The self-potential (SP) method is a passive geophysical technique that measures natural voltage potentials in the ground generated by electrochemical processes. It does not require injecting electric currents like resistivity and IP methods. SP has been used for mineral and groundwater exploration. Measurements are made at the surface using non-polarizing electrodes to detect subtle potential differences ranging from less than 1 mV to over 1 V. Anomalies are caused by electrokinetic, thermoelectric, electrochemical and mineralization potentials. SP is useful for mapping ore bodies, faults, water seepage and geothermal features. Interpretation of SP data considers polarity, amplitude and shape of anomalies to infer subsurface structures.
This Lecture includes the Resistivity survey, field procedure, application advantage, limitaion, Apparant resistivity, VES (Vertical Electrical Sounding), Resistivity Profiling and IP Survey in brief.
The presentation comprises the Gravity Method, It's anomaly, reduction, and its applications. The Gravity method is commonly used in Geology specifically in Geophysics.
This Lecture includes the Resistivity survey, field procedure, application advantage, limitaion, Apparant resistivity, VES (Vertical Electrical Sounding), Resistivity Profiling and IP Survey in brief.
The presentation comprises the Gravity Method, It's anomaly, reduction, and its applications. The Gravity method is commonly used in Geology specifically in Geophysics.
The Lectures describes the Electrical method of Geophysical Prospecting in brief. SP surveying and Occurrence of Self potential and its application is discussed in brief.
Information about these fluids is an invaluable aid in mineral exploration.
Conventional academic methods of analysing fluid inclusions are too slow and tedious to be of practical application in typical mineral exploration activities.
However, the academic data from numerous studies does show that CO2 is an exceptionally important indicator when exploring for most types of gold deposit.
Because the baro-acoustic decrepitation method is a rapid and reliable method to measure CO2 contents in fluids, it can be used to study a spatial array of data and it is an invaluable and practical exploration method.
Measurements of temperatures of fluid inclusions does not usually help in mineral exploration as hydrothermal minerals deposit over a wide temperature range and there is no specific temperature which is indicative of mineralisation. However, if temperatures are available on a large spatial array of samples, then temperature trends may be a useful exploration method to find the hottest part of the system, which is presumably the location of the best economic mineralisation. Baro-acoustic decrepitation is the most practical method to determine temperatures of the large numbers of samples required.
Salinities of fluid inclusions are of limited use in exploration and are difficult to measure. However, they can be used to recognise intrusion related hydrothermal systems.
The Lectures describes the Electrical method of Geophysical Prospecting in brief. SP surveying and Occurrence of Self potential and its application is discussed in brief.
Information about these fluids is an invaluable aid in mineral exploration.
Conventional academic methods of analysing fluid inclusions are too slow and tedious to be of practical application in typical mineral exploration activities.
However, the academic data from numerous studies does show that CO2 is an exceptionally important indicator when exploring for most types of gold deposit.
Because the baro-acoustic decrepitation method is a rapid and reliable method to measure CO2 contents in fluids, it can be used to study a spatial array of data and it is an invaluable and practical exploration method.
Measurements of temperatures of fluid inclusions does not usually help in mineral exploration as hydrothermal minerals deposit over a wide temperature range and there is no specific temperature which is indicative of mineralisation. However, if temperatures are available on a large spatial array of samples, then temperature trends may be a useful exploration method to find the hottest part of the system, which is presumably the location of the best economic mineralisation. Baro-acoustic decrepitation is the most practical method to determine temperatures of the large numbers of samples required.
Salinities of fluid inclusions are of limited use in exploration and are difficult to measure. However, they can be used to recognise intrusion related hydrothermal systems.
