Recent developments Flat dilatometer (DMT) & Seismic DMT (SDMT)

Slides:



Advertisements
Similar presentations
1 MAJOR FINDINGS OF THE PROJECT AND THEIR POSSIBLE INCLUSION IN EUROPEAN STANDARD -Major findings -Major findings suitable for inclusion in European Standard.
Advertisements

Educational Resource Library
AN INNOVATIVE METHOD TO EVALUATE DEGREE OF COMPACTION OF RIVER EMBANKMENTS USING CPT BARBARA COSANTI N. SQUEGLIA D.C.F. LO PRESTI University of Pisa –
The standard penetration test (SPT) is an in-situ dynamic penetration test designed to provide information on the geotechnical.
3-D Dynamic Base Shaking Model 2-D Static BNWF Pushover Model
Objectives Be able to use basic volume weight equations
Development of an In-Situ Test for Direct Evaluation of the Liquefaction Resistance of Soils K. H. Stokoe, II, E. M. Rathje and B.R. Cox University of.
8. Axial Capacity of Single Piles
ENGINEERING MATERIAL PROPERTIES (CE1303)
The Flat Dilatometer Test (DMT): and Recent Developments
Course : S0705 – Soil Mechanic
INTRODUCTION Session 1 – 2
Università degli Studi dell’Aquila Ing. Sara Amoroso SDMT Workshop and Field Demonstration Cesano 18 novembre 2011 Applicazioni alla progettazione geotecnica.
Pore-Pressure Generation During CPT Probe Advancement By Michael Fitzgerald.
Chapter (1) Geotechnical Properties of Soil
Silvano Marchetti University of L'Aquila, Italy Flat dilatometer (DMT) & Seismic DMT (SDMT) 1 Frontespizio University of PISA.
Fawad S. Niazi Geosystems Engineering Division Civil & Environmental Engineering Georgia Institute of Technology April 27, 2010 Spatial Variability of.
“LIQUEFACTION” Prepared By: Husni M. Awwad Talal Z. Zammar
  AN-najah National University Faculty of Engineering Civil engineering Department Prepared by: Eng. Imad A. F. Jarara’h. Submitted.
Use of SDMT results for engineering applications
CE 486 DEEP COMPACTION Name : Ali Hamood Al-teeb. ID :
Bearing Capacity Theory
7. Soil Compaction (Das, chapter 6)
Session 17 – 18 PILE FOUNDATIONS
SOIL, GEOTECHNICAL ENGINEERING AND FOUNDATION ENGINEERING
3 rd International Conference on the Flat Dilatometer (DMT) Rome 15 th -17 th June
Direct Shear Test CEP 701 PG Lab.
Analysis of results and parameters derived from SDMT
1 Interpretation and Visualization of Model Test Data for Slope Failure in Liquefying Soil Bruce L. Kutter Erik J. Malvick R. Kulasingam Ross Boulanger.
A Study on Liquefaction Evaluation Using Shear Wave Velocity for Gravelly Sand Deposits Ping-Sien Lin, National Chung-Hsing University Fu-Sheng Chen, China.
CIVIL ENGINEERING. Civil engineering work includes: dams embankments motorways bridges buildings cuttings quarries tunnels mines All these need to take.
BEARING CAPACITY OF SOIL Session 3 – 4
SOIL MECHANICS AND FOUNDATION ENGINEERING-II (CE 311)
CVE 308 SOIL MECHANICS ENGR S.O ODUNFA DEPT. OF CIVIL ENGINEERING UNIVERSITY OF AGRICULTURE, ABEOKUTA.
SOIL MECHANICS AND FOUNDATION ENGINEERING-II (CE 311)
Field characterization of problematic earthfills, by DMT. A case history Nuno Cruz - MOTA-ENGIL; Universidade de Aveiro, Portugal Isabel Caspurro - Estradas.
GROUND IMPROVEMENT PRINCIPLES OF COMPACTION. A good foundation has a safe and economic design with the following properties: 1.Have adequate shearing.
1 ROAD & BRIDGE RESEARCH INSTITUTE WARSAW Juliusz Cieśla ASSESSSMENT OF PRESTRESSING FORCE IN PRESTRESSED CONCRETE BRIDGE SPANS.
Silvano Marchetti University of L'Aquila, Italy Flat dilatometer (DMT). Deformation parameters, compaction, liquefaction Frontespizio.
Silvano Marchetti University of L'Aquila, Italy Flat dilatometer (DMT). Seismic DMT. 1 Frontespizio Australian Geomechanics Society.
Stats Methods at IC Lecture 3: Regression.
The Engineering of Foundations
G-γ stiffness degradation curves by seismic dilatometer (SDMT)
FE: Geotechnical Engineering
Some 2015 Updates to the TC16 DMT Report 2001
Piezocone Penetration
QuakeCoRE Project Update
Presented By: Sanku Konai
SOIL, GEOTECHNICAL ENGINEERING AND FOUNDATION ENGINEERING
Concept of Test Validity
Methodologies for Geotechnical Characterization in Railways in Operation. An Experience. Nuno Cruz, Eduardo Fortunato, Francisco Asseiceiro, Jorge Cruz,
PREPARED BY SK SOHEL, CE-3RD YEAR GUIDED BY JAYASHREE SENGUPTA
Short Course on the DMT Paola Monaco 2nd International Conference on
The Calibration Process
Pile Group
Reinforced earth structures
on soft clay using finite element method Road & Highway Engineering
WHAT IS LIQUEFACTION.
S S SUBMITTED BY:- CHARU BHARDWAJ civil engineering
5. WEIGHT VOLUME RELATIONSHIPS
Geotechnical Engineering II
Structural Design of Highway
Christopher R. McGann, Ph.D. Student University of Washington
GEOTECHNICAL ENGINEERING – I B.E. IVTH SEMESTER
Preliminary design of foundation for HEPS
Classification, Engineering Properties & Consolidation Methods
Scott McFarlane & Richard Merifield
Roger A. Failmezger, P.E., F. ASCE, D. GE
Graduation Project Bracing system for deep excavation.
lectures Notes on: Soil Mechanics
Presentation transcript:

