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Study of alpine glaciers with cosmic- ray muon radiograph Akitaka Ariga, University of Bern, Switzerland for the Eiger-m GT collaboration Aletsch glacier © Swissinfo

Akitaka Ariga, University of Bern, Switzerland for …flab.phys.nagoya-u.ac.jp/2011/ICMASS2017/Ariga_Eiger...Eiger-m GT: Application of muon tomography to glaciers •Erosion process

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Study of alpine glaciers with cosmic-ray muon radiograph

Akitaka Ariga, University of Bern, Switzerland

for the Eiger-m GT collaboration

Aletsch glacier © Swissinfo

Volcanoes for Japan, glaciers for Switzerland

• Symbol of national landscape

• Source of hazards & resources

• Public interest

• Problems in glaciology • Several models for glacial erosional process have been proposed

from the observation of “past” glaciers, c. 24 Kys ago

• However, no measurement of “active” glaciers, particularly where they originate

• The models left experimentally untested, because no appropriate method to study bedrock morphology

• Muon radiography is an excellent method to study the bedrock morphology

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Bern

24,000 years ago

Zurich

Geneve

Eiger

Moench Jungfrau

Eiger-m GT

Jungfrau research station

Eiger-m GT: Application of muon tomography to glaciers

• Erosion process by glaciers is of interest in glaciology

• Eiger & Aletsch glaciers in Swiss central alps

• Suited experimental conditions • Length from surface to detector = 500-1000 m

• High density contrast between rock and ice, 2.7: 0.85g/cm^3

• Support from Jungfrau rail company

ρ = 0.85 g/cm3

ρ = 2.7 g/cm3

detector

muons

glacier

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5

Sphynx observatory

Exit for tourists

Jungfrau Bedrock morphology at the upmost part of Aletsch glacier

Bedrock morphology at the upmost part of Aletsch glacier • Glaciers hold mountains. If the glacier retreat…

• Need to know the bedrock for safety measures

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Glacier retreat Landslides

Safer Dangerous

Test observation at Aletsch glacier • 3 detectors around region of interest along the

rail way

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100 m D2

47 days, 250 cm2 at each site

Observed muon flux

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Angular distribution at D1 Rock thickness along muon pass (rock + ice)

D1

D2

D3

slope x

slo

pe

y

Mountain peak Glacier

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Analysis procedure

(i) Rock density calibration

(ii) Bedrock measurement (two density approximation)

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Calibration of rock density

• Two methods • Bulk density measurement, by sampling 14 rocks in the railway

tunnel.

• Muon attenuation (3 detectors)

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Result of bedrock reconstruction at Aletsch glacier R. Nishiyama, A. Ariga, T. Ariga, S. Kaser, A. Lechmann, D. Mair, P. Scampoli, M. Vladymyrov, A. Ereditato, F. Schlunegger, Geophysical Research Letters 55933 (2017). DOI: 10.1002/2017GL073599.

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accumulation

erosion overdeepening

ablation

U shape

Main project: Eiger glacier

Observation from 3 sites to reconstruct in 3D

Detector size: 0.2 m2 2 detectors at all 3 sites

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Status of project

• Spring run (8m2) 2017/3-2017/7 scanning

• Summer run (8m2) 2017/7-2018/12 exposing

• Currently, one mic. ~ 15 cm2/h

• October on, 50 cm2/h

• By end of this year, 130 cm2/h

• First result in winter

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New software, enlarged stage

Development of extra-large crystals for large scale muon radiography

• Established a crystal size up to 1200 nm (standard size= 200 nm)

36 times faster readout

• Sufficient S/N for MIP

• Testing for a practical use

• Partially used for the main project

200 nm crystal 650 nm 650-1000 nm

200 nm

650 nm

1000 nm

Collaboration with Nagoya Univ.

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Summary

• Application of muon radiography to glaciology

• The first result at the Aletsch glacier was published public impact • The first application to glaciology

• Analysis for Eiger glacier will appear soon • The new type emulsion is being tested in situ

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予備スライド

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氷河学の問題点

• 過去 (約2万4千年前) の氷河地形の観測によりいくつかの浸食モデルが提案された

• しかし、現在アクティブな氷河についての測定はない、特に氷河の上流について。

• 氷河の岩盤を測定に適した技術がないため、モデルは検証されずにいる。

• レーダー (電気伝導度) : 水と氷が混在する場所では使えない。危険。

• 重力 (質量) : 原理的に3D再構成が難しい。危険。

• ボアリング : 1D情報しか得られない、形状についての情報がない。危険。

• 地震波:水の存在は地震波を減衰。危険。

• ミューオンラジオグラフィー (密度) は岩盤の形状測定に適している。

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Jungfrau railway • Cooperative with us!

• Provide the necessary and sufficient environment

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天頂角

方位角 (azimuth angle) (elevation angle)

(zenith angle)

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How emulsion detectors work

Sensitive layer

Plastic base

Charged particle

High speed camera

Objective lens

After development

Trajectory of particle as a sequence of dots

Read out by automated scanning microscopes

20 mm

10GeV/c beam

Sensitivity 36 grains/100 mm

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European scanning system • CPU tracking, up to 20 cm2 /h

• Based on commercial products

• About 40 microscopes in OPERA

• Go-and-Stop motion

CMOS camera

1280×1024 pixel

376 frames/sec

(Mikrotron MC1310)

XY stage (Micos)

0.1 μm nominal

precision

Emulsion film Z stage (Micos)

0.05 μm nominal

precision

objective (Dry 50× NA 0.95)

(or oil lens)

Automatic Plate Changer

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