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ELECTRICAL DOUBLE LAYER-TYPES-DYNAMICS OF ELECTRON TRANSFER-MARCUS THEORY-TUNNELING - BUTLER VOLMER EQUATIONS-TAFEL EQUATIONS-POLARIZATION AND OVERVOLTAGE-CORROSION AND PASSIVITY-POURBAIX AND EVAN DIAGRAM-POWER STORAGE-FUEL CELLS
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In this book, we use conservation of energy techniques on a fluid element to derive the Modified Bernoulli equation of flow with viscous or friction effects. We derive the general equation of flow/ velocity and then from this we derive the Pouiselle flow equation, the transition flow equation and the turbulent flow equation. In the situations where there are no viscous effects , the equation reduces to the Bernoulli equation. From experimental results, we are able to include other terms in the Bernoulli equation. We also look at cases where pressure gradients exist. We use the Modified Bernoulli equation to derive equations of flow rate for pipes of different cross sectional areas connected together. We also extend our techniques of energy conservation to a sphere falling in a viscous medium under the effect of gravity. We demonstrate Stokes equation of terminal velocity and turbulent flow equation. We look at a way of calculating the time taken for a body to fall in a viscous medium. We also look at the general equation of terminal velocity.
Toxic effects of heavy metals : Lead and Arsenicsanjana502982
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Richard's aventures in two entangled wonderlandsRichard Gill
Since the loophole-free Bell experiments of 2020 and the Nobel prizes in physics of 2022, critics of Bell's work have retreated to the fortress of super-determinism. Now, super-determinism is a derogatory word - it just means "determinism". Palmer, Hance and Hossenfelder argue that quantum mechanics and determinism are not incompatible, using a sophisticated mathematical construction based on a subtle thinning of allowed states and measurements in quantum mechanics, such that what is left appears to make Bell's argument fail, without altering the empirical predictions of quantum mechanics. I think however that it is a smoke screen, and the slogan "lost in math" comes to my mind. I will discuss some other recent disproofs of Bell's theorem using the language of causality based on causal graphs. Causal thinking is also central to law and justice. I will mention surprising connections to my work on serial killer nurse cases, in particular the Dutch case of Lucia de Berk and the current UK case of Lucy Letby.
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Binocular Telescope, show evidence of a major resurfacing event on Io’s trailing hemisphere. When compared to the most recent spacecraft images, the SHARK-VIS images
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Slide 1: Title Slide
Extrachromosomal Inheritance
Slide 2: Introduction to Extrachromosomal Inheritance
Definition: Extrachromosomal inheritance refers to the transmission of genetic material that is not found within the nucleus.
Key Components: Involves genes located in mitochondria, chloroplasts, and plasmids.
Slide 3: Mitochondrial Inheritance
Mitochondria: Organelles responsible for energy production.
Mitochondrial DNA (mtDNA): Circular DNA molecule found in mitochondria.
Inheritance Pattern: Maternally inherited, meaning it is passed from mothers to all their offspring.
Diseases: Examples include Leber’s hereditary optic neuropathy (LHON) and mitochondrial myopathy.
Slide 4: Chloroplast Inheritance
Chloroplasts: Organelles responsible for photosynthesis in plants.
Chloroplast DNA (cpDNA): Circular DNA molecule found in chloroplasts.
Inheritance Pattern: Often maternally inherited in most plants, but can vary in some species.
Examples: Variegation in plants, where leaf color patterns are determined by chloroplast DNA.
Slide 5: Plasmid Inheritance
Plasmids: Small, circular DNA molecules found in bacteria and some eukaryotes.
Features: Can carry antibiotic resistance genes and can be transferred between cells through processes like conjugation.
Significance: Important in biotechnology for gene cloning and genetic engineering.
Slide 6: Mechanisms of Extrachromosomal Inheritance
Non-Mendelian Patterns: Do not follow Mendel’s laws of inheritance.
Cytoplasmic Segregation: During cell division, organelles like mitochondria and chloroplasts are randomly distributed to daughter cells.
Heteroplasmy: Presence of more than one type of organellar genome within a cell, leading to variation in expression.
