NA LP A0S1 A0S2 A0S1 NA A2S3/S4 LP A1S3/S4 NA LP A0S2 A1S2 A0S1 S3/S4 NA A0S1 LP NA A0S3/S4 A0S2 a0S3/S4 A1S2 A2S3/S4 A0S1 A0S1 S0 LP A0S1 LP A1S2 A1S1 LP A0S1 S0 A2S3/S4 S3/S4 A0S1 A1S2 NA LP NA NA a0S2 NA a0S3/S4 a0S2 LP LP A1S0 LP NA NA LP S3/S4 LP LP LP A0S2 LP LP NA A0S2 LP NA NA NA A0S2 NA A0S1 LP LP A0S1 LP A0S1 LP A0S1 a0S1 a0S1 a0S1 LP S3/S4 S3/S4 S3/S4 NA NA NA S2 NA LP NA S3/S4 NA LP NA LP NA NA NA S3/S4 LP LP LP S3/S4 LP S2 LP NA NA NA S3/S4 NA S3/S4 S3/S4 NA S3/S4 S3/S4 NA S3/S4 S3/S4 NA NA NA LP NA LP NA NA NA LP NA LP NA NA NA NA NA NA NA NA NA NA NA 1 2 3 4 5 6 7 8 9 10 11 12 13 14 15 16 17 18 19 20 21 22 23 24 25 26 27 28 29 30 31 32 33 34 ACID SULFATE SOILS - MARYBOROUGH AREA LP NA LAND WITH A LOW PROBABILITY OF ACID SULFATE SOIL OCCURRENCE Land between the 5m AHD contour and the outer limit 5 of Holocene, estuarine ASS (ie. land <5m AHD) as mapped at this scale, with low probability of ASS occurrence. Limited field investigation. LAND NOT ASSESSED Land not assessed for ASS as part of this survey. It may include non ASS land beyond the boundary established as the limit of Holocene, estuarine, pyrite sediments 5 but insufficient or no field testing was carried out. Acid sulfate soil is the generic term used to define soils derived from estuarine sediments containing iron sulfides (pyrite) or containing the acidic products of the oxidation of sulfides. The term includes actual and potential acid sulfate soils. An "A" preceding the soil depth code indicates the probable depth to a soil layer or horizon where a field pH of 4.0 is first encountered. A field pH of 4.0 or less is used as an indicator of an Actual Acid Sulfate Soil (AASS) which has mobile acidity in the form of ionic hydrogen, aluminium, iron or acid salts. Extensive areas with high actual acidity derived from sulfide oxidation may constitute a significant environmental hazard. Some soils with high organic matter may have low pH from organic acids. An 'a' preceding the depth code indicates the probable depth to a soil layer or horizon with field pH ranging from >4.0 to 5.0. This may or may not be a result of ASS oxidation. An "S" preceding the soil depth code indicates the probable depth to a Potential Acid Sulfate Soil (PASS) layer or horizon. PASS are soils where the oxidisable sulfur percentage of pyritic origin exceeds the prescribed 'action criteria 4 ' at which treatment is required if disturbed. Testing for Oxidisable sulfur is conducted by the Total Oxidisable Sulfur (TOS) method, the Chromium Reducible Sulfur (S CR ) method or the Peroxide Oxidisation - Combined Acidity and Sulfate (POCAS) method. Oxidisable sulfur 'Action Criteria' that trigger treatment are currently: Sands, 0.03 S%; Loams to light clays, 0.06 S%; Medium to heavy clays, 0.1 S%. NOTE: For disturbance > 1000 tonnes the action criteria is 0.03% regardless of soil texture. The outer boundary of Holocene estuarine ASS commonly occurs at the intersection with hard rock or other materials of non estuarine origin. It is either at the 5m contour or at lower elevation. This boundary is established using limited field checking at the boundary itself, together with the use of contour lines and geological map boundaries. There is no field assessment beyond the 5m AHD contour level. It should be noted, however, that certain lithologies on land above 5m AHD may contain sulfidic material of non estuarine/Holocene origin. Additionally, much older, estuarine, pyritic sediments may occur at depth on land >5m AHD. NOTE: This map should be used in conjunction with the accompanying report covering this area. Borehole locations where profiles were described in detail and samples taken for analysis Local Authority boundary Digital Cadastral Data Base 1 2 3 4 5 REFERENCE 0 1 1000 2 3 4 metres kilometres SCALE 1 : 50 000 Projection: Universal Transverse Mercator (MGA Zone 56) Horizontal Datum: GEOCENTRIC DATUM OF AUSTRALIA (GDA94) Note: This map is GDA94 compliant ACCURACY STATEMENT: Due to varying sources of data sets, spatial locations may not coincide when overlaid. Produced at the Indooroopilly Sciences Centre by Natural Resource Information Management, Natural Resource Sciences, Department of Natural Resources and Mines. DISCLAIMER: While every care is taken to ensure the accuracy of this product, the Department of Natural Resources and Mines makes no representations or warranties about its accuracy, reliability, completeness or suitability for any particular purpose and disclaims all responsibility and all liability (including without limitation, liability in negligence) for all expenses, losses, damages (including indirect or consequential damage) and costs which you might incur as a result of the product being inaccurate or incomplete in any way for any reason. CARTOGRAPHY by G J Finney, Natural Resource Information Management, Department of Natural Resources and Mines, Indooroopilly Sciences Centre, Brisbane. C The State of Queensland (Department of Natural Resources and Mines) 2002. PROJECT MANAGEMENT C R Ahern, QASSIT, Natural Resource Sciences, Department of Natural Resources and Mines, Indooroopilly Sciences Centre, Brisbane. SURVEY by P R Wilson, H M Anderson and D M Brown, Natural Resource Services, Department of Natural Resources and Mines, Bundaberg and C R Ahern, QASSIT, Natural Resource Sciences, Department of Natural Resources and Mines, Indooroopilly Sciences Centre, Brisbane. LABORATORY ANALYSIS by Natural Resource Sciences Laboratories, Department of Natural Resources and Mines, Indooroopilly Sciences Centre, Brisbane. 23 Cane Assignments (July 1995) ACID SULFATE SOILS MARYBOROUGH AREA Ref. No. NR&M-MAC-I-A0 3285 0 - 0.5m 0.5 - 1m 1 - 2m 2 - 3m 3 - 4m 4 - 5m >5m 0 1 2 3 4 5 5+ A0 A1 A2 A3 A4 A5 A5+ S0 S1 S2 S3 S4 S5 S5+ Depth Depth Code Depth to Actual Acid Sulfate Soil 2 (pH 4.0) Depth to Potential Acid Sulfate Soil 3 ACID SULFATE SOILS (ASS) 1 ON RELATIVELY UNDISTURBED LAND Depth to Strongly Acidic Soil layer 2 (pH >4.0 to 5.0) a0 a1 a2 a3 a4 a5 a5+ NOTE: A0S2 a1S2 S1/S2 The depth codes above imply that a predominance of profiles in the map unit fall within the nominated depth range. Actual acid sulfate soil layers (designated with an A code) often overlie potential acid sulfate soil layers (designated with an S code). Where this occurs e.g. the map unit is coloured according to the depth of the upper surface of the 'actual' layer (A0) and overlayed with yellow dots. An 'a' preceding the soil depth code e.g. indicates a strong acid soil layer with field pH ranging from >4.0 to 5.0. This may or may not be a result of sulfide oxidation. While 'a' depth code is shown on the map, no colour is assigned to it. In areas where there is varying depth to an ASS layer that cannot be separately mapped at the operative scale, two colours are used to designate the dominant depths. This appears as equal width striped colours. e.g.

