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Unbalance of uranium radiation system and its application in environmental research
The imbalance of uranium radiation system and its application in environmental research is a book published by Ocean Press 199 1.

Basic Introduction Translator: Chen Tiemei/et al. ISBN :9787502702809 Page: 392 Pricing: 18.90 Publishing House: Ocean Publishing House Publishing Time: 199 1-07 Binding: Paperback Content Introduction, Working Directory, Uranium (235U, 2337) The destruction and reconstruction of radioactive balance among members of uranium series are all over the natural environment. This book was written by 19 influential foreign scholars in this field. Chapter *** 19 of the book systematically introduces the theory, experimental methods and techniques of uranium series imbalance, summarizes the application of uranium series imbalance method in geology, oceanography, hydrology, geochemistry, isotope chronology, archaeology and environmental science in recent 30 years, and looks forward to the development prospect of this field. This book can be used as a reference for researchers in the above disciplines and teachers and students in colleges and universities. The first chapter of the catalogue of works is radioactive phenomenon.

1. 1 Introduction to Nuclear Physics

1.2 nuclear stability limit

1.3 radioactive disintegration type

1.3. 1 a decay

1.3.2 β decay

1.3.3 γ -ray emission

Radioactive decay law of 1.4

1.5 radioactive decay system

Chapter II Geochemistry of Actinides and Their Subelements

2. 1 Introduction

2. 1. 1 attribute of the element

2. 1.2 Comprehensive general chemical properties and geochemistry

2. 1.3 Influence of weathering

2.2 Sources of Actinides

2.2. 1 igneous rock

2.2.2 Sedimentary rocks and quasi-sedimentary rocks

2.2.3 Modern sediments

hydrosphere

deposit

2.3 geochemical cycle

Mobilization and treatment in solution

2.3.2 Mobilization and treatment of particulate matter

2.3.3 Gas phase activation and treatment

2.4 Deposition process in near-surface environment

2. 1.4 Inorganic deposition and biological deposition

adsorbing

deposition

2.5 Influence of age effect and diagenesis on isotope imbalance

2.5. 1 uranium isotope fractionation

2.5.2 Natural variation of radioactivity ratio

2.5.3 Fractionation of other actinides and their sub-elements.

Chapter III Application of Uranium Series Unbalanced Casing in Geochronology

3. 1 Radioactivity Dating

3.2 Uranium series unbalanced dating method

3.3 Dating method based on U-series daughter accumulation

3. 3. 1 230/234 u dating method

3.3.2 23 1Pa/235U dating method

3.3.3 Helium/uranium dating method

3.4 Dating method based on the decay of residual uranium series daughters

3.4. 1 234U/238U dating method

3.4.2 Over-dating method for the 30th issue.

3.4.3 23 1Pa over-dating method

3.4.4 230th/232nd Dating Method

3.4.5 231pa/230s dating method

3.4.6 Article 234 Dating Method

3.4.7 The 238th/232nd Dating Method

3.4.8 2 10Pb dating method

3.5 suitability criteria for dating

3.6 drilling cuttings pollution correction technology

3.7 open system dating method

Chapter IV Chemical Process

4. 1 Introduction

4. 1. 1 preconcentration or extraction

4. 1.2 separation process

4. 1.3 Preparation of radioactive sources

4.2 Comprehensive evaluation of analytical separation technologies for uranium-thorium-phosphorus, radium, radon, lead and polonium.

4.2. 1 uranium

thorium

praseodymium (Pr)

radium (Ra)

ammonia

leader

polonium

4.3 Sample Preparation and Pretreatment

4.3. 1 homologous sample

Liquid sample

4.4 published meThod for determination of u, th, Pb, Po, Pa, Ra, Rn and he in environmental samples.

4.5 Preparation of radioactive sources

4.5. 1 a spectrometer source

4.5.2 Total α and β Counting Sources

Mass spectrometry source

4.6 Summary

Chapter V Nuclear Energy Spectrum Technology

5. 1 Interaction between nuclear radiation and matter

5.2 Detection of Nuclear Radiation

5.2. 1 nuclear radiation detector

ancillary equipment

5.3 Radionuclide detection and measurement methods

5.3. 1 energy spectrum measurement

β energy spectrum measurement

5.3.3 γ -ray spectrum measurement

5.3.4 Other methods for analyzing radionuclides

5.4 Nuclear Statistics and Data Processing

5.5 Measurement of Uranium Series Imbalance

5.5. 1 uranium content and radioactivity ratio are 234U/238U, 230t/34U and 20t/232t.

