CONTRIBUTION OF THE COARSE AGGREGATE ...Introduction - Rheology influences in concrete 07.03.2018...

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CONTRIBUTION OF THE COARSE AGGREGATE

FRACTION TO RHEOLOGY –

EFFECTS OF FLOW COEFFICIENT, PARTICLE SIZE

DISTRIBUTION, AND VOLUME FRACTION

Wolfram Schmidt, Alejandra Ramírez Caro,

Regine Sojref, Berta Mota, Toni Fenger, Charles Osei

07.03.2018

Introduction - Rheology influences in concrete

07.03.2018Contribution of the coarse aggregates to rheology - effects of flow coefficient, particle size distribution, and volume fraction | wolfram.schmidt@bam.de

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• Ion content and strength• Surface chemistry and charges• Polymer sizes and structure• Selective adsorption• Competitive adsorption• Different particle charges• Hydration phases• Morphology• Powder properties• Different particle sizes• Solid volume fraction• Interaction of particle sizes• PSD of finest particles• PSD of coarser particles

nm

µm

mm

cm

Introduction – Relevance of coarse aggregates

07.03.2018Contribution of the coarse aggregates to rheology - effects of flow coefficient, particle size distribution, and volume fraction | wolfram.schmidt@bam.de

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• With increasingflowability and increasing strength, the relevance of thefiner fractionsincreases.

• However, 96% of all ready mixed concretetypes are normal strength and normal consistency.(BTB 2016)

• We can effectively manipulate the rheology on nm to mm scale.

• We would not try to significantly control rheology based on mm scale.

• But effects on mm and cm scale overlap with paste effects.

07.03.2018Contribution of the coarse aggregates to rheology - effects of flow coefficient, particle size distribution, and volume fraction | wolfram.schmidt@bam.de

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Introduction – Relevance of coarse aggregates

Introduction – Challenges

07.03.2018Contribution of the coarse aggregates to rheology - effects of flow coefficient, particle size distribution, and volume fraction | wolfram.schmidt@bam.de

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Different ideas have been developed,

– Grading curves (e.g. Andreasen, Funk & Dinger)

– Modelling (e.g. De Larrard, Stroeven)

But grading curves cannot represent the complexreality,

And real aggregates seldomly behave like modellised(and mostly uni-sized, often round) particles.

Introduction - Motivation

07.03.2018Contribution of the coarse aggregates to rheology - effects of flow coefficient, particle size distribution, and volume fraction | wolfram.schmidt@bam.de

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Is there a simple experimental parameter thatcan predict the „rheology“ of aggregates?

Can the flow coefficient provide adequateinformation?

EN 933-6 Tests for geometrical properties of aggregates - Part 6: Assessment of surface characteristics - Flow coefficient of aggregates,Beuth Verlag GmbH, Berlin, Juli 2014

www.bam.de

EXPERIMENTAL SETUP

Experimental – aggregate properties

07.03.2018Contribution of the coarse aggregates to rheology - effects of flow coefficient, particle size distribution, and volume fraction | wolfram.schmidt@bam.de

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Quartzitic aggregates

Three fractions: 2/4; 4/8; 8/16

Density ~ 2650 kg/m³

0

10

20

30

40

50

60

70

80

90

100

1 2 4 8 16

Mesh m

inus [

%]

Sieve diameter [mm]

2/4

8/16

4/8

Experimental – investigated variations

07.03.2018Contribution of the coarse aggregates to rheology - effects of flow coefficient, particle size distribution, and volume fraction | wolfram.schmidt@bam.de

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2/4 4/8

2/4 8/16

4/8 8/16

100:0 80:20 60:40 40:60 20:80 0:100

07.03.2018Contribution of the coarse aggregates to rheology - effects of flow coefficient, particle size distribution, and volume fraction | wolfram.schmidt@bam.de

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Experimental – investigated variations

Experimental – grading curves

07.03.2018Contribution of the coarse aggregates to rheology - effects of flow coefficient, particle size distribution, and volume fraction | wolfram.schmidt@bam.de

