terra mdc limited - waitaki district...the site lies within an area where seismic shaking 4 from an...

13
Page | 1 4 April 2016 Terra MDC Limited 1/326 Moray Place Dunedin 9016 New Zealand Ph/Fax: +64 (0) 3 477 0090 Mob: +64 (0) 220 737 480 E-mail: [email protected] Web: www.TerraMDC.co.nz For Attention: Mike Forgie Project Reference: 201603114 Waitaki District Council c/o Forgie Hollows & Associates (Oamaru) Ltd P O Box 32 Oamaru 9444 Dear Mike, RE: Geotechnical Assessment of Land for the proposed new Cultural and Arts Facilities at 9 Thames Street Oamaru This report has been prepared as a preliminary geotechnical assessment of the above property and provides a summary of the likely ground conditions and a preliminary geotechnical hazard assessment. It is understood that Waitaki District Council (WDC) wish to develop the existing building and the rear car-parking area into a new Cultural and Arts Facility. This will involve a new three storey building to be formed, which you have advised will cover most of the rear car-parking area (refer MacKenzie Architects concept drawing for the basement layout 855/D201Feb2016). The data provided and the findings of this report are based upon a site walkover completed on 9 th March 2016 by the undersigned, along with reference made to the Otago Regional Council (ORC), WDC’s District Plan information and the Geological and Nuclear Sciences (GNS) databases. Five Scala penetrometers (SP01 - SP05) and three test pits (TP01 – TP03) were excavated at the proposed site and these along with a number of photos taken during the site visit are attached for your reference. It is considered that the ground investigation and initial geotechnical design assumptions will be required to be verified by a suitably experienced engineer during foundation construction to confirm the observations and conclusions made in this assessment. Further investigations including deeper drilling may be required dependent upon the final building layout and design. Observations around the Property and Immediate Environs The site fronts onto Thames St, with the rear carpark accessed via a driveway from Humber St which winds around a landscaped area. It is zoned in Business Area ‘H’ (BH) as determined from the WDC Zones Map 76, with a total area of 1012 m 2 . The building on the site is deemed to be a heritage building (H29). It is currently owned by the WDC and used as an art gallery. The neighbouring site to the north is also listed as a heritage building (H38) and is owned by ANZ bank, while the southern site is owned and operated by the Steam Café. Property information 1 for 9 Thames Street Oamaru: Land Zone = BUS H Legal Description = SEC 1 BLK IV OAMARU TOWN Area = 0.1012ha 1 Property and Rates information provided by WDC: http://www.waitaki.govt.nz

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Page 1: Terra MDC Limited - Waitaki District...The site lies within an area where seismic shaking 4 from an Alpine Fault Magnitude 8.0 (1:100 year) event can expect Modified Mercalli Intensity

Page | 1

4 April 2016

Terra MDC Limited

1/326 Moray Place

Dunedin 9016

New Zealand

Ph/Fax: +64 (0) 3 477 0090

Mob: +64 (0) 220 737 480

E-mail: [email protected]

Web: www.TerraMDC.co.nz

For Attention: Mike Forgie Project Reference: 201603114

Waitaki District Council

c/o Forgie Hollows & Associates (Oamaru) Ltd

P O Box 32

Oamaru 9444

Dear Mike, RE: Geotechnical Assessment of Land for the proposed new

Cultural and Arts Facilities at 9 Thames Street Oamaru

This report has been prepared as a preliminary geotechnical assessment of the above property and

provides a summary of the likely ground conditions and a preliminary geotechnical hazard assessment.

It is understood that Waitaki District Council (WDC) wish to develop the existing building and the rear

car-parking area into a new Cultural and Arts Facility. This will involve a new three storey building to be

formed, which you have advised will cover most of the rear car-parking area (refer MacKenzie Architects

concept drawing for the basement layout 855/D201Feb2016).

The data provided and the findings of this report are based upon a site walkover completed on 9th March

2016 by the undersigned, along with reference made to the Otago Regional Council (ORC), WDC’s

District Plan information and the Geological and Nuclear Sciences (GNS) databases.

Five Scala penetrometers (SP01 - SP05) and three test pits (TP01 – TP03) were excavated at the

proposed site and these along with a number of photos taken during the site visit are attached for your

reference. It is considered that the ground investigation and initial geotechnical design assumptions will

be required to be verified by a suitably experienced engineer during foundation construction to confirm

the observations and conclusions made in this assessment. Further investigations including deeper

drilling may be required dependent upon the final building layout and design.