5.5.2 Measurement of radioactivity ratio 5.5.2 23 1Pa/235U

5.5.3 measurement of ra and Rn

5.5.4 measurement of pbbi and Po

Chapter VI Igneous Rock

6. 1 concentration of radioactive elements in igneous rocks

6.2 Distribution of Uranium and Thorium

6.3 Chemical Properties of Uranium and Thorium in Igneous Environment

6.4 Geochronology

6.4. 1 Introduction

6.4.2 Theory

6.4.3 Example

6.5 Study on Tracer

6.5. 1 Introduction

6.5.2 Theory

6.5.3 Example

Chapter VII Activation and Weathering

7. 1 Introduction

7.2 Activity and Leaching Experiment

7.3 Alteration and Weathering 2

7.3. 1 Early weathering

Surface weathering

Chapter VIII Chemistry of Uranium-series and Thorium-series Nuclides in Rivers

8. 1 Introduction

8.2 Uranium

Uranium in river water

8.2.2 Uranium in Estuary Waters

8.2.3 Uranium in river sediments

8.3 Thorium and Praseodymium

8.4 Radium

8.5 lead -2 10

Chapter IX Groundwater

9. 1 background and theory

9. 1. 1 Introduction

9. 1.2 water cycle fractionation

9. 1.3 activator

9. 1.4 Radioisotope evolution and aquifer classification

9. 1.5 aquifer imbalance and geochemical front

9.2 Case study

9.2. 1 Introduction

Conservative state

Non-conservative state

9.3 sets are used to determine the age of groundwater.

9.3. 1 General requirements

Radon and helium

Isotopes of radium

9.3.4 uranium isotope

Chapter X Continental Surface Sediments

10. 1 Introduction

10.2 surface carbonate sediments

10.2. 1 Possibility of formation and dating of various authigenic carbonates.

An example of 10.2.2 uranium series method for determining carbonate age in surface sediments.

10.3 sediments and soil

Behavior of 10.3. 1 U in sediments

10.3.2 uranium trend model dating method

Chapter II XI Carbonate and Sulfate Deposition

1 1. 1 carbonate and sulfate precipitation in groundwater and surface water

1 1.2 uranium and thorium geochemistry of freshwater carbonates and sulfates

Cave sediments 1 1.3 uranium series dating

1 1.3. 1 physical properties of cave sediments

1 1.3.2 analysis technology

1 1.3.3 Early research

1 1.3.4 Recent Works

1 1.4 uranium dating of travertine and hydrate

1 1.5 Lake sediments

1 1.5. 1 Physical properties of sediments

8.2.3 Uranium in river sediments

8.3 Thorium and Praseodymium

8.4 Radium

8.5 lead -2 10

Chapter IX Groundwater

9. 1 background and theory

9. 1. 1 Introduction

9. 1.2 water cycle fractionation

9. 1.3 activator

9. 1.4 Radioisotope evolution and aquifer classification

9. 1.5 aquifer imbalance and geochemical front

9.2 Case study

9.2. 1 Introduction

Conservative state

Non-conservative state

9.3 sets are used to determine the age of groundwater.

9.3. 1 General requirements

Radon and helium

Isotopes of radium

9.3.4 uranium isotope

Chapter X Continental Surface Sediments

10. 1 Introduction

10.2 surface carbonate sediments

10.2. 1 Possibility of formation and dating of various authigenic carbonates.

An example of 10.2.2 uranium series method for determining carbonate age in surface sediments.

10.3 sediments and soil

Behavior of 10.3. 1 U in sediments

10.3.2 uranium trend model dating method

Chapter II XI Carbonate and Sulfate Deposition

1 1. 1 carbonate and sulfate precipitation in groundwater and surface water

1 1.2 uranium and thorium geochemistry of freshwater carbonates and sulfates

Cave sediments 1 1.3 uranium series dating

1 1.3. 1 physical properties of cave sediments

1 1.3.2 analysis technology

1 1.3.3 Early research

1 1.3.4 Recent Works

1 1.4 uranium dating of travertine and hydrate

1 1.5 Lake sediments

1 1.5. 1 Physical properties of sediments

1 1.5.2 analysis technology

Previous works 1 1.5.3

1 1.6 summary and conclusion

Chapter XII Application of Uranium Dating Method in Archaeology

12. 1 introduction: the absolute time scale of human evolution

12.2 is suitable for dating archaeological samples of uranium series method.