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Experimental – flow coefficient

07.03.2018Contribution of the coarse aggregates to rheology - effects of flow coefficient, particle size distribution, and volume fraction | wolfram.schmidt@bam.de

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1. Determine funnel opening

2. Place beaker and balance

3. Fill aggregates in plastic pipe

4. Start vibrating

5. Open funnel

6. At 1000 g, start stop watch

7. Take time, when balance shows

m = 1000 ⋅ (1 + 7 ⋅ rp/2.70)

8. For standard aggregates, the flow

coefficient is the time that

~7 kg or ~2.6 l take to run out.

Experimental – flow coefficient

07.03.2018Contribution of the coarse aggregates to rheology - effects of flow coefficient, particle size distribution, and volume fraction | wolfram.schmidt@bam.de

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Each sample was tested three times from the same

batch.

Each batch was repeated individually for three times.

3 x 3 x 15 = 135 repetitions

The flow coefficient was determined as the arithmetic

mean of 9 measurements.

Experimental – loose bulk density

07.03.2018Contribution of the coarse aggregates to rheology - effects of flow coefficient, particle size distribution, and volume fraction | wolfram.schmidt@bam.de

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EN 1097-3:199 Tests for mechanical properties of aggregates. Part 3: Determination of loose bulk density and voids

Experimental – limestone filler paste

07.03.2018Contribution of the coarse aggregates to rheology - effects of flow coefficient, particle size distribution, and volume fraction | wolfram.schmidt@bam.de

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0%

20%

40%

60%

80%

100%

Reference SCC Reference

mortar mix

Limestone

filler based

paste

Water

Water

Water

LS Filler

LS Filler

LS Filler

Cement Cement

Cement LS Filler

Air Water

Fine sand (< 2mm) Coarse sand and aggregates (2mm - 16mm)

Coarse

sand &

aggre-

gates

Fine

sand

Fine

sand

Similarrheology

!

No fine sand in the paste toavoid any

interactions!

Experimental – limestone filler paste

07.03.2018Contribution of the coarse aggregates to rheology - effects of flow coefficient, particle size distribution, and volume fraction | wolfram.schmidt@bam.de

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0%

20%

40%

60%

80%

100%

Reference SCC Reference

mortar mix

Limestone

filler based

paste

Water

Water

Water

LS Filler

LS Filler

LS Filler

Cement Cement

Cement LS Filler

Air Water

Fine sand (< 2mm) Coarse sand and aggregates (2mm - 16mm)

Coarse

sand &

aggre-

gates

Fine

sand

Fine

sand

Similarrheology

07.03.2018Contribution of the coarse aggregates to rheology - effects of flow coefficient, particle size distribution, and volume fraction | wolfram.schmidt@bam.de

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Influence of the admixture combination:

Experimental – limestone filler paste

07.03.2018Contribution of the coarse aggregates to rheology - effects of flow coefficient, particle size distribution, and volume fraction | wolfram.schmidt@bam.de

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Experimental – limestone filler paste

07.03.2018Contribution of the coarse aggregates to rheology - effects of flow coefficient, particle size distribution, and volume fraction | wolfram.schmidt@bam.de

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Influence of the admixture combination:

Experimental – limestone filler paste

07.03.2018Contribution of the coarse aggregates to rheology - effects of flow coefficient, particle size distribution, and volume fraction | wolfram.schmidt@bam.de

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100% LS paste

88% LS paste

12% coarse 78% LS paste

22% coarse

59% LS paste

41% coarse

70% LS paste

30% coarse 64% LS paste

36% coarse

Experimental – limestone filler “concrete”

Experimental – rheometric investigations

07.03.2018Contribution of the coarse aggregates to rheology - effects of flow coefficient, particle size distribution, and volume fraction | wolfram.schmidt@bam.de

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Rheometer 4-SCC

Bingham evaluation of measurement data

Only qualitative results possible:

• Yield stress related value: [A]