Observations around the Property and Immediate Environs

The site fronts onto Thames St, with the rear carpark accessed via a driveway from Humber St which

winds around a landscaped area. It is zoned in Business Area ‘H’ (BH) as determined from the WDC

Zones Map 76, with a total area of 1012 m2. The building on the site is deemed to be a heritage building

(H29). It is currently owned by the WDC and used as an art gallery. The neighbouring site to the north

is also listed as a heritage building (H38) and is owned by ANZ bank, while the southern site is owned

and operated by the Steam Café. Property information1 for 9 Thames Street Oamaru:

• Land Zone = BUS H

• Legal Description = SEC 1 BLK IV OAMARU TOWN

• Area = 0.1012ha

1 Property and Rates information provided by WDC: http://www.waitaki.govt.nz

Page 2: Terra MDC Limited - Waitaki District...The site lies within an area where seismic shaking 4 from an Alpine Fault Magnitude 8.0 (1:100 year) event can expect Modified Mercalli Intensity

Page | 2

The WDC water services map indicates a 150mm diameter sewer pipe bisecting the southern corners

of the site and a 150mm diameter stormwater pipe crossing alongside the drive way on the eastern

corner of the site. Initial ground scanning by local contractor Whitestone also indicated other old cables

or metallic pipes are buried within the site.

Review of Geological Hazards and Other Information

The bedrock geology of the area, as recorded on the GNS Geology Webmaps2, is noted to be in the

late Pleistocene Sediments Group. These are described as gravels, sand and silt of low river terraces

with patchy loess cover in places. A geological boundary is located approximately 50m to the south of

the site, where the shallow bedrock geology is noted to be in the Waiareka Volcanics Alma group. These

are described as agglomerated tuffs, basaltic dikes, sills and pillow lava.

The test pit and Scala testing indicated a soils strata comprising:

• 0.1m to 0.5m = Topsoil with many roots and tree stumps in landscape areas (made ground) or,

• 0.2m to 0.3m (SP04 only) = angular fine to coarse gravels in car-parking area (made ground)

• 0.5m to 3.2m = Soft to firm silt with traces of fine sand (loess)

• 3.2m to 3.5m = Medium dense to dense sandy gravel with occasional cobbles (alluvium).

Ground water was not encountered, with the soils typically dry in the upper 1.0m, i.e. desiccated and

thereafter the soil is damp with increasing depth below this crusted layer. There is some variation within

the soils with localised softer soil strata encountered at depth below 1.0m. The nearby Oamaru Creek

was flowing at relatively low levels at time of investigation, however it is considered this water level

would interconnect to the sandy gravel stratum encountered beneath the site.

The ORC Hazards3 database makes note of a flood hazard area around the Oamaru Creek which

approaches to within 100m of the site. It is noted the site is approximately 5m above the watercourse.

The ORC Hazards database also notes that the site lies on an area with low susceptibility to liquefaction

during an expected shaking intensity of 1:100 year earthquake. The nearest fault to the site is the

Awamoa Creek Fault which is approximately 2.6km away, this fault is determined to be currently

inactive. The nearest active fault is the Stone Wall Fault which is approximately 32km from the site.

The site lies within an area where seismic shaking4 from an Alpine Fault Magnitude 8.0 (1:100 year)

event can expect Modified Mercalli Intensity (MMI) of 6. The requirements of NZSL 1170 ‘Structural

Design Actions’ would prevail in any structural design. The site lies within what is determined as Class

‘C’ – Shallow Stiff Soils, per NZS: 1170 - Part 5.

The site does not lie within any mapped active alluvial fan hazard zone or active land slide zone.

Discussion and Conclusions:

The shallow soils strata underlying the site is assessed as approximately 3.0m to 3.5m thick layer of

firm (or compact) silty loessial soil overlying typically medium dense to dense sandy gravel. There are

some variable thickness of made ground overlying this soil strata, either a loose topsoil in the

landscaped areas or a medium dense to dense angular gravel which formed the car-parking surface.

It is considered that the upper 1.0m to 1.2m of soils strata is an unsuitable stratum for bearing any new

building foundations upon. Localised ‘soft spots’ may also be encountered at greater depths which

would also need to be removed and replaced with engineering fill. It is considered a suitable strip

foundation stratum may be achieved for any new building development at depths below 1.0m to 1.2m

where an allowable bearing capacity >100kPa may be inferred from the Scala Penetrometer test results

i.e. on ‘good ground’ per NZS: 3604 ‘Timber Framed Buildings’. However as the proposed building is a

multi-storey structure with a complex layout it is considered likely that there will be specific foundation

2 GNS website: http://data.gns.cri.nz/geology 3 ORC website: http://hazards.orc.govt.nz/Exponare/ORCWebMaps-advanced-1280x994.aspx 4 Opus – Seismic Risk in Otago Region, May 2005

Page 3: Terra MDC Limited - Waitaki District...The site lies within an area where seismic shaking 4 from an Alpine Fault Magnitude 8.0 (1:100 year) event can expect Modified Mercalli Intensity

Page | 3

design and detailing required. This will likely necessitate specific rafted or strip foundations or even

deeper foundations to be formed down into the sandy gravel stratum, the latter which could be

undertaken more efficiently with bored cast insitu or driven piles. Consideration to gross and differential

settlement along with design loads for bearing shall need to be included in overall foundation design.