Recent developments Flat dilatometer (DMT) & Seismic DMT (SDMT) University of PISA – DESTEK Oct. 9 th 2014 Workshop on Penetration Testing Frontespizio Flat dilatometer (DMT) & Seismic DMT (SDMT) Recent developments Silvano Marchetti University of L'Aquila, Italy silvano@marchetti-dmt.it 1

DMT results KD = 2  NC clay ID  M Cu   KD  soil type or Stress History Index KD = 2  NC clay  amplified Ko ID  M Cu   KD  soil type (clay, silt, sand) common use shape similar to OCR helps understand history of deposit 1-D modulus @ ’vo . Treat as if obtained by oed

Seismic Dilatometer

SDMT results repeatability ≈ 1-2% SHEAR WAVE VELOCITY GO= ρ Vs2 Vs (m/s) mechanical DMT Seismic DMT (Recommended graphical format – no just po p1)

Main SDMT applications (details  papers) Settlements of shallow foundations Liquefability evaluation Compaction control Detecting slip surfaces in OC clay Laterally loaded piles Diaphragm walls : “springs” for design FEM input parameters In situ G- decay curves Seismic design (NTC08, Eurocode 8) Have in common : need of Stress History (by Kd) 5

Lee 2011, Eng. Geology  30 CC in sand Diagrams compare sensitivity of CPT-DMT to Stress History Lee 2011, Eng. Geology  30 CC in sand Box 1. Effect of SH on Qc Box 2. Effect of SH on Kd OCR = 1,2,4,8 CPT DMT Kd ++ reactive than Qc to Stress History For a given Qcn : can be many Kd, depending on SH Kd distinguish sands with SH / no SH. Qcn  much less.

(3/7) Two sites : same Qc , but different KD. Site 2 much “stronger” (higher SH)  settlement and liquefaction.

Many formulae OCR-Qc proposed, even relatively complex. Given the scarce sensitivity of Qc to OCR, is it possible to estimate OCR from CPT ? Effect of OCR on Qc Many formulae OCR-Qc proposed, even relatively complex. CPT No mathematics, plaxis, statistics, FEM… can replace low degree of correlation