Slide 7: Examples of Extrachromosomal Inheritance
Four O’clock Plant (Mirabilis jalapa): Shows variegated leaves due to different cpDNA in leaf cells.
Petite Mutants in Yeast: Result from mutations in mitochondrial DNA affecting respiration.
Slide 8: Importance of Extrachromosomal Inheritance
Evolution: Provides insight into the evolution of eukaryotic cells.
Medicine: Understanding mitochondrial inheritance helps in diagnosing and treating mitochondrial diseases.
Agriculture: Chloroplast inheritance can be used in plant breeding and genetic modification.
Slide 9: Recent Research and Advances
Gene Editing: Techniques like CRISPR-Cas9 are being used to edit mitochondrial and chloroplast DNA.
Therapies: Development of mitochondrial replacement therapy (MRT) for preventing mitochondrial diseases.
Slide 10: Conclusion
Summary: Extrachromosomal inheritance involves the transmission of genetic material outside the nucleus and plays a crucial role in genetics, medicine, and biotechnology.
Future Directions: Continued research and technological advancements hold promise for new treatments and applications.
Slide 11: Questions and Discussion
Invite Audience: Open the floor for any questions or further discussion on the topic.
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Inspired by David Donoho's vision, this talk aims to revisit the three crucial pillars of frictionless reproducibility (data sharing, code sharing, and competitive challenges) with the perspective of deep software variability.
Our observation is that multiple layers — hardware, operating systems, third-party libraries, software versions, input data, compile-time options, and parameters — are subject to variability that exacerbates frictions but is also essential for achieving robust, generalizable results and fostering innovation. I will first review the literature, providing evidence of how the complex variability interactions across these layers affect qualitative and quantitative software properties, thereby complicating the reproduction and replication of scientific studies in various fields.
I will then present some software engineering and AI techniques that can support the strategic exploration of variability spaces. These include the use of abstractions and models (e.g., feature models), sampling strategies (e.g., uniform, random), cost-effective measurements (e.g., incremental build of software configurations), and dimensionality reduction methods (e.g., transfer learning, feature selection, software debloating).
I will finally argue that deep variability is both the problem and solution of frictionless reproducibility, calling the software science community to develop new methods and tools to manage variability and foster reproducibility in software systems.
Exposé invité Journées Nationales du GDR GPL 2024
1. Self‐potential (SP) Method
•or spontaneous polarization method is based on the surface measurement
of natural potentials resulting from electrochemical reactions in the
subsurface.
subsurface.
•does not require electric currents to be injected into the ground as in the
RESISTIVITY & IP methods
RESISTIVITY & IP methods.
•has been used in base metal exploration, to detect the presence of massive
b di i t t t th IP th d hi h i d t d i tl t
ore bodies, in contrast to the IP method which is used to predominantly to
investigate disseminated ore bodies.
•has been increasingly used in groundwater & geothermal investigations,
environmental and engineering applications‐‐‐> mapping seepage flow
associated with dams, geological mapping, delineate shear zones and near‐
associated with dams, geological mapping, delineate shear zones and near
surface faults.
•ranks as the cheapest of surface geophysical methods in terms of
•ranks as the cheapest of surface geophysical methods in terms of
equipment necessary and amongst the simplest to operate in the field.
2. Occurrence of Self‐potentials
•SP method is passive, i.e. differences in natural ground potentials are
measured between any two points on the ground surface.
•The potentials measured can range from < a millivolt (mV) to > 1
Volt.
• + or – sigh of the potential is an important diagnostic factor in the
interpretation of SP anomalies
interpretation of SP anomalies.
•Self‐potentials are generated by a number of natural sources (exact
Self potentials are generated by a number of natural sources (exact
physical processes still unclear).
3. Occurrence of Self‐potentials
•Natural ground potentials consist of 2 components
1. Background Potentials‐‐‐fluctuate with time caused by different
1. Background Potentials fluctuate with time caused by different
processes ranging from AC currents induced by thunderstorms,
variations in Earth’s magnetic fields, effects of heavy rainfalls
2. Mineral Potentials‐‐‐constant due to electrochemical processes
4.
