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The Evolution of Battery Technology

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The Battery Series
Part 1: The Evolution of Battery Technology

The Battery Series is a five-part infographic series that explores what investors need to know about modern battery technology, including raw material supply, demand, and future applications.

Presented by: Nevada Energy Metals, eCobalt Solutions Inc., and Great Lakes Graphite

The Battery Series - Part 1The Battery Series - Part 2The Battery Series - Part 3The Battery Series - Part 4The Battery Series - Part 5

The Battery Series: The Evolution of Battery Technology

The Battery Series - Part 1The Battery Series - Part 2The Battery Series - Part 3The Battery Series - Part 4The Battery Series - Part 5

Introduction to The Battery Series

Today, how we store energy is just as important as how we create it.

Battery technology already makes electric cars possible, as well as helping us to store emergency power, fly satellites, and use portable electronic devices.

But tomorrow, could you be boarding a battery-powered airplane, or living in a city powered at night by solar energy?

The Battery Series is a five-part infographic series that explores how batteries work, the players in the market, the materials needed to build batteries, and how future battery developments may affect the world. This is Part 1, which looks at the basics of batteries and the history of battery technology.

Sponsors
Nevada Energy Metals
eCobalt Solutions Inc.
Great Lakes Graphite

Battery Basics

Batteries convert stored chemical energy directly into electrical energy. Batteries have three main components:

(-) Anode:The negative electrode that gets oxidized, releasing electrons

(+) Cathode: The positive electrode that is reduced, by acquiring electrons

Electrolyte: The medium that provides the ion transport mechanism between the cathode and anode of a cell. It can be liquid or solid.

At the most basic level, batteries are very simple. In fact, a primitive battery can even be made with a copper penny, galvanized nail (zinc), and a lemon or potato.

The Evolution of Battery Technology

While creating a simple battery is quite easy, the challenge is that making a good battery is very difficult. Balancing power, weight, cost, and other factors involves managing many trade-offs, and scientists have worked for hundreds of years to get to today’s level of efficiency.

Here’s a brief history of how batteries have changed over the years:

Voltaic Pile (1799)

Italian physicist Alessandro Volta, in 1799, created the first electrical battery that could provide continuous electrical current to a circuit. The voltaic pile used zinc and copper for electrodes with brine-soaked paper for an electrolyte.

His invention disproved the common theory that electricity could only be created by living beings.

Daniell Cell (1836)

About 40 years later, a British chemist named John Frederic Daniell would create a new cell that would solve the “hydrogen bubble” problem of the Voltaic pile. This previous problem, in which bubbles collected on the bottom of the zinc electrodes, limited the pile’s lifespan and uses.

The Daniell cell, invented in 1836, used a copper pot filled with copper sulfate solution, which was further immersed in an earthenware container filled with sulfuric acid and a zinc electrode.

The Daniell cell’s electrical potential became the basis unit for voltage, equal to one volt.

Lead-acid (1859)

The lead-acid battery was the first rechargeable battery, invented in 1859 by French physicist Gaston Planté.

Lead-acid batteries excel in two areas: they are very low cost, and they also can supply high surge currents.
This makes them suitable for automobile starter motors even with today’s technology, and it’s part of the reason $44.7 billion of lead-acid batteries were sold globally in 2014.

Nickel Cadmium (1899)

NiCd batteries were invented in 1899 by Waldemar Jungner in Sweden. The first ones were “wet-cells” similar to lead-acid batteries, using a liquid electrolyte.

Nickel Cadmium batteries helped pave the way for modern technology, but they are being used less and less because of cadmium’s toxicity. NiCd batteries lost 80% of their market share in the 1990s to batteries that are more familiar to us today.

Alkaline Batteries (1950s)

Popularized by brands like Duracell and Energizer, alkaline batteries are used in regular household devices from remote controls to flashlights. They are inexpensive and typically non-rechargeable, though they can be made rechargeable by using a specially designed cell.

The modern alkaline battery was invented by Canadian engineer Lewis Urry in the 1950s. Using zinc and manganese oxide in the electrodes, the battery type gets its name from the alkaline electrolyte used: potassium hydroxide.

Over 10 billion alkaline batteries have been made in the world.

Nickel-Metal Hydride (1989)

Similar to the rechargeable NiCd battery, the NiMH formulation uses a hydrogen-absorbing alloy instead of toxic cadmium. This makes it more environmentally safe – and it also helps to increase the energy density.

NiMH batteries are used in power tools, digital cameras, and some other electronic devices. They also were used in early hybrid vehicles such as the Toyota Prius.

The development of the NiMH spanned two decades, and was sponsored by Daimler-Benz and Volkswagen AG. The first commercially available cells were in 1989.

Lithium-Ion (1991)

Sony released the first commercial lithium-ion battery in 1991.

Lithium-ion batteries have high energy density and have a number of specific cathode formulations for different applications.

For example, lithium cobalt dioxide (LiCoO2) cathodes are used in laptops and smartphones, while lithium nickel cobalt aluminum oxide (LiNiCoAlO2) cathodes, also known as NCAs, are used in the batteries of vehicles such as the Tesla Model S.

Graphite is a common material for use in the anode, and the electrolyte is most often a type of lithium salt suspended in an organic solvent.

The Rechargeable Battery Spectrum

There are several factors that could affect battery choice, including cost.