Similarly higher sensitivity of Kd to SH & aging observed by Jamiolkowski (ISC'98 Atlanta) They applied prestraining cycles in calibration chamber. Found : KD (DMT) 3 to 7 times more sensitive to AGING than penetration resistance CC TEST N. 216 IN TICINO SAND PRESTRAINING CYCLES simulate AGING (grain slippage) KD + 20 % qD + 3 %

that DMT MORE REACTIVE TO STRESS HISTORY confirmed in the field … Q c BEFORE AFTER Jendeby 92 Measured in a loose sandfill Qc & Mdmt before-after compaction NC : M/Qc  5-12 OC : M/Qc  12-24 Mdmt v. effective in reflecting benefits of compaction Schmertmann 1988 : Since aim of compaction is reduce settlements :  More logic specs in terms of M instead of Dr (Dr wrong target and Dr correlations v. uncertain)

Can estimate OCR based on ratio =M/Qc Estimate OCR in sand. Qc or Mdmt alone : not sufficient (multiparameter). Need both, one sensitive to SH, other less sensitive Can estimate OCR based on ratio =M/Qc (Monaco et al. Asce Jan 2014) If  = M/Qc  5-12  NC If  = M/Qc  12-24  OC Principle behind : To convert Qc to M (by M=Qc) we need  = 4 to 20 f(OCR) (?) If we know = M/Qc, can get an idea of OCR Difficult enough with 2 parameters (CPT,DMT) … …once having OCR : Ko=Ko,nc (OCR)m

MDMT before-after compaction COMPACTION ( applying SH) produces a MDMT% increase  twice the Qc% increase Schmertmann (1986) DYNAMIC COMPACTION of sand site. MDMT % increase  twice % increase in Qc. Jendeby (1992) monitored DEEP COMPACTION in a sand fill by VIBROWING. MDMT increase  twice increase in qc. Pasqualini & Rosi (1993) VIBROFLOTATION job : "DMT clearly detected improvement even in layers where benefits were undetected by CPT". Ghent group (1993) before‑after CPTs DMTs to evaluate effects (h , Dr) by PILE (Atlas) INSTALLATION "DMTs before-after installation demonstrate more clearly [than CPT] beneficial effects of Atlas installation". MDMT before-after compaction bar …hence Mdmt effective in reflecting benefits of compaction Resonant vibro-compaction technique Van Impe, De Cock, Massarsch, Mengé, New Delhi (1994)

(Multi parameter – both DMT) ….conclusion : good sensitivity of KD to Stress History … (SH : OCR overburden, aging, any factor better grain interlocking) Sensitivity to SH important : (1) not many SH tools (2) SH important for settlements and liquefaction Importance of SH to predict Settlements Jamiolkowski (Isopt-1,‘88,1) : “without Stress History, impossible to select reliable E (or M) from Qc” (also Terzaghi, Leonards, Schmertmann…) Yoshimi (1975) “… the NC sand specimens were six times more compressible than the prestressed sand” hence imperative SH to characterize compressibility of sand Application #1 DMT : predict settlements (operative modulus) MDMT= ED x Rm(Kd, Id) (combines ED with Stress History) (Multi parameter – both DMT)

Settlement predictions by DMT In general classic Terzaghi 1-D (even in 3-D (Poulos : modulus, not formula !! ) by Boussinesq Accuracy of DMT-predicted settlements : confirmed by a large number case histories in the last decades Cruz (2010), 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 (1986)…………… > 40 papers at ISC4-Brazil 2012

Silos on Danube's Bank (Belgrado) SETTLEMENTS Measured 63 cm DMTpredicted 77 cm (+22%) (D. Berisavijevic 2013)

M at Sunshine Skyway Bridge, Tampa Bay – Florida (Schmertmann – Asce Civil Engng – March 1988) World record span for cable stayed post-tensioned concrete box girder concrete construction DMT results: M  200 MPa (1000 DMT test points) Laboratory results: M  50 MPa From observed Settlements: M  240 MPa  DMT = good evaluation of constrained modulus

CAPE HATTERAS LIGHT HOUSE : was moved from its original location to protect it from a receding coastline. Selected as one of ASCE outstanding civil engineering achievement 2000 DMTs : executed by Law Engineering Allan Tice, Assistant Vice President : "DMT data provided reliable settlement estimates in the predominately sandy soils along the path and at the final destination of the light house”.

Lacasse & Lunne (1986) of NGI compare observed vs DMT-predicted settlements of a silos on sand in Norway.