• Plastic viscosity related value: [A⋅s]

www.bam.de

RESULTS

07.03.2018Contribution of the coarse aggregates to rheology - effects of flow coefficient, particle size distribution, and volume fraction | wolfram.schmidt@bam.de

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70

75

80

85

90

95

100

100/0 80/20 60/40 40/60 20/80 0/100

Flo

w c

oeff

icie

nt [s

]

Increasing content of coarser fraction

2/4-4/8 4/8-8/16

Fineraggregates

cause higherflow coefficients

Results – flow coefficient

07.03.2018Contribution of the coarse aggregates to rheology - effects of flow coefficient, particle size distribution, and volume fraction | wolfram.schmidt@bam.de

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70

75

80

85

90

95

100

100/0 80/20 60/40 40/60 20/80 0/100

Flo

w c

oeff

icie

nt [s

]

Increasing content of coarser fraction

2/4-4/8 4/8-8/16

Range = 7.2 s

Range = 8.1 s

Results – flow coefficient

The variation ranges aresimilar for:

fine medium

and medium coarse

70

75

80

85

90

95

100

100/0 80/20 60/40 40/60 20/80 0/100

Flo

w c

oeff

icie

nt [s

]

Increasing content of coarser fraction

2/4-4/8 2/4-8/16 4/8-8/16

07.03.2018Contribution of the coarse aggregates to rheology - effects of flow coefficient, particle size distribution, and volume fraction | wolfram.schmidt@bam.de

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The variation ranges aresimilar for:

fine medium

and medium coarse

but significantly wider for:

fine coarse

Range = 23.4 s

Results – flow coefficient

70

75

80

85

90

95

100

100/0 80/20 60/40 40/60 20/80 0/100

Flo

w c

oeff

icie

nt [s

]

Increasing content of coarser fraction

2/4-4/8 2/4-8/16 4/8-8/16

07.03.2018Contribution of the coarse aggregates to rheology - effects of flow coefficient, particle size distribution, and volume fraction | wolfram.schmidt@bam.de

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Increasing coarseaggregate contentsdecrease the flow

coefficient.

A minimum can be foundbetween the two

fractions.

Results – flow coefficient

07.03.2018Contribution of the coarse aggregates to rheology - effects of flow coefficient, particle size distribution, and volume fraction | wolfram.schmidt@bam.de

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1350

1400

1450

1500

1550

1600

100/0 80/20 60/40 40/60 20/80 0/100

Loose b

ulk

density [

kg/m

³]

Increasing content of coarser fraction

2/4-4/8 2/4-8/16 4/8-8/16

Ideal packing was achieved for 40:60 and 60:40 of two fractions.

Better packing densitywhen the smaller fraction

is finer sand.

Best packing possiblewith largest gap between

coarse and fineaggregate.

Results – loose bulk density

Results – loose bulk density

07.03.2018Contribution of the coarse aggregates to rheology - effects of flow coefficient, particle size distribution, and volume fraction | wolfram.schmidt@bam.de

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1350

1400

1450

1500

1550

1600

100/0 80/20 60/40 40/60 20/80 0/100

Loose b

ulk

density [

kg/m

³]

Increasing content of coarser fraction

2/4-4/8 2/4-8/16 4/8-8/16

70

75

80

85

90

95

100

100/0 80/20 60/40 40/60 20/80 0/100

Flo

w c

oeff

icie

nt

[s]

Increasing content of coarser fraction

2/4-4/8 2/4-8/16 4/8-8/16

70

75

80

85

90

95

100

1300 1350 1400 1450 1500 1550 1600

Flo

w c

oeff

icie

nt

Loose bulk density [kg/m³]

'2/4 - 4/8

'4/8 - 8/16

'2/4 - 8/16Correlation?

No correlation!

Results – yield stress

07.03.2018Contribution of the coarse aggregates to rheology - effects of flow coefficient, particle size distribution, and volume fraction | wolfram.schmidt@bam.de

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4/8 – 8/162/4 – 8/162/4 – 4/8

Aggr.

vol. f

raction

No similarity between theblends.

