1Geotechnica 2016 | 6th & 7th July 2016 | Brunel University, London | www.geotechnica.co.uk
www.marchetti-dmt.it
Flat Dilatometer (DMT) and Seismic Dilatometer (SDMT):
Applications and Recent Developments
Diego Marchetti – [email protected]
Paola Monaco – [email protected]
Silvano Marchetti – [email protected]
L’Aquila University
In cooperation with:
In penetrable soils:
Lab Testing In situ: CPT & DMT
Reason: simple, fast, economical,
repeatable, provides continuous soil profile,
results real time, ..
In Sand :
recovering undisturbed samples very difficult
and in situ testing is the state-of-practice.
17th Int. Conf. on Soil Mechanics and Geotechnical Engng, 2009
State-of-the-art Lecture No. 1 (Alessandria Egypt Oct 2009)
Mayne P.W. Georgia Institute of Technology, Atlanta, USA
Coop M.R. Imperial College, London, UK
Springman S.M. Swiss Federal Institute of Technology, Zurich, CH
Uang A.B. National Chiao Tung University, Taiwan, China
Zornberg J.G. University of Texas, Austin, USA
“Soil borings … laboratory testing … SPT … pressuremeter (PMT) … vane(VST) … crosshole (CHT) … Taken together, all of these are suitable … yetat considerable cost in time and money…”
TOO SLOW !
Mayne et al: State-of-the-Art Lecture (Alexandria Egypt 2009)
17th Int. Conference on Soil Mechanics and Geotechnical Engineering
SCPT & SDMT fast and convenient tools for everyday investigations
DMT Test Layout
blade
rods
penetration
machine
pneumatic-electric cable control box
gas tank
(air, nitrogen,etc)
Test Procedure
advance 20 cm
stop penetration
P0: Lift-off pressure
P1: Pressure for
1.1 mm expansion
DMT using TORPEDO + DRILL-RIG
Test starts from bottom of a borehole (like SPT, but 3-5m long)
≈ 40 m / day
ability to overcome obstacles
usually
3 - 5 m
Role of penetration for the DMT
Difference with CPT: measurements taken during
penetration at a fix speed of 2 cm / sec
DMT readings taken when blade is not moving
Penetration is only to advance the blade to next test
depth – no strict constraint on penetration speed.
High flexibility to advance DMT in the soil
EUROCODE 7 (1997) ASTM (2007) TC16 (1997) ISO (2016)
SDMT used in over 70 countries (°) (200 DMT in US)
(°) Algeria, Angola, Argentina, Australia, Austria, Bahrain, Bangladesh, Belgium, Bolivia, Bosnia, Brazil, Bulgaria, Canada, Czech
Republic, China, Chile, Cyprus, Colombia, Costa Rica, Croatia, Denmark, Ecuador, Egypt, United Arab Emirates, Estonia, Finland,
France, Germany, Greece, Guadalupe, Guatemala, Honduras, Hong Kong, Hungary, India, Indonesia, Iran, Ireland, Israel, Italy, Japan,
Korea, Kosovo, Kuwait, Lithuania, Malaysia, Netherland, New Zealand, Norway, Oman, Pakistan, Paraguay, Philippines, Poland,
Portugal, Romania, Russia, Saudi Arabia, Serbia, Singapore, Slovenia, South Africa, Spain, Sri Lanka, Sweden, Switzerland, Taiwan,
Thailand, Tunisia, Turkey, United Kingdom, United States of America, Venezuela, Vietnam.