5. h l d f ll l
Mechanism of Self‐potentials
•Some physical processes caused sources of SP are still unclear.
•Groundwater is thought to be common factor responsible for SP.
P t ti l t d b th fl f t b t ti
•Potentials are generated by the flow of water, by water reacting as
an electrolyte and as a solvent of different minerals.
•Electrical conductivity to produce potentials of porous rocks depends
on porosity and on mobility of water to pass through the pore spaces
‐‐‐depend on ionic mobilities, solution concentrations, viscosity,
depend on ionic mobilities, solution concentrations, viscosity,
temperature & pressure.
•There are a few types of SP :
•There are a few types of SP :
1.Electrokinetic potential
2 Thermoelectric potential
2. Thermoelectric potential
3. Electrochemical potential
4. Mineral/mineralization potential
/ p
6. Fl i f fl id ( l t l t ) th h ill
Electrokinetic potential
• Flowing of fluid (electrolyte) through a capillary or porous
medium generates potentials along the flow path.
• The potentials are alternatively called as electrofiltration
• The potentials are alternatively called as electrofiltration,
electromechanical or streaming potentials.
• The effect is believed to be due to electrokinetic coupling
The effect is believed to be due to electrokinetic coupling
between the fluid ions and the walls of the capillary.
• The electrokinetic potential (Ek) generated between the ends of
The electrokinetic potential (Ek) generated between the ends of
the capillary passage is given by
= Dielectric permittivity of pore fluid
= Electrical resistivity of pore fluid
= Electrofiltration coupling coefficient
= Pressure difference
= Dynamic viscosity of pore fluid
7. E di t i i th di ti th di t i
Electrokinetic potential
• Ek gradient is in the same direction as the pressure gradient, i.e.
opposite to the direction of the electrolyte flow.
• E normally providse amplitudes of some mV to several hundreds
• Ek normally providse amplitudes of some mV to several hundreds
of mV.
• Ek can be found associated with flow of subsurface water and
Ek can be found associated with flow of subsurface water and
thermal fluids
• Ek effects have been observed over zones of water leakage
Ek effects have been observed over zones of water leakage
through fissures in the rock floor of reservoirs, over terrains with
large elevation changes, and in geothermal areas.
8. P t ti l di t ill k l if
Thermoelectric potential
• Potential gradient will appear across a rock sample if a
temperature gradient is maintained across the rock sample.
• Thermoelectric coupling coefficient (TEC) is defined as the ratio of
• Thermoelectric coupling coefficient (TEC) is defined as the ratio of
the voltage to the temperature difference‐‐‐> TEC=∆V/∆T
• TEC values of rocks vary from ‐0 09 to + 1 36 mV/°C
TEC values of rocks vary from 0.09 to + 1.36 mV/ C
average ~ 0.27 mV/°C
• SP generated from TE potentials are of smaller amplitudes than
• SP generated from TE potentials are of smaller amplitudes than
usually seen in geothermal areas.
• More concentrated areas of high temperature at shallow depth,
More concentrated areas of high temperature at shallow depth,
such as thermal fluids in a fault zone, could give rise to anomalies
of greater amplitude.
• Boundaries of SP anomalies measured in several geothermal
areas appear to correlate with zones of known anomalous high
heat flow‐‐‐‐>portion of anomalies is generated by TE mechanism.
9. If th t ti f th l t l t i th d i l ll
Electrochemical potential
• If the concentration of the electrolytes in the ground varies locally,
potential differences are set up due to the difference in mobilities of
anions and cations in solutions of different concentrations‐‐‐called
anions and cations in solutions of different concentrations called
liquid‐junction or diffusion potentials.