Minimum always betweenthe single fractions.

Minimum always withhigher coarse volume.

0

1

2

3

4

5

6

7

8

9

10

H-V

isco

sity

aggr

./

H-V

isco

sity

past

e

12% by vol. 22% by vol. 30% by vol.

07.03.2018Contribution of the coarse aggregates to rheology - effects of flow coefficient, particle size distribution, and volume fraction | wolfram.schmidt@bam.de

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4/8 – 8/162/4 – 8/162/4 – 4/8

Aggr.

vol. f

raction

Lowest viscosity alwayswith smallest aggregate

fraction.

No big effect fromsmall to medium

Significant effect withcoarsest fraction.

Results – viscosity

Results – rheology

07.03.2018Contribution of the coarse aggregates to rheology - effects of flow coefficient, particle size distribution, and volume fraction | wolfram.schmidt@bam.de

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0

1

2

3

4

5

6

7

8

9

10

H-V

isco

sity

aggr

./

H-V

isco

sity

past

e

12% by vol. 22% by vol. 30% by vol.

Regardless of the volume fraction, theinfluence of the aggregates was always

particular.

This means: Already at smallest volume fractions, the

aggregates affect the rheology.

And: The aggregate volume fraction is a multiplier of the particular effect.

Results – yield stress vs. flow coefficient

07.03.2018Contribution of the coarse aggregates to rheology - effects of flow coefficient, particle size distribution, and volume fraction | wolfram.schmidt@bam.de

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50

55

60

65

70

75

80

85

90

95

100

Flo

w c

oef

fici

ent

[s]

Yield stress Flow coefficient

0

1

2

3

4

5

6

7

8

9

10

H-V

isco

sity

aggr

./

H-V

isco

sity

past

e

12% by vol. 22% by vol. 30% by vol.

Results – viscosity vs. flow coefficient

07.03.2018Contribution of the coarse aggregates to rheology - effects of flow coefficient, particle size distribution, and volume fraction | wolfram.schmidt@bam.de

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50

55

60

65

70

75

80

85

90

95

100

Flo

w c

oef

fici

ent

[s]

Plastic viscosity Flow coefficient

?

Results – lowest yield stress PSD

07.03.2018Contribution of the coarse aggregates to rheology - effects of flow coefficient, particle size distribution, and volume fraction | wolfram.schmidt@bam.de

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0

10

20

30

40

50

60

70

80

90

100

0.5 1 2 4 8 16

Mesh m

inus [

%]

Sieve diameter [mm]

0

10

20

30

40

50

60

70

80

90

100

0.5 1 2 4 8 16

Mesh m

inus [

%]

Sieve diameter [mm]

0

10

20

30

40

50

60

70

80

90

100

0.5 1 2 4 8 16

Mesh m

inus [

%]

Sieve diameter [mm]

Results – highest viscosity PSD

07.03.2018Contribution of the coarse aggregates to rheology - effects of flow coefficient, particle size distribution, and volume fraction | wolfram.schmidt@bam.de

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CONCLUSIONS

Conclusions

07.03.2018Contribution of the coarse aggregates to rheology - effects of flow coefficient, particle size distribution, and volume fraction | wolfram.schmidt@bam.de

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Flow coefficient assessment:

• The flow coefficient does not correlate with loose bulk density.

• The flow coefficient is also not an adequate tool to predict the rheology influence

of the coarse particle.

Grading:

• Best yield stress reduction with coarse fractions > 50%

• Hardly effects of sand fractions on viscosity. Strong effect of coarse fraction.

Volume fraction:

• Blends of different aggregate fractions have particular influence of rheology.

• Volume fraction does not change particular effects, only the order of magnitude.

Conclusions

07.03.2018Contribution of the coarse aggregates to rheology - effects of flow coefficient, particle size distribution, and volume fraction | wolfram.schmidt@bam.de

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www.bam.de

THANK YOU VERY MUCH FOR YOUR KIND ATTENTION

ACKNOWLEDGEMENT:The study was part of the M-Flow project funded by BAM