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Page 1: Acid Sulfate Soils - Maryborough Area · 25 42 25 36 25 30 25 24 25 18 152 36 152 42 152 48 152 54 152 36 152 42 152 48 152 54 25 42 25 36 25 30 25 24 25 18 7160000mN 7205000mN 65

25 42

25 36

25 30

25 24

25 18

152 36 152 42 152 48 152 54

152 36 152 42 152 48 152 54

25 42

25 36

25 30

25 24

25 18

7160000mN

7205000mN

65

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75

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90

95

00

7160000mN

7205000mN

65

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75

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95

00

460000mE 495000mE65 70 75 80 85 90

460000mE 495000mE65 70 75 80 85 90

Toogoom

Pialba

Urangan

Maaroom

Torbanlea

TORBANLEA - PIALBA

ROAD

BRUC

E HIG

HW

AY

BOONOOROO ROAD

MARYBOROUGH

HERVEY BAYDundowran

Susan River

Mary River

Granville

Tinana MARYBOROUGH TUAN FOREST ROAD

Bingham

Walligan

Takura

Hervey Bay

Great

SandyStrait

Owanyilla

Boonooroo

Tuan

Mungar

BR

UC

E

HIG

HW

AY

Oakhurst

Mary River

Tinana Creek

Sugar Mill

HERVEY BAY (CITY)

MARYBOROUGH (CITY)