• For this mechanism to explain the continued occurrence of such
p
potentials, a source capable of maintaining imbalances in the
electrolytic concentration is needed, otherwise the concentrations
differences will disappear with time by diffusion.
• Electrical potential is also generated when 2 identical metal
l t d i d i l ti f diff t t ti
electrodes are immersed in solutions of different concentrations‐‐‐
called Nernst potential.
• Diffusion + Nernst potentials = Electrochemical or static self
• Diffusion + Nernst potentials = Electrochemical, or static, self‐
potential.
10. O f th t t l l t l t i N Cl
Electrochemical potential
• One of the most common natural electrolytes is NaCl.
• For NaCl solutions of different concentration (C1,C2) but at the same
temperature T (°C) the amplitude of the electrochemical potential
temperature, T ( C), the amplitude of the electrochemical potential
(Ec) is given by
• For example, if C1:C2 = 5:1 ‐‐‐‐‐> Ec ≈ 50 mV
11. i th t i t t i i l l ti f SP i t d ith
Mineral potential
• is the most important in mineral exploration of SP associated with
massive sulphide ore bodies.
• Large negative ( ) SP anomalies (100 1000mV)can be observed
• Large negative (‐) SP anomalies (100‐1000mV)can be observed
particularly over deposits of pyrite, chalcopyrite, pyrrhotite,
magnetite, and graphite.
g , g p
• The potentials are almost invariably negative over the top of the
deposit and are quite stable in time.
• Sato and Mooney (1960) have provided the most complete
explanation of the electrochemical processes caused the observed
SP anomalies.
• However this hypothesis does not explain all the occurrences of the
SP i di h h l h i l li d
SP indicates that the actual physical processes are more complicated
and no yet truly understood.
12.
13. Measurement of Self‐potentials
• simple and inexpensive.
• 2 non‐polarizable porous‐pot electrodes connected to a precision
p p p p
voltmeters capable of measuring to at least 1 mV
• Each electrode is made up of a copper electrode dipped in a
saturated solution of copper sulphate which can percolate through
the porous base to the pot.
• An alternate zinc electrode in saturated zinc sulphate solution or
silver in silver chloride can be used.
Maximum depth of sensitivity of SP method = ~60‐100m depending
b d d t f b d
on ore body and nature of overburden.
15. 2 fi ld t h i 2 l t d fi ti
Measurement of Self‐potentials
2 field techniques or 2 electrode configurations
1.Potential gradient method (dipole/leap frog/gradient configuration)
fi i f 2 l d (5 10 )
‐fix separation of 2 electrodes (5 or 10 m)
‐measure potential difference between 2 electrodes = potential
gradient [mV/V]
gradient [mV/V]
‐2 porous are leap‐frogged along traverse with care of correct polarity
of potential recorded
of potential recorded
‐observation points = midpoint between 2 electrodes
16. Measurement of Self‐potentials
2.Potential amplitude, or total field method (fixed‐base)
configuration
‐keep one electrode fixed at a base station
‐measure potential difference [mV] between base & 2nd
electrodes moving along traverse
‐lower level of cumulative errors & confusing polarity
‐disadvantages of transporting long wire
17. Interpretation of Self‐Potential Data
• SP anomalies are often interpreted qualitatively by
– Profile shape
– Amplitude
– Polarity (+ or ‐)
C
– Contour pattern
• Top of ore body is assumed to lie directly beneath position of
minimum potential
minimum potential.
• For quantitative interpretation, it is possible to calculate the
potential distributions around polarized bodies of simple shape,
potential distributions around polarized bodies of simple shape,
such as sphere, ellipsoid, and dipole, by making some
simplifications and assumptions concerning the potential on the
surface of the sources.
19. SP fil b i d l i d h
SP profiles over buried polarized sphere
20.
21.
22.
23.
24.
25. mV]
SP
[m
SP anomalies generated by buried metal pipelines and well casings at Meso California USA
SP anomalies generated by buried metal pipelines and well casings at Meso, California, USA