Paul Mayne Prof. at Georgia Tech (2005) compares observed vs DMT-predicted settlements of a building in residual soil in Atlanta

Sliding Micrometers installed every meter Agreement of settlements not sufficient (might be compensating errors). Must check moduli at each depth. M by DMT vs. M back-calculated from LOCAL vertical strains measured under Treporti full-scale test embankment (Italy) Sliding Micrometers installed every meter

Possible reasons DMT predicts well settlement Wedges deform soil << cones Modulus by mini load test relates better to modulus than to penetr. resistance Availability of Stress History parameter Kd. (DMT is a 2- parameter test. Fundamental to have both: Ed and Kd) The soil is loaded at a lower, more appropriate, strain level Stiffnes  Strength  Need moduli, not strength !

Predicting settlements is application # 1 of DMT. Settlements obviously important, a key section in all Geotechnical Reports De Vincenzi (2001) “More and more, today, the factor controlling the design is not the bearing capacity, but the necessity of limiting settlements”

M can also be predicted as M=  Qc Problem is :  depends on SH (OCR) – missing info. Who will tell us OCR to select the curve and select  ? Calibration chamber :  = 2.5 to 25 ! Jamiolkowski concludes : "without Stress History impossible to select reliable E (or M) from Qc“ (Isopt-1, '88, Vol. 1, p.263) Powell (BRE) “The scarce ability to predict modulus is a well known weakness of CPT”. OCR??? Qc cannot be used twice : (1) as denominator In E/Qc (2) As parameter to select which curve

Liquefiability evaluations also in need of info on Stress History / Aging Jamiolkowski et al. (S. Francisco 1985) "Reliable predictions of sand liquefiability...require…some new in situ device [other than CPT or SPT], more sensitive to effects of past STRESS-STRAIN HISTORIES” Leon et al. (ASCE GGE 2006) South Carolina sands. “Ignoring AGING and evaluating CRR from in situ tests insensitive to aging (SPT, CPT, VS) underestimated CRR by a large 60 %” Salgado et al. (Jnl Asce 1997). “OCR increases liquefaction resistance CRR, but changes negligibly Qcn”

Ignoring Stress History  omit a primary parameter Ignoring Stress History  omit a primary parameter. Consequence : CRR predicted by CPT (insensitive to SH) uncertain Is reason of v. cautious recommendations on CRR(CPT) : Robertson & Wride (1998)  CRR by CPT adequate for low-risk projects. For high-risk : estimate CRR by more than one method Youd & Idriss 2001 (NCEER Workshops )  use 2 or more tests for a more reliable evaluation of CRR Idriss & Boulanger (2004)  the allure of relying on a single approach (e.g. CPT-only) should be avoided … difficult situation considering…

Soil Liquefaction due to Earthquake Latest Research TREND in 2014 onwards (Extract from Geo-Congress, ASCE 2014 Panel Discussion) Panelists: Prof. Idriss, Prof. Boulanger, Prof. Robertson, Prof. Cetin, Prof. Finn, Prof. Green, Prof. Stokoe, Prof. Mayne No laboratory tests are suitable for liquefaction estimation. Only suitable field tests MUST be used. (Terzaghi Lecture-2011)

Why expect a stricter correlation and a more accurate CRR if CRR is predicted by Kd

Estimating CRR using KD Many curves developed in the last 30 years. Curves are converging to a narrow stripe Latest CRR(Kd) : Robertson (2012) : CRR = 93 (0.025 KD)3 + 0.08

ESTIMATING CRR As today : 2 CRR estimates, from two separate one-to-one correlations One estimate from Qc (Idriss & Boulanger 2006) One estimate from Kd (Robertson 2012) Recent research (2015) has produced a combined CRR-Qcn-Kd correlation. Provides estimates of CRR based at the same time on Qc & Kd. Note. When SH (Kd) is high, CRR is higher than predicted by baseline.

