INTEGRATED MINING IMPACT MONITORING (EU-PROJECT I2MON) FOR OPEN-PIT AND UNDERGROUND MINES

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Abstract. Monitoring mining impact has become increasingly important as the awareness of safety and environmental protection is rising. Our project Integrated Mining Impact Monitoring (i2Mon), funded by European Commission – Research Fund for Coal and Steel, intends to monitor the mining-induced impact, in particular, ground movement. The monitoring system comprises terrestrial measurement and remote sensing: levelling, GPS, LiDAR scanning, UAV survey, and SAR interferometry. The aim is to launch an interactive GIS-based platform as an early warning and decision making service for mining industry. This study has developed a scheme based on advanced SAR interferometry to monitor the ground movement over an extensive area at millimetre level. The first test site is a deactivated open-pit mine in Cottbus, Germany owned by Lausitz Energie Bergbau AG. The whole area was reclaimed into a post-mining lake and must be monitored for the safety. The second test site is located in Poland, where the underground mining operated by POLSKA GRUPA GÓRNICZA began in June 2021. We have monitored the in-situ ground movement carefully as part of the influenced area covers the human settlement. The ground movement of our test sites was analysed from Sentinel-1 images. The crucial parameters include stepwise movement series, instantaneous velocities and accelerations, and significance index. In addition, six corner reflectors along with sensors like GPS were installed across the region in Cottbus. They were observed in the Sentinel-1 series and the GPS readings will be used for validation. Finally, all the data will be integrated into DMT’s platform – SAFEGUARD.

Location: Deutsche Nationalbibliothek Frankfurt am Main

Extent: Online-Ressource

Language: Englisch

Bibliographic citation: INTEGRATED MINING IMPACT MONITORING (EU-PROJECT I²MON) FOR OPEN-PIT AND UNDERGROUND MINES ; volume:XLIII-B3-2022 ; year:2022 ; pages:367-372 ; extent:6
The International Archives of the Photogrammetry, Remote Sensing and Spatial Information Sciences ; XLIII-B3-2022 (2022), 367-372 (gesamt 6)

Classification: Natürliche Ressourcen, Energie und Umwelt

Creator: Yang, C. H.
Stemmler, C.
Pakzad, K.
Zimmermann, K.
Müterthies, A.

DOI: 10.5194/isprs-archives-XLIII-B3-2022-367-2022

URN: urn:nbn:de:101:1-2022060206092901159713

Rights: Open Access; Der Zugriff auf das Objekt ist unbeschränkt möglich.

Last update: 15.08.2025, 7:23 AM CEST

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Yang, C. H.
Stemmler, C.
Pakzad, K.
Zimmermann, K.
Müterthies, A.

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Verzeichnungseinheit

Besetzung der Generalsuperintendentur I, enth. Vita: Gen. Sup. Hlldebrandt 1623; Gen. Sup. Eickfeldt 1691; Gen. Sup. Lyser 1708; Gen. Sup. Böhmer 1726; Gen. Sup. Guden 1736; Gen. Sup. Plesken 1743; Gen. Sup. Eggers 1805; Gen. Sup. Hoppenstedt 1815

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Hochschulschrift

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Modelling oxygen (18O, 17O, 16O) and hydrogen (2H, 1H) water isotopes in the coupled numerical climate model iLOVECLIM (version 1.1.5)

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s - sup

Karte

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INTEGRATED MINING IMPACT MONITORING (EU-PROJECT I<sup>2</sup>MON) FOR OPEN-PIT AND UNDERGROUND MINES

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s - sup

Rhenus sup.

Saxonia sup.

Phasenbestand und Gleichgewichtsbeziehungen in den quaternären Systemen Li / M / P / O (M: Fe<sup>II</sup>, Co<sup>II</sup>, Ni<sup>II</sup>, Cu<sup>II</sup> und Cu<sup>II</sup>)

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s - sup

Rhenus sup.

Saxonia sup.

INTEGRATED MINING IMPACT MONITORING (EU-PROJECT I<sup>2</sup>MON) FOR OPEN-PIT AND UNDERGROUND MINES

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Other Objects (12)

Phasenbestand und Gleichgewichtsbeziehungen in den quaternären Systemen Li / M / P / O (M: Fe<sup>II</sup>, Co<sup>II</sup>, Ni<sup>II</sup>, Cu<sup>II</sup> und Cu<sup>II</sup>)

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Besetzung der Generalsuperintendentur I, enth. Vita: Gen. Sup. Hlldebrandt 1623; Gen. Sup. Eickfeldt 1691; Gen. Sup. Lyser 1708; Gen. Sup. Böhmer 1726; Gen. Sup. Guden 1736; Gen. Sup. Plesken 1743; Gen. Sup. Eggers 1805; Gen. Sup. Hoppenstedt 1815

s - sup

Rhenus sup.

Saxonia sup.

