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SANDSTONE-HOSTED URANIUM MINERALIZATION IN
SELOUS GAME RESERVE AND ENVIRONMENTAL
ISSUES : A CASE OF MKUJU RIVER PROJECT-
TANZANIA




D.A. MWALONGO, S.L.C MDOE AND I.S.N. MKILAHA
CONTENTS
1.   INTRODUCTION
2.   OBJECTIVES
3.   U MINERALIZATION
4.   ENVIRONMENTAL ISSUES
5.   METHODOLOGY
6.   RESULTS
7.   CONCLUSION
INTRODUCTION
• Uranium mining is treated differently than other mines!
• The environmental Impact Statement (EIS) during
  approval process
• Higher level of community concern in relation to
  uranium mining than with other mining activities
• Lack of trust consultants/contractors EIA reports
• Increase cost and Delays
   – The Community perceptions;
   – The actual and perceived risks
OBJECTIVES OF THIS PRESENTATION

(I)BRIEF OVERVIEW OF URANIUM
   MINERALIZATION IN TANZANIA



(I)TO ESTABLISH A PRELIMINARY
   BASELINE RADIOACTIVITY LEVELS
U MINERALIZATION IN TANZANIA
Geosurvey International in 1976-1980 carried out uranium
exploration on country wide
Further ground follow-up was undertaken by Uranerzbergbau of
Germany in 1978-82
 Airborne geophysical survey comprising magnetics, radiometric
and electromagnetic methods was carried out all over the country
Spacing of the flight lines was 1 km and tie lines 10 km
Potential for follow up work suggested:
Sandstone and siltstone of Karroo System;
Igneous/intrusive type;
         -Carbonatite; and
         -Intra-intrusive rocks.
Hydrothermal type;
         - Unconformity vein type in Ubendian and Karagwe-Ankolean System
Phosphate rocks;
 Superficial calcrete and mbuga deposits; and
Radioactive beach sand.
THE DISTRIBUTION OF THE RADIOMETRIC ANOMALIES
Selous Game Reserve (SGR)U Anomalies
• Tabular Sandstone-hosted
  uranium deposit
• The SGR is the largest game
  reserve in Africa and
  includes two national parks
• It was declared a natural
  world heritage site in 1982
  by UNESCO
• The discovery alarmed the
  public and encounters
  oppositions from public and
  civil societie
• The baseline radiological
  studies were conducted by
  non partial audience to
  characterize the initial
  conditions
SGR RADIOMETRIC MAP
LOCAL GEOLOGY
The local geology of the project is located in large intracratonic
 basin filled with clastic sediments
The uranium mineralization is a tabular occurs intestinally in the
  course sandstones and conglomerate channel
Three trap lithologies namely:
   (i) Arkose unit containing carbonaceous debris, carbonaceous
         siltstone rip-up and mercasite/pyrite concretions
   (ii) Permeable coarser sandstones with marcasite concretions and
         fine joints and clay development in the matrix of permeable
         stratigraphy
   (iii) The oxidized organic rich outer zones where mineralized layers
         exposed on the sides of the steep hills

The rich outer zones are caused by uranium concentration and
upgrading as a direct result of reducing environment caused by
increase in organic materials
ENVIRONMENTAL ISSUES!!
WILD HABITAT!
Why?
Independent information for:
Regulatory authorities
 government Authorities
Environmentalist
The public,
Politicians; and
Government officials
High Purity Germanium (HPGe) detector was used
Relative efficiency of 55% and resolution of 1.70 keV at 1332
  keV energy of 60Co
The detector chamber was shielded with three layers of copper,
   cadmium and Lead of 30 mm, 3 mm and 100 mm thick,
   respectively
 Soil, sediment and surface water, food crops and
 Vegetations commonly feed by wild animals samples were
 measured
 The performance of the system was validated using IAEA
 reference materials like soil 375, the experimental values
 were within ± 5 %
RESULTS
ACTIVITY CONCENTRATION IN SOIL




Maximum activity concentration of 238U and 232Th and 40K
 in soil samples compared to the control (7*)

Any significant deviation from these values in future may
 be attributed to the uranium mining processes
Activity Concentration in sediments




The activity concentrations of 238U and 232Th and 40K
  radionuclide were higher than the control samples
 As expected, the activity concentration of the 238U, 232Th and
  40K in the sediment samples were much higher than those

   found in control samples
Activity Concentration in water




The activity concentrations 238U in the samples from Mkuju were slightly higher
 than the mean value in control sample
The activities of radionuclides in the analyzed water samples were comparable
The activities were also in the same range as the activity in the control sample
 The samples from wet Mkuju River had slightly higher activity concentration
  than other three samples
Activity Concentration in food crops




The results show highest average activity concentration of
238U, 232Th and 40K in from maize samples while cassava tuber

and millet grains have lowest activity concentration.
Activity Concentration in wild vegetation feed by wild animals




 The results showed elevated activity concentration of
  radionuclides 238U and 232Th in weeds sampled from riverbank
  than in grass
 Wild fruits showed lowest activity concentrations for all
  radionuclides
 The activity concentration is typical grass shows lowest activity
   concentrations which are commonly fed by animals d animals
6. CONCLUSION
The baseline information presented compared with
environmental data collected once the mine is
operational, will be used as a basis to evaluate potential
environmental impacts of the mine operations

The radiological baseline studies are important to
 build public trust about the industry

The Wildlife Act of 2009 has weakened the legal
  basis for World heritage
However, the status of to whether mining and milling
 activities will take place or not awaits UNESCO
 discretion
THANK YOU!