12.2. 1 inorganic calcium carbonate deposition

12.2.2 biological source samples

12.3 Appointment Steps and Scope

12.3. 1 travertine (including cave carbonate sediments, water stone, spring flowers, etc. )

12.3.2 biocarbonate

12.3.3 bones and teeth

12.3.4 Other criteria

12.4 application

12.4. 1 travertine

mollusc

12.4.3 skeleton

12.5 future work

Chapter XIII Application of Uranium Dating Method in Quaternary Climate Problems

13. 1 Introduction

13.2 nature of paleoclimate records

13.2. 1 maritime record

13.2.2 mainland records

13.3 examples of dating continental sediments with climatic significance

1.3. 1 lake sediments

13.3.2 spring sediments

13.3.3 Cave carbonate sediments

13.3.4 carbonate during soil formation

13.3.5 organic sediments

13.4 summary and conclusion

Chapter XIV Uranium Exploration

14. 1 Introduction

/kloc-classification of 0/4.2u deposits

Determination of uranium source rocks by 14.3 unbalanced method

14.4 uranium exploration

14.4. 1 238U and 235U in uranium exploration

14.4.2 234U in uranium exploration

14.4.3 No.230th uranium exploration

14.4.4 226Ra in uranium exploration

14.4.5 22Rn in uranium exploration

14.4.6 2 14Bi in uranium exploration

14.4.7 2 10Pb and 2 10Po in uranium exploration.

14.4.8 stable nuclides (4He and 206Pb) in uranium exploration.

14.5 uranium series imbalance and environmental safety issues

14.6 conclusion

Chapter XV Marine Chemistry of Uranium-series and Thorium-series Nuclides

15. 1 Introduction

15. 1. 1 Import and export of uranium and thorium nuclides in the ocean.

15.2 uranium

15.2. 1 uranium input into the ocean

15.2.2 uranium in offshore waters

15.2.3 uranium in the ocean

Uranium in pore water of sediments

15.2.5 migration of uranium from the ocean

15.2.6 source and migration of 236U in the ocean

15.3 thorium

Removal of Thorium from Deep Sea

Balance 15.3.2 No.230th and No.231pa

15.3.3 thorium migration from offshore and surface seawater

15.4 radium

1 radium 226

15.4.2 radium 228

15.5 radon

15.5. 1 radon in surface seawater

15.5.2 222Rn is used as a tracer for vertical mixing near the bottom.

15.6 Pb-2 10

15.6. 1 2 10Pb replenishment in the ocean

Distribution of 2 10Pb in surface seawater

Behavior of 15. 6. 3 2 10Pb in deep sea

15.7 ? -2 10

Chapter 16 Sediments and Deposition Process

16. 1 Introduction and history

16.2 sediments and pore water? Concentration and distribution of series nuclides

1 uranium

Thorium and praseodymium

16.2.3 Radium

16.2.4 radon

16.2.5 lead

16.3 dating of sediment accumulation and mixing

16.3. 1 deep-sea sediment accumulation rate (230,231pa)

16.3.2 Growth rate of manganese nodules

16.3.3 shallow sea sediments

16.4 as the source and migration site of actinides.

Chapter XVII Carbonate and Phosphate Deposits

17. 1 Introduction

17.2 u series dating of marine carbonate

coral

mollusc

17.2.3 application

U-series dating of 17.3 phosphorite

Geochemical considerations

17.3.2 marine phospholimestone

17.3.3 island phosphorite

The meaning of geology and oceanography

Chapter 18 Sea Level History of Late Pleistocene

18. 1 Introduction

18.2 dating technique of coral fossils

18.3 substances used for date determination

18.4 coral fossil age

18.5 research example

Barbados, West Indies

18.5.2 huhne peninsula, new guinea

18.5.3 Ryukyu islands, Japan

New hebrides and Loyalty.

Timor and atauro island.

18.5.6 Bahamas

18.5.7 Bermuda

18.5.8 Oahu, Hawaii

Jamaica

18.5. 10 Western Australia

18.5. 1 1

18.5. 12 southern California

18.5. 13 American Atlantic coastal plain

Yucatan Peninsula and South Caribbean Sea

18.5. 15 Tonga Island Arc

18.5. 16 Comprehensive analysis of research cases

18.6 uranium series technology popularization

Late Pleistocene 18.7 sea level curve

The influence of 18.8 on Pleistocene theory

Chapter 19 Progress and Prospect

19. 1 Introduction

19.2 geochronology study

19.3 tracer study

Derivation of radioactivity-age equations of appendix I 234 u/238 u and 230t/234 u

An example of determining counting error in Appendix II

Appendix III UTAGE-3 computer program for calculating the age of 230/234 u

Appendix IV computer program for calculating the age of 23 1Pa/235U by measuring the 27th century method.

Appendix V Equation of uranium trend model

refer to