The soils are typically damp at 1.0m depth and greater, however the underlying ground water table was

not encountered. It is considered the water table would be coincident with the sandy gravels and will

likely be interconnected to the nearby Oamaru Creek. Appropriate drainage will be required including

replacement of the existing building stormwater and potentially sewer drainage. It is noted the soils

closest to the existing building are typically softer than further out into the car parking area and it is

considered this is likely due to leaking stormwater drainage.

The difficulties associated with deep excavations will need to be considered if deep foundations and

excavations for a basement or retaining walls are required. Underpinning or staging of excavations at

the existing building or boundary walls of adjacent properties may be required, such that there is no

potential for destabilising or undermining of the existing buildings foundations.

Where driven piling is adopted there must be consideration given as to what the effects of the

construction vibrations will have on the existing building and adjacent structures.

Deep excavations will require to consider and plan appropriately for the temporary control and

management of groundwater ingress, including discharges if pumping is required. New storm water

drainage and any structural back of wall drainage plus any new foul piped outfalls should be integrated

to tie into existing piped services.

The site is not considered to be prone to significant damage from potential land hazards, including

liquefaction or land sliding. There should be some consideration given to the potential for flooding

hazard from the nearby Oamaru Creek. Suitable topographical survey should be undertaken at the site

with a level check made on relative levels to the nearby Oamaru Creek at the bed and the top of the

bank of the watercourse.

It is likely that the new development will extensively disturb or remove the existing landscaping and as

such new landform will be made. This may require alterations to the current driveway and retaining

walls dependant on final design and geometrics of the building floor levels and driveway and accesses.

It may be necessary to undertake further specific investigation to establish with a higher degree of

accuracy the ground and groundwater conditions as a detailed design evolves, this may involve deeper

rotary or cone penetrometer (CPT) drilling.

Appropriate drainage and new landscaping should be designed to accommodate the layout and

infrastructure associated with the new house. As a minimum, any soils left exposed by the works should

be covered with a topsoil and grassed or re-vegetated to promote good erosion control.

I trust the above information and recommendations are sufficient that your proposed planning and

funding application for the new development may continue as per envisaged.

Yours sincerely,

James Molloy

For Terra MDC Ltd

Enclosures: • Plates 1 to 6 of Site Reconnaissance and Investigation

• Site Investigation Location Plan

• Test Pit and Scala Penetrometer logs

Page 4: Terra MDC Limited - Waitaki District...The site lies within an area where seismic shaking 4 from an Alpine Fault Magnitude 8.0 (1:100 year) event can expect Modified Mercalli Intensity

Page | 4

Plate 1: Looking across carparking area toward Steam Café, with existing building to the rear right.

Plate 2: Test pit TP01 being excavated to rear of building.

Page 5: Terra MDC Limited - Waitaki District...The site lies within an area where seismic shaking 4 from an Alpine Fault Magnitude 8.0 (1:100 year) event can expect Modified Mercalli Intensity

Page | 5

Plate 3: Existing stormwater piped drainage from building to outfall along northern boundary of the site.

Plate 4: Test pit TP01 arisings, noting thick layer of topsoil in upper strata of excavation.

Page 6: Terra MDC Limited - Waitaki District...The site lies within an area where seismic shaking 4 from an Alpine Fault Magnitude 8.0 (1:100 year) event can expect Modified Mercalli Intensity

Page | 6

Plate 5: Excavation and arisings from Test Pit TP02.

Page 7: Terra MDC Limited - Waitaki District...The site lies within an area where seismic shaking 4 from an Alpine Fault Magnitude 8.0 (1:100 year) event can expect Modified Mercalli Intensity

Page | 7

Plate 6: Excavation and arisings for Test Pit TP03.