Phasenbestand und Gleichgewichtsbeziehungen in den quaternären Systemen Li / M / P / O (M: Fe<sup>II</sup>, Co<sup>II</sup>, Ni<sup>II</sup>, Cu<sup>II</sup> und Cu<sup>II</sup>)

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Precise dating of deglacial Laptev Sea sediments via <sup>14</sup>C and authigenic <sup>10</sup>Be/<sup>9</sup>Be &ndash; assessing local <sup>14</sup>C reservoir ages

Insights into Protein Dynamics from <sup>15</sup>N-<sup>1</sup>H HSQC

Reaction dynamics of P (<sup>4</sup>S) + O<sub>2</sub>(X <sup>3</sup>&Sigma;<sup>-</sup>) &rarr; O (<sup>3</sup>P) + PO (X <sup>2</sup>&Pi;) on a global CHIPR potential energy surface of PO<sub>2</sub>(X <sup>2</sup>A<sub>1</sub>): implication for atmospheric modelling

Global simulation of dissolved <sup>231</sup>Pa and <sup>230</sup>Th in the ocean and the sedimentary <sup>231</sup>Pa∕<sup>230</sup>Th ratios with the ocean general circulation model COCO ver4.0

Besetzung der Generalsuperintendentur I, enth. Vita: Gen. Sup. Hlldebrandt 1623; Gen. Sup. Eickfeldt 1691; Gen. Sup. Lyser 1708; Gen. Sup. Böhmer 1726; Gen. Sup. Guden 1736; Gen. Sup. Plesken 1743; Gen. Sup. Eggers 1805; Gen. Sup. Hoppenstedt 1815

s - sup

Rhenus sup.

Saxonia sup.

Phasenbestand und Gleichgewichtsbeziehungen in den quaternären Systemen Li / M / P / O (M: Fe<sup>II</sup>, Co<sup>II</sup>, Ni<sup>II</sup>, Cu<sup>II</sup> und Cu<sup>II</sup>)

Modelling oxygen (<sup>18</sup>O, <sup>17</sup>O, <sup>16</sup>O) and hydrogen (<sup>2</sup>H, <sup>1</sup>H) water isotopes in the coupled numerical climate model iLOVECLIM (version 1.1.5)

Precise dating of deglacial Laptev Sea sediments via <sup>14</sup>C and authigenic <sup>10</sup>Be/<sup>9</sup>Be &ndash; assessing local <sup>14</sup>C reservoir ages

Insights into Protein Dynamics from <sup>15</sup>N-<sup>1</sup>H HSQC

Reaction dynamics of P (<sup>4</sup>S) + O<sub>2</sub>(X <sup>3</sup>&Sigma;<sup>-</sup>) &rarr; O (<sup>3</sup>P) + PO (X <sup>2</sup>&Pi;) on a global CHIPR potential energy surface of PO<sub>2</sub>(X <sup>2</sup>A<sub>1</sub>): implication for atmospheric modelling

Global simulation of dissolved <sup>231</sup>Pa and <sup>230</sup>Th in the ocean and the sedimentary <sup>231</sup>Pa∕<sup>230</sup>Th ratios with the ocean general circulation model COCO ver4.0

Besetzung der Generalsuperintendentur I, enth. Vita: Gen. Sup. Hlldebrandt 1623; Gen. Sup. Eickfeldt 1691; Gen. Sup. Lyser 1708; Gen. Sup. Böhmer 1726; Gen. Sup. Guden 1736; Gen. Sup. Plesken 1743; Gen. Sup. Eggers 1805; Gen. Sup. Hoppenstedt 1815

s - sup

Rhenus sup.

Saxonia sup.

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Precise dating of deglacial Laptev Sea sediments via <sup>14</sup>C and authigenic <sup>10</sup>Be/<sup>9</sup>Be – assessing local <sup>14</sup>C reservoir ages

Reaction dynamics of P (<sup>4</sup>S) + O<sub>2</sub>(X <sup>3</sup>Σ<sup>-</sup>) → O (<sup>3</sup>P) + PO (X <sup>2</sup>Π) on a global CHIPR potential energy surface of PO<sub>2</sub>(X <sup>2</sup>A<sub>1</sub>): implication for atmospheric modelling

Precise dating of deglacial Laptev Sea sediments via <sup>14</sup>C and authigenic <sup>10</sup>Be/<sup>9</sup>Be – assessing local <sup>14</sup>C reservoir ages

Reaction dynamics of P (<sup>4</sup>S) + O<sub>2</sub>(X <sup>3</sup>Σ<sup>-</sup>) → O (<sup>3</sup>P) + PO (X <sup>2</sup>Π) on a global CHIPR potential energy surface of PO<sub>2</sub>(X <sup>2</sup>A<sub>1</sub>): implication for atmospheric modelling

Precise dating of deglacial Laptev Sea sediments via <sup>14</sup>C and authigenic <sup>10</sup>Be/<sup>9</sup>Be – assessing local <sup>14</sup>C reservoir ages

Reaction dynamics of P (<sup>4</sup>S) + O<sub>2</sub>(X <sup>3</sup>Σ<sup>-</sup>) → O (<sup>3</sup>P) + PO (X <sup>2</sup>Π) on a global CHIPR potential energy surface of PO<sub>2</sub>(X <sup>2</sup>A<sub>1</sub>): implication for atmospheric modelling