WOOCOO

TIARO

TIARO

26 00

25 30

25 00

152 30 153 00

152 30 153 00

26 00

25 30

25 00

0 1515km km

SCALE

Point Vernon

Tawan

Toolara Forest

Coonarr

Burrum HeadsBuxton

Horton

Toogoom

Colton

Mount Benargie

Sunny Glen

BaupleMount Urah

Woolooga

Woodgate

HERVEY BAY

LOCALITY MAP

Study Area

Maryborough - Hervey Bay Study

Maryborough - Tiaro Study

UranganPialba Hervey Bay

Torquay

Pialba South

Bingham

Lynwood Isis Junction

TakuraHowardBurrum

Torbanlea

Duckinwilla

Aldershot

Mount Doongul

Oakhurst

MaryboroughYengarie

Childers

Cordalba

GRE

AT

SAN

DY

STR

AIT

Maaroom

BoonoorooTuan

Tinnanbar

Tin Can BayToolara

BrooweenaPilerwaAramara

BlackmountTiaro

Netherby

GundiahGootchie

Gunalda

Grout Mountain

NA

NA

LPa0S2

LP

NA

a1S2

S2

LP

A0S1

S2

NA

LP

NA

LPLP

NA

S2

NA

NA NA

NA

NA

NA

NA

LP

NA

NA

NA

NANA

A0S2

NA

NA

NA

a0S3/S4

NA

NA

S0

A0S2

S0

A0S2LP

A0S2

NA

LP

A0S1

S0

LP

a0S1

LPa1S2

LP

a1S2

A0S2

S0a1S2

A0S2A0S0

LP

A0S1

A0S0

A0S1

NA

NA

A0S2

A0S1 NA

S0

LP

NA

NA

NA

LP

NA

A0S1LP

LP

A0S1

LP

A0S2

A0S1

S0LP

A1S2

A0S1

NA

A0S1

A0S1

LPLP

S0

NA

LP

S0

A0S1

NA

LP

A0S1

S0

NA

LPA0S1

A0S2

A0S1

NA

A2S3/S4LP

A1S3/S4

NALP

A0S2

A1S2

A0S1

S3/S4

NA

A0S1

LP

NA

A0S3/S4A0S2

a0S3/S4

A1S2A2S3/S4

A0S1

A0S1

S0

LP

A0S1

LP

A1S2

A1S1

LPA0S1

S0

A2S3/S4

S3/S4

A0S1

A1S2

NA

LPNA

NA

a0S2

NA

a0S3/S4

a0S2

LP

LP

A1S0

LP

NA

NA

LP

S3/S4

LPLP

LPA0S2LP LP

NA A0S2

LP

NA

NA

NA

A0S2NA

A0S1LP

LP

A0S1

LP

A0S1

LP

A0S1

a0S1

a0S1a0S1

LP

S3/S4

S3/S4

S3/S4

NA

NA

NA

S2

NA

LP

NA

S3/S4

NA

LP

NA

LP

NA

NA

NA

S3/S4LP

LP

LP

S3/S4

LP

S2

LPNA

NA

NAS3/S4

NA

S3/S4

S3/S4

NAS3/S4

S3/S4

NA

S3/S4

S3/S4

NA

NA

NA

LP

NA

LP

NA

NA

NA

LP

NA

LP

NA

NA

NA

NA

NA

NA

NA

NA

NA

NA

NA

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2

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5

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ACID SULFATE SOILS - MARYBOROUGH AREA

LP

NA

LAND WITH A LOW PROBABILITY OF ACID SULFATE SOIL OCCURRENCE

Land between the 5m AHD contour and the outer limit5 of Holocene, estuarine ASS (ie. land <5m AHD) as mapped at this scale, with low probability of ASS occurrence. Limited field investigation.

LAND NOT ASSESSED

Land not assessed for ASS as part of this survey. It may include non ASS land beyond the boundary established as the limit of Holocene, estuarine, pyrite sediments5 but insufficient or no field testing was carried out.

Acid sulfate soil is the generic term used to define soils derived from estuarine sediments containing iron sulfides (pyrite) or containing the acidic products of the oxidation of sulfides. The term includes actual and potential acid sulfate soils.

An "A" preceding the soil depth code indicates the probable depth to a soil layer or horizon where a field pH of ≤4.0 is first encountered. A field pH of 4.0 or less is used as an indicator of an Actual Acid Sulfate Soil (AASS) which has mobile acidity in the form of ionic hydrogen, aluminium, iron or acid salts. Extensive areas with high actual acidity derived from sulfide oxidation may constitute a significant environmental hazard. Some soils with high organic matter may have low pH from organic acids. An 'a' preceding the depth code indicates the probable depth to a soil layer or horizon with field pH ranging from >4.0 to ≤5.0. This may or may not be a result of ASS oxidation.

An "S" preceding the soil depth code indicates the probable depth to a Potential Acid Sulfate Soil (PASS) layer or horizon. PASS are soils where the oxidisable sulfur percentage of pyritic origin exceeds the prescribed 'action criteria4' at which treatment is required if disturbed. Testing for Oxidisable sulfur is conducted by the Total Oxidisable Sulfur (TOS) method, the Chromium Reducible Sulfur (SCR) method or the Peroxide Oxidisation - Combined Acidity and Sulfate (POCAS) method.