Soils testable by DMT/SDMT
DMT• ALL SANDS, SILTS, CLAYS• Very soft soils (Cu = 2-4 kPa, M=0.5 MPa)
• Hard soils/Soft Rock (Cu = 1 MPa, M=400 MPa)
• Blade robust (safe push 25 ton)
SDMT• All penetrable soils
• Non penetrable soils (gravel, rock, ..):
inside a backfilled borehole
Max depth: 135 m in L’Aquila (2009)
SDMT main results and repeatability (≈ 1-2%)
other results: OCR (clay), K0 (clay), ɣ, ɸ (sand), Ch, Kh, VP ,…
Field Data
Z
(m)
P0
(kPa)
P1
(kPa)
0.20
0.40
0.60
0.80
1.00
1.20
…
220
210
305
310
285
290
…
300
310
420
450
380
390
…
DMT Intermediate parameters
Intermediate ParametersDMT Field Readings
P0
P1
Kd: Horizontal Stress Index
Ed: Dilatometer Modulus
Id: Material Index
DMT Formulae – Interpreted parameters
Intermediate
Parameters
Id
Kd
Ed
Interpreted Geotechnical Parameters
Cu: Undrained Shear Strength (clay)
Ko: Earth Pressure Coeff (clay)
OCR: Overconsolidation ratio (clay)
: Safe floor friction angle (sand)
: Unit weight and description
M: Constrained Modulus
ID contains information on soil type
Performing DMT, immediately notice that:
p1
CLAY
pp0
SAND
p0
p1
p
SILT falls in between
ID=(p0 -u0)
(p1 -p0)
Definition of KD (Horizontal stress index)
KD is an ‘amplified’ K0, because p0 is
an ‘amplified’ σh, due to penetration
KD =σ’v
(p0 - u0)
p0
D
M
T
same formula as K0: (p0 – u0) σ’h
De
pth
Z
KD
KD information on stress history
2
KD = 2 in NC clay (OCR = 1)
NC
OC
KD > 2 in OC clay (OCR > 1)
CLAY: KD correlated to OCR
ExperimentalKamei & Iwasaki 1995
TheoreticalFinno 1993
TheoreticalYu 2004
OCR = Kd
1.56
Marchetti 1980 (experimental)0.5
CLAY: KD correlated to K0
Theoretical
2004 Yu
Experimental
Marchetti (1980)
K0 =KD 0.47
Marchetti 1980 (experimental)1.5
0.6
SAND: KD sensitive to prestressing
Calibration chamber tests with prestressing cycles
Jamiolkowski & Lo Presti ISC'98 Atlanta
CC TEST N. 216 IN TICINO SAND
Kd increased 7 times the increase
of penetration resistance
Normally Consolidated Prestressed
SAME FINAL STATE OF STRESS, but after prestress
soil is stiffer and stronger Important impact on
design (settlements, liquefaction, compaction, ..)
Sensitivity to prestressing is valuable !
Stress History: effects on CPT and DMT
Effect of SH on
normalized Qc (CPT)
Lee 2011, Eng. Geology – CC in sand
Effect of SH
on KD (DMT)
Kd sensitive to Stress History
ED contains information on deformation
Theory of elasticity:
ED = elastic modulus of the horizontal load test performed
by the DMT membrane (D = 60mm, 1.1 mm expansion)
1.1 mm
D
M
T
ED= 34.7 (P1 -P0)
Gravesen S. "Elastic Semi-Infinite Medium bounded by a Rigid Wall with a Circular
Hole", Danmarks Tekniske Højskole, No. 11, Copenhagen, 1960, p. 110.
ED not directly usable corrections
(penetration,etc)
M obtained from ED using information on
soil type ID and stress history KD
ED (DMT modulus)
M
Constrained
Modulus
KD (stress history)
ID (soil type)
Definition of M (no ambiguity)
Vertical drained confined
tangent modulus (at 'vo)
M = Eoed = 1/mv = 'v / v (at 'vo)
M Comparison from DMT and from Oedometer
Norwegian Geotechnical Institute (1986).
"In Situ Site Investigation Techniques and
interpretation for offshore practice".
Report 40019-28 by S. Lacasse, Fig. 16a,
8 Sept 86
ONSOY Clay – NORWAY
Constrained Modulus M (Mpa)
Constrained Modulus M (Mpa)
Tokyo Bay Clay - JAPAN
Iwasaki K, Tsuchiya H., Sakai Y.,
Yamamoto Y. (1991) "Applicability of the
Marchetti Dilatometer Test to Soft
Ground in Japan", GEOCOAST '91,
Sept. 1991, Yokohama 1/6
Virginia - U.S.A.
Failmezger, 1999
Many publications & case histories of
good agreement between measured and
DMT-predicted settlements / moduli:
• McNulty & Harney (2014)
• Berisavijevic (2013)
• Vargas (2009)
• Bullock (2008)
• Monaco (2006)
• Lehane & Fahey (2004)
• Mayne (2001, 2004)
• Failmezger (1999, 2000, 2001)
• Crapps & Law Engineering (2001)
• Tice & Knott (2000)
• Woodward (1993)
• Iwasaki et al. (1991)
• Hayes (1990)
• Mayne & Frost (1988)
• Schmertmann 1986,1988)
• Steiner (1994)
• Leonards (1988)
• Lacasse and Lunne (1986)
• ..
• ..
Observed vs. predicted by DMTSilos on Danube Bank (Belgrade )
Silo founded on mat 100 m x 23 m, with qnet = 160 kPa
DMT Settlement prediction: 77 cm
Measured Settlement: 63 cm
DMT +22%
D. Berisavijevic, 2013
M at Sunshine Skyway Bridge
Tampa Bay – Florida
World record span for cablestayed post-tensioned concretebox girder concrete construction
(Schmertmann – Asce Civil Engineering – March 1988)
M from DMT 200 MPa ( 1000 DMT data points)M from laboratory: M 50 MPaM from observed settlements: M 240 MPa DMT good estimate of M
Observed vs. predicted by DMTDormitory Building 13 storeys (Atlanta - USA)
DMT
observed
Settlements profile: Measured vs DMT predicted
(Piedmont residual soil)
Mayne, 2005
SPT Settlement prediction: 46 mm
DMT Settlement prediction: 250 mm
Observed Settlement: 250 mm
SPT large error !!!