Page 8: Terra MDC Limited - Waitaki District...The site lies within an area where seismic shaking 4 from an Alpine Fault Magnitude 8.0 (1:100 year) event can expect Modified Mercalli Intensity

OF

Key

Scala Penetrometer

Test Pit

Refer to test pit and scala logs for ground information

1SHEET 1

SKETCH SHEET

PROJECT: WDC Cultural and Art facilities CLIENT: Waitaki District Council

DATE: 09/03/16SKETCH BY: Regan LordPROJECT No: 201603114

SUBJECT: Site Investigation Location Plan

SP03

TP01

SP02

SP04

SP05

SP01

TP03

TP02

Page 9: Terra MDC Limited - Waitaki District...The site lies within an area where seismic shaking 4 from an Alpine Fault Magnitude 8.0 (1:100 year) event can expect Modified Mercalli Intensity

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Page 10: Terra MDC Limited - Waitaki District...The site lies within an area where seismic shaking 4 from an Alpine Fault Magnitude 8.0 (1:100 year) event can expect Modified Mercalli Intensity

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1900

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#N

/A2400

#N

/A2400

#N

/A

2500

715

190

2500

#N

/A2500

#N

/A2500

#N

/A

2600

715

190

2600

#N

/A2600

#N

/A2600

#N

/A

2700

715

190

2700

#N

/A2700

#N

/A2700

#N

/A

2800

10

23

260

2800

#N

/A2800

#N

/A2800

#N

/A

2900

14

33

310

2900

#N

/A2900

#N

/A2900

#N

/A

3000

#N

/A3000

#N

/A3000

#N

/A3000

#N

/A

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Page 11: Terra MDC Limited - Waitaki District...The site lies within an area where seismic shaking 4 from an Alpine Fault Magnitude 8.0 (1:100 year) event can expect Modified Mercalli Intensity

1

TPLOG.PUB

Site Investigation

Test Pit Log

Contract Title: WDC cultural facilities redevelopment Client: Waitaki District Council Contract No.: 201603114 Weather: Overcast Date: 09/03/16 Logged By: James Molloy Excavator: 14 tonne digger

Dark brown topsoil, soft with bark chippings ~ 50-100mm. Many tree roots with the occasional stumps.

Yellow brown SILT with traces of sand. Soft with low plasticity and in damp condition. Occasional roots in upper 1.0m. (Loess) (damage 4” clay pipe at back of test pit damaged during excavation)

HSV at 0.8m 135/120/105

Hard digging

Yellow brown clayey, fine to coarse gravel, much medium to coarse sand and occasional cobbles. Medi-um dense, damp to moist. (Alluvium)

End of Test Pit at 3.5m

Note: 4” pipe repaired and back filled with arisings. Possible softened ground due to poor drainage of water off building.

4 Photos, hole stable., slight belling of hole in the gravel layer.

Water @ Depth Soils Description

1.0m

2.0m

1.5m

TRIAL PIT No. TP01

0.5m

2.5m

3.0m

0.0m - 0.5m

0.5m - 3.2m

3.5m

4.0m

3.2m - 3.5m

Page 12: Terra MDC Limited - Waitaki District...The site lies within an area where seismic shaking 4 from an Alpine Fault Magnitude 8.0 (1:100 year) event can expect Modified Mercalli Intensity

2

TPLOG.PUB

Site Investigation

Test Pit Log

Contract Title: WDC cultural facilities redevelopment Client: Waitaki District Council Contract No.: 201603114 Weather: Overcast Date: 09/03/16 Logged By: James Molloy Excavator: 14 tonne digger

Dark brown topsoil, soft with bark chippings ~ 50-100mm in dry condition. Many tree roots with the occasional stumps.

Yellow brown SILT with traces of sand. Soft with low plasticity and in dry condition. Occasional roots in upper 1.0m. (Loess).

HSV at 0.6m 100/100/105

Becoming firm to stiff at 1.0m

Hard digging.

End of Test Pit at 1.8m

Note: 3 Photos, hole stable and dry

Water @ Depth Soils Description

1.0m

2.0m

1.5m

TRIAL PIT No. TP02

0.5m

2.5m

3.0m

0.0m - 0.3m

0.3m - 1.8m

3.5m

4.0m

Page 13: Terra MDC Limited - Waitaki District...The site lies within an area where seismic shaking 4 from an Alpine Fault Magnitude 8.0 (1:100 year) event can expect Modified Mercalli Intensity

3

TPLOG.PUB

Site Investigation

Test Pit Log

Contract Title: WDC cultural facilities redevelopment Client: Waitaki District Council Contract No.: 201603114 Weather: Overcast Date: 09/03/16 Logged By: James Molloy Excavator: 14 tonne digger

Dark brown topsoil, soft with bark chippings ~ 50-100mm in dry condition. Many tree roots with the occasional stumps.

Yellow brown SILT with traces of sand. Soft with low plasticity and in dry condition from 0.1 - 1.2m turning slightly damp until 2.3m. Occasional roots in upper 1.0m. (Loess)

End of Test Pit at 2.3m

Note: 3 Photos, hole stable and dry

Water @ Depth Soils Description

1.0m

2.0m

1.5m

TRIAL PIT No. TP03

0.5m

2.5m

3.0m

0.0m - 0.1m

0.1m - 2.3m

3.5m

4.0m