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Sandstone Uranium in Selous Game Reserve

  • 1. SANDSTONE-HOSTED URANIUM MINERALIZATION IN SELOUS GAME RESERVE AND ENVIRONMENTAL ISSUES : A CASE OF MKUJU RIVER PROJECT- TANZANIA D.A. MWALONGO, S.L.C MDOE AND I.S.N. MKILAHA
  • 2. CONTENTS 1. INTRODUCTION 2. OBJECTIVES 3. U MINERALIZATION 4. ENVIRONMENTAL ISSUES 5. METHODOLOGY 6. RESULTS 7. CONCLUSION
  • 3. INTRODUCTION • Uranium mining is treated differently than other mines! • The environmental Impact Statement (EIS) during approval process • Higher level of community concern in relation to uranium mining than with other mining activities • Lack of trust consultants/contractors EIA reports • Increase cost and Delays – The Community perceptions; – The actual and perceived risks
  • 4. OBJECTIVES OF THIS PRESENTATION (I)BRIEF OVERVIEW OF URANIUM MINERALIZATION IN TANZANIA (I)TO ESTABLISH A PRELIMINARY BASELINE RADIOACTIVITY LEVELS
  • 5. U MINERALIZATION IN TANZANIA Geosurvey International in 1976-1980 carried out uranium exploration on country wide Further ground follow-up was undertaken by Uranerzbergbau of Germany in 1978-82  Airborne geophysical survey comprising magnetics, radiometric and electromagnetic methods was carried out all over the country Spacing of the flight lines was 1 km and tie lines 10 km Potential for follow up work suggested: Sandstone and siltstone of Karroo System; Igneous/intrusive type; -Carbonatite; and -Intra-intrusive rocks. Hydrothermal type; - Unconformity vein type in Ubendian and Karagwe-Ankolean System Phosphate rocks;  Superficial calcrete and mbuga deposits; and Radioactive beach sand.
  • 6. THE DISTRIBUTION OF THE RADIOMETRIC ANOMALIES
  • 7. Selous Game Reserve (SGR)U Anomalies • Tabular Sandstone-hosted uranium deposit • The SGR is the largest game reserve in Africa and includes two national parks • It was declared a natural world heritage site in 1982 by UNESCO • The discovery alarmed the public and encounters oppositions from public and civil societie • The baseline radiological studies were conducted by non partial audience to characterize the initial conditions
  • 9. LOCAL GEOLOGY The local geology of the project is located in large intracratonic basin filled with clastic sediments The uranium mineralization is a tabular occurs intestinally in the course sandstones and conglomerate channel Three trap lithologies namely: (i) Arkose unit containing carbonaceous debris, carbonaceous siltstone rip-up and mercasite/pyrite concretions (ii) Permeable coarser sandstones with marcasite concretions and fine joints and clay development in the matrix of permeable stratigraphy (iii) The oxidized organic rich outer zones where mineralized layers exposed on the sides of the steep hills The rich outer zones are caused by uranium concentration and upgrading as a direct result of reducing environment caused by increase in organic materials
  • 12. Why? Independent information for: Regulatory authorities  government Authorities Environmentalist The public, Politicians; and Government officials
  • 13. High Purity Germanium (HPGe) detector was used Relative efficiency of 55% and resolution of 1.70 keV at 1332 keV energy of 60Co The detector chamber was shielded with three layers of copper, cadmium and Lead of 30 mm, 3 mm and 100 mm thick, respectively Soil, sediment and surface water, food crops and Vegetations commonly feed by wild animals samples were measured The performance of the system was validated using IAEA reference materials like soil 375, the experimental values were within ± 5 %
  • 15. ACTIVITY CONCENTRATION IN SOIL Maximum activity concentration of 238U and 232Th and 40K in soil samples compared to the control (7*) Any significant deviation from these values in future may be attributed to the uranium mining processes
  • 16. Activity Concentration in sediments The activity concentrations of 238U and 232Th and 40K radionuclide were higher than the control samples  As expected, the activity concentration of the 238U, 232Th and 40K in the sediment samples were much higher than those found in control samples
  • 17. Activity Concentration in water The activity concentrations 238U in the samples from Mkuju were slightly higher than the mean value in control sample The activities of radionuclides in the analyzed water samples were comparable The activities were also in the same range as the activity in the control sample  The samples from wet Mkuju River had slightly higher activity concentration than other three samples
  • 18. Activity Concentration in food crops The results show highest average activity concentration of 238U, 232Th and 40K in from maize samples while cassava tuber and millet grains have lowest activity concentration.
  • 19. Activity Concentration in wild vegetation feed by wild animals The results showed elevated activity concentration of radionuclides 238U and 232Th in weeds sampled from riverbank than in grass Wild fruits showed lowest activity concentrations for all radionuclides The activity concentration is typical grass shows lowest activity concentrations which are commonly fed by animals d animals
  • 20. 6. CONCLUSION The baseline information presented compared with environmental data collected once the mine is operational, will be used as a basis to evaluate potential environmental impacts of the mine operations The radiological baseline studies are important to build public trust about the industry The Wildlife Act of 2009 has weakened the legal basis for World heritage However, the status of to whether mining and milling activities will take place or not awaits UNESCO discretion