SEAFLOOR DILATOMETER WATERDEPTH 0 to 100 m (nearshore jobs) PUSH CAPACITY 7 ton Max test depth is the depth penetrable with 7 ton push. Shipped by air (50 Kg) 4 bolts 7 ton ballast (built locally)

Ballast (iron blocs) are put into container

Seafloor DMT lifted

Seafloor DMT lowered in water : rods pre-charged

First Seafloor DMT test: 13 June 2014

Krabbenhoff (Delhi 2014) : FEM programs like mob phones Krabbenhoff (Delhi 2014) : FEM programs like mob phones. We just want to talk, not bothered by complexity of the wires. In sand (lab no possible) : Designer assigns just the raw data (inequivocally measured) e.g. CPT & DMT  Then FEM gives the solution. Dream for practitioner. Separates responsibility. Practicioners amateurs vs model specialists, profes- sionals payed for running FEM avoiding pitfalls. Assign to each region : Strength Stress History Stiffness Soil type Qc Kd Ed Id

CPT (1) & DMT(2) : 3 indep. responses This idea of FEM possibly oversimplified. But main message is not FEM, is input (sands) Moving lab  in situ OK. But in lab : Strength, Stiffness, Stress History … Can we just input strength (Qc) without Stress History and Stiffness ? Need multiple (significant) in situ soil responses). 3 unknowns  3 Eqns. CPT (1) & DMT(2) : 3 indep. responses Assign to each region : Rupture Stress History Stiffness Soil type Qc Kd Ed Id Same for evaluating liquefaction Can we do with just Qc, without SH and Stiffness ? Same for evaluating porosity n= f(Qc) does not work Try n= f(Qc, Kd, Ed, Id) ---------------------------------------- As material index is indicated : Id (DMT) or FR(CPT) ? Id is believed having more solid soil paternity

Repeatibility v. good v. bad CPT in sand is essentially a one-parameter test (or 1.5?). Sleeve friction fs not very reliable Eg. Frost (2001) "Underuse" of fs is related to common sentiment that fs is unreliable… Repeatibility v. good v. bad Lunne (CPT10) had CPT done by 4 different well-qualified firms. Qc was found repeatable, fs highly variable. “with the present large variations in fs, impossible to utilize this measure…for soil parameters” Reason not just instrumental ! fs not so “fundamental”. fs highly unstable, being what is left after an enormous stress reduction – in a situation of arching, with a stiff soil ring surrounding the sleeve. Moreover : h sleeve is transformed into vert force, via Øsoil-steel

Sensitivity to h of fs and KD fs highly unstable, being what is left after an enormous stress reduction CIRCULAR PROBE FLAT 38

fs & KD both reflect h against probe Mc Connell 2014 : fs & KD much in common fs & KD both reflect h against probe KD measures h directly (i.e. po) fs indirectly, transforming h to Fvertical Thus fs  an attenuated KD , weaker and much less stable and direct. And repeatibility... 39

(Robertson Jnl Asce Nov 2009) CPT-DMT inter correlations Robertson has formulae for estimating DMT from CPT. V. dispersed in particular Kd from Qcn. Expectable : no way reconstructing Kd sensitive to Stress History from insensitive Qcn. Some researchers study opposite direction : Qc from DMT. Should have +success. Should be easier to predict one parameter from two than viceversa. DMT a genuine two parameter test. In that DMT appears a +informative test.

Detecting slip surfaces in clay slopes (look for Kd  2) Method permits to verify if an OC clay slope contains active or quiescent slip surfaces(Totani et al. 1997) Useful to know : Old slip surface may reactivate ! – Øresidual

Validation of DMT-KD method LANDSLIDE "FILIPPONE" (Chieti) DOCUMENTED SLIP SURFACE (inclinometers) LANDSLIDE "CAVE VECCHIE" (S. Barbara) DOCUMENTED SLIP SURFACE (inclinometers) active: Kd=2 quiescent: Kd=2

Kd  2 detects both active (moving) and quiescent slip surfaces active: Kd=2 quiescent: Kd=2 active: Kd=2 quiescent: Kd=2

OTHER APPLICATIONS

Totani, Calabrese, Monaco (1998) Dissipation test in cohesive soils. Estimate coefficient consolidation & permeability From u(t) in a singular highly disturbed point Time (min) σ h (kPa) Totani, Calabrese, Monaco (1998) From a mini embankment. Larger volume less disturbed

LATERALLY LOADED PILES DMT for P-y CURVES for LATERALLY LOADED PILES Robertson et al. (1987) Marchetti et al. (1991) 2 methods recommended for deriving P-y curves for laterally loaded piles from DMT (single pile, 1st time monotonic loading) Figure shows that the 2 methods provide similar predictions, both in good agreement with observed full-scale pile behaviour