Oxidisable sulfur 'Action Criteria' that trigger treatment are currently: Sands, 0.03 S%; Loams to light clays, 0.06 S%; Medium to heavy clays, 0.1 S%. NOTE: For disturbance > 1000 tonnes the action criteria is 0.03% regardless of soil texture.

The outer boundary of Holocene estuarine ASS commonly occurs at the intersection with hard rock or other materials of non estuarine origin. It is either at the 5m contour or at lower elevation. This boundary is established using limited field checking at the boundary itself, together with the use of contour lines and geological map boundaries. There is no field assessment beyond the 5m AHD contour level. It should be noted, however, that certain lithologies on land above 5m AHD may contain sulfidic material of non estuarine/Holocene origin. Additionally, much older, estuarine, pyritic sediments may occur at depth on land >5m AHD.

NOTE: This map should be used in conjunction with the accompanying report covering this area.

Borehole locations where profiles were described in detail and samples taken for analysis

Local Authority boundary

Digital Cadastral Data Base

1

2

3

4

5

REFERENCE

0 11000 2 3 4metres kilometres

SCALE 1 : 50 000

Projection: Universal Transverse Mercator (MGA Zone 56)Horizontal Datum: GEOCENTRIC DATUM OF AUSTRALIA (GDA94)

Note: This map is GDA94 compliant

ACCURACY STATEMENT:Due to varying sources of data sets, spatial locations may not coincide when overlaid.

Produced at the Indooroopilly Sciences Centre by Natural Resource Information Management, Natural Resource Sciences, Department of Natural Resources and Mines.

DISCLAIMER:While every care is taken to ensure the accuracy of this product, the Department of Natural Resources and Mines makes no representations or warranties about its accuracy, reliability, completeness or suitability for any particular purpose and disclaims all responsibility and all liability (including without limitation, liability in negligence) for all expenses, losses, damages (including indirect or consequential damage) and costs which you might incur as a result of the product being inaccurate or incomplete in any way for any reason.

CARTOGRAPHY by G J Finney, Natural Resource Information Management, Department of Natural Resources and Mines, Indooroopilly Sciences Centre, Brisbane.

C The State of Queensland (Department of Natural Resources and Mines) 2002.

PROJECT MANAGEMENTC R Ahern, QASSIT, Natural Resource Sciences, Department of Natural Resources and Mines, Indooroopilly Sciences Centre, Brisbane.

SURVEY by P R Wilson, H M Anderson and D M Brown, Natural Resource Services, Department of Natural Resources and Mines, Bundaberg and C R Ahern,QASSIT, Natural Resource Sciences, Department of Natural Resources and Mines, Indooroopilly Sciences Centre, Brisbane.

LABORATORY ANALYSIS by Natural Resource Sciences Laboratories, Department of Natural Resources and Mines, Indooroopilly Sciences Centre, Brisbane.

23

Cane Assignments (July 1995) ACID SULFATE SOILSMARYBOROUGH AREA

Ref. No. NR&M-MAC-I-A0 3285

0 - 0.5m

0.5 - 1m

1 - 2m

2 - 3m

3 - 4m

4 - 5m

>5m

0

1

2

3

4

5

5+

A0

A1

A2

A3

A4

A5

A5+

S0

S1

S2

S3

S4

S5

S5+

Depth DepthCode

Depth to ActualAcid Sulfate Soil2

(pH ≤4.0)

Depth to PotentialAcid Sulfate Soil3

ACID SULFATE SOILS (ASS)1 ON RELATIVELY UNDISTURBED LAND

Depth to StronglyAcidic Soil layer2

(pH >4.0 to ≤5.0)

a0

a1

a2

a3

a4

a5

a5+

NOTE:

A0S2

a1S2

S1/S2

The depth codes above imply that a predominance of profiles in the map unit fall within the nominated depth range.

Actual acid sulfate soil layers (designated with an A code) often overlie potential acid sulfate soil layers (designated with an S code). Where this occurs e.g. the map unit is coloured according to the depth of the upper surface of the 'actual' layer (A0) and overlayed with yellow dots. An 'a' preceding the soil depth code e.g. indicates a strong acid soil layer with field pH ranging from >4.0 to ≤5.0. This may or may not be a result of sulfide oxidation. While 'a' depth code is shown on the map, no colour is assigned to it.

In areas where there is varying depth to an ASS layer that cannot be separately mapped at the operative scale, two colours are used to designate the dominant depths. This appears as equal width striped colours. e.g.