Possible reasons DMT good settlement predictions
Baligh & Scott (1975)
measure zone
measurezone
Stiffness Strength
2. Modulus by mini load test relates better
to modulus than penetration resistance
1. Wedge minimizes soil disturbance
Possible reasons DMT predicts well settlement
Mayne
(2001)
Soil is loaded at strain level for deformation analysis
Cu from OCR
Ladd SHANSEP 77 (SOA TOKYO)
Ladd: best Cu measurement not from TRX UU !!
Using m 0.8 (Ladd 1977) and (Cu/’v)NC 0.22 (Mesri 1975)
Cu
σ’vOC
=Cu
σ’vNC
OCR m OCR = 0.5 Kd
1.56
Cu = σ’v 0.5 Kd
1.25
0.22
best Cu from oed OCR Shansep
Cu comparisons from DMT and from other tests
Recife - Brazil
Coutinho et al., Atlanta ISC'98 Mekechuk J. (1983). "DMT Use on C.N.
Rail Line British Columbia",
First Int.Conf. on the Flat Dilatometer,
Edmonton, Canada, Feb 83, 50
Skeena Ontario – Canada Tokyo Bay Clay - JAPAN
Iwasaki K, Tsuchiya H., Sakai Y.,
Yamamoto Y. (1991) "Applicability of the
Marchetti Dilatometer Test to Soft
Ground in Japan", GEOCOAST '91,
Sept. 1991, Yokohama 1/6
A.G.I., 10th ECSMFE Firenze 1991
Vol. 1, p. 37
Cu at National Site FUCINO – ITALY
CPT: different profiles
according to Nc (=14-22)
Main SDMT applications
Settlements of shallow foundations
Compaction control
Liquefaction risk analysis
Slip surface detection in OC clay
Seismic design (Eurocode 8)
In situ G- decay curves
Laterally loaded piles (P-y curves)
Diaphragm walls (springs model)
FEM input parameters (es. Plaxis)
DMT for Compaction Control
Compaction of a loose sandfillResonant vibrocompaction technique
Van Impe, De Cock, Massarsch, Mengé - New Delhi (1994)
Dep
th(m
)
Many publications show that
DMT is ≈ twice more sensitive
than CPT to detect benefits of
compaction
(Schmertmann 1986, Jendeby 1992,
Pasqualini & Rosi 1993, Balachowsky
2015, …).
Jendeby (1992) measured in a loose sandfill
QC and MDMT before & after compaction
Before
MDMT increases about twice the increase of QC
After
Sensitivity to σh of DMT and CPT/SPT
Hughes & Robertson (Canadian Journal August 1985)
Arching effect
MDMT / QC before and after compaction
MDMT / QC before compaction 5-10
Jendeby 1992 Balachowski and Kurek 2015
MDMT / QC after compaction 12-24
Ratio M/Qc appears solid and site-independent, but further validation required
In many soil improvement jobs:
Monaco et al. 2014 Jnl GED 1, 2014
Tentative correlation
OCR = f (MDMT / qt)
OC
R
MDMT / qt
Qc ∼ DR
Lee 2011, Eng. Geology – CC in sand
KD ∼ (DR , OCR)
QC ∼ DR and KD ∼ (DR , OCR) ➨ OCR ∼ f (QC, KD)
3
OCR in SANDS: requires both CPT and DMT
DMT for Compaction Control - Palma Jumeirah DubaiE. Sharif (2015)
Aim of DMT tests: to confirm OC of
vibrocompaction, detected also by very
high Vs (400-500 m/s)
“..hydraulically filled silty fine calcareous
sand dredged from sea bed, underlain by
sedimentary rock of very weak
sandstone and siltstone..”
Floating Barge Limitations
Floating barge configuration is adequate
only nearshore (harbour, bay, ..)
Offshore impracticable:
horizontal anchoring difficult and time
consuming
waves ≥ 0.5 m
Seafloor Dilatometer version 1
WATERDEPTH 0 to 100 m - PUSH CAPACITY 5 ton
Max test depth is the depth penetrable with 5 ton push.
ballast(built locally)
Shipped byair (50 Kg)
4 bolts
Seafloor Dilatometer version 2 (2015)
Seafloor
ballast built locally ballast built locally
Support
anchored
to ballast
Seismic
Dilatometer
Seafloor DMT version 2 (2015)
2015 April 30th
6.5 ton ballast (steel plate)
5 ton push max (measured)
Medusa DMT
• Self-contained cableless DMT probe
• Pulsates indefinitely at programmable
fix periods: example 1-minute:
• DMT readings: 1/2 minute
• Penetration to next depth 1/2
minute
• DMT readings stored with time
• Probe depth recorded with time
• Data downloaded and synchronized at
end of test