DMT for coeff. subgrade reaction Kh for DIAPHRAGM WALLS Monaco & Marchetti (2004 – ISC'2 Porto) Tentative correlation for deriving the coefficient of subgrade reaction Kh for design of multi-propped diaphragm walls from MDMT Indications on how to select input moduli for FEM analyses (PLAXIS Hardening Soil model) based on MDMT

Subgrade compaction control Bangladesh Subgrade Compaction Case History 90 km Road Rehabilitation Project 10 cm interval MDMT acceptance profile (max M always found at 25-26 cm) An acceptance MDMT profile was established and used as alternative/fast acceptance tool for quality control of subgrade compaction, with only occasional verifications by originally specified methods (Proctor, CBR, plate)

Website: www.marchetti-dmt.it

CONCLUDING REMARKS (1/7) Direct push CPT and DMT are increasingly recognized as fast and convenient tools for everyday investigations. DMT’s KD has the peculiarity of being sensitive to Stress History, scarcely felt by other tools. Sensitivity to SH is fundamental for good predictions of settlements and of CRR.

PREDICTING SETTLEMENTS (2/7) PREDICTING SETTLEMENTS Countless researchers : without Stress History it is impossible to predict modulus from CPT or SPT. A large number of comparisons confirm DMT predicts well settlement. With DMT no  (2 to 20) to guess in M= Qc. DMT correlations guide without subjective choices to M, taking into account soil type (Id) and Stress History (Kd).

KD may lead to a more economical design (3/7) KD may lead to a more economical design KD reflects benefits of Stress History on settlement and liquefaction. SH scarcely sensed by other tools, which ignore SH  benefits are wasted. Site 2 “stronger” despite the same Qc

“CPT costs less than DMT. Is CPT therefore preferable ?” (4/7) “CPT costs less than DMT. Is CPT therefore preferable ?” As to pure cost CPT preferable. But info / cost A CPT investigation costs less, but does not provide accurate predictions of settlements. Been : State of Art at CPT 2010 Los Angeles : CPT can easily mislead in terms of soil type, strength and particularly modulus”. Robertson (1986) : Prediction of modulus from Qc can be rather poor, especially for OC soils, with a large potential error.

SETTLEMENTS ARE IMPORTANT (5/7) SETTLEMENTS ARE IMPORTANT If we do CPT only : may save in investigation. But if we spend a bit more doing DMT, predict more accurate settlements, save in design of foundation, where the $ is. Settlements can have important $ consequences (piles/ shallow foundations…). Important jobs cannot do w/o Accurate Settlements  more economical design. Info=$.

When considering costs : into account (6/7) When considering costs : into account With DMT "not many things can go wrong“ No electronics, no temperature effects, no vacuum pump, no saturation-deairing, no glycerin, no area correction… start testing immediately … … uncertain data, when present : big cost. Designer looses time choosing parameters, becomes nervous, increases Fs  overdesign. DMT easy to run, short training time (  3 hours) Any operator gets same results. In remote regions : easy to instruct a local technician. No need to leave a highly skilled (costly) operator.

CONCLUDING REMARK (7/7) Stress History is sometimes considered a gourmet property, as not directly used in calculations as c’ Ø’ Cu … Or of academic interest, to separate elastic/ plastic behaviour… Not so. SH makes the soil much stronger. It is a substantial $ resource. Ignoring SH when present  wasting $. BUT must be able to distinguish when SH is present / not. Not easily done by penetration tests. -------------------------- TREND today  Multiparameter approach better than one-to-one correlations. Soil has many unknowns : need multiple responses

3rd International Conference on the Flat Dilatometer (DMT) Rome 14th-16th June 2015

Highlights of the conference include www.dmt15.com Highlights of the conference include Prof. Roger Frank (ISSMGE president) Welcome speech Prof. J. Schmertmann’s dinner talk Prof. M. Jamiolkowski: use of SDMT in the Zelazny Most dam in Poland Prof. F. Schnaid: use of DMT and SDMT in tailings dam Sofar 120 abstracts from 32 Countries

Venue is in the town center www.dmt15.com Venue is in the town center

Rome touristic attractions www.dmt15.com Rome touristic attractions

St. Peters and Pope Francesco www.dmt15.com St. Peters and Pope Francesco

Difficult booking ( Hotel, Flights ) expected in June 2015: www.dmt15.com Difficult booking ( Hotel, Flights ) expected in June 2015: June is high season High popularity of the Pope EXPO 2015 (Milan-Rome)