However, here are two of the most important factors that determine the fit and use of rechargeable batteries specifically:

Think of specific energy as in the amount of water in a tank. It’s the amount of energy a battery holds in total.

Meanwhile, specific power is the speed at which that water can pour out of the tank. It’s the amount of current a battery can supply for a given use.

And while today the lithium-ion battery is the workhorse for gadgets and electric vehicles – what batteries will be vital to our future? How big is that market?

Find out in the rest of the Battery Series. (Parts 2 through 5 will be released throughout the summer of 2016).

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Tracking Antarctica Sea Ice Loss in 2023

Antarctica’s ice extent has reached record lows. This visual details and maps Antarctica sea ice loss over the last two years.

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Antarctica sea ice loss tracked from 1979 to 2023

Tracking Antarctica Sea Ice Loss in 2023

Scientists have been tracking the extent and concentrations of Antarctica’s sea ice for decades, and the last two years have raised global alarm bells.

As temperatures are breaking records around the world, the southernmost continent’s ice sheet is visibly smaller than it has been in decades past.

The above graphic uses tracking data from the National Oceanic and Atmospheric Administration (NOAA) and the National Snow and Ice Data Center (NSIDC) to visualize sea ice extent in Antarctica as of August 2023

How Much Ice Has Antarctica Lost?

According to satellite data tracked by the NSIDC, sea ice extent in Antarctica has shrunk to record lows.

When compared to previously charted data dating back to 1979, daily record lows in sea ice extent have been recorded for every day in 2023 so far.

Here is how daily Antarctic sea ice extent in 2023 compares to 2022 (which had many of the previous record lows), and the median from 1981 to 2010.

Date2023 (km²)2022 (km²)Median (1981‒2010, km²)
Aug 2415.87M17.29M17.94M
Aug 2315.79M17.24M17.91M
Aug 2215.74M17.21M17.89M
Aug 2115.69M17.19M17.87M
Aug 2015.64M17.14M17.84M
Aug 1915.55M17.11M17.82M
Aug 1815.45M17.06M17.79M
Aug 1715.34M16.99M17.73M
Aug 1615.22M16.93M17.68M
Aug 1515.12M16.88M17.63M
Aug 1415.07M16.84M17.60M
Aug 1315.04M16.81M17.56M
Aug 1215.02M16.78M17.54M
Aug 1115.00M16.76M17.50M
Aug 1014.98M16.75M17.45M
Aug 0914.96M16.73M17.39M
Aug 0814.95M16.70M17.34M
Aug 0714.92M16.64M17.27M
Aug 0614.88M16.57M17.21M
Aug 0514.86M16.46M17.15M
Aug 0414.82M16.35M17.10M
Aug 0314.78M16.22M17.05M
Aug 0214.75M16.11M17.01M
Aug 0114.69M15.99M16.96M
Jul 3114.62M15.87M16.92M
Jul 3014.55M15.76M16.86M
Jul 2914.47M15.68M16.79M
Jul 2814.38M15.62M16.71M
Jul 2714.29M15.59M16.63M
Jul 2614.21M15.57M16.56M
Jul 2514.16M15.56M16.49M
Jul 2414.10M15.53M16.41M
Jul 2314.03M15.50M16.33M
Jul 2213.97M15.43M16.24M
Jul 2113.91M15.35M16.16M
Jul 2013.82M15.25M16.08M
Jul 1913.70M15.14M16.00M
Jul 1813.58M15.03M15.94M
Jul 1713.45M14.93M15.88M
Jul 1613.31M14.84M15.80M
Jul 1513.17M14.78M15.71M
Jul 1413.07M14.72M15.62M
Jul 1312.98M14.64M15.54M
Jul 1212.88M14.57M15.46M
Jul 1112.77M14.47M15.39M
Jul 1012.65M14.37M15.32M
Jul 0912.54M14.28M15.25M
Jul 0812.43M14.19M15.19M
Jul 0712.36M14.12M15.12M
Jul 0612.32M14.06M15.05M
Jul 0512.31M13.98M14.98M
Jul 0412.28M13.89M14.91M
Jul 0312.22M13.79M14.82M
Jul 0212.14M13.68M14.73M
Jul 0112.06M13.58M14.64M
Jun 3011.96M13.46M14.54M
Jun 2911.87M13.33M14.45M
Jun 2811.81M13.19M14.36M
Jun 2711.75M13.06M14.26M
Jun 2611.68M12.92M14.17M
Jun 2511.61M12.81M14.07M
Jun 2411.53M12.73M13.98M
Jun 2311.46M12.67M13.88M
Jun 2211.39M12.61M13.79M
Jun 2111.31M12.56M13.69M
Jun 2011.21M12.50M13.59M
Jun 1911.10M12.41M13.48M
Jun 1811.02M12.32M13.37M
Jun 1710.92M12.22M13.26M
Jun 1610.84M12.11M13.17M
Jun 1510.78M12.02M13.08M
Jun 1410.73M11.92M12.98M
Jun 1310.66M11.81M12.89M
Jun 1210.61M11.72M12.81M
Jun 1110.54M11.62M12.72M
Jun 1010.46M11.53M12.61M
Jun 0910.39M11.45M12.48M
Jun 0810.33M11.36M12.36M
Jun 0710.26M11.26M12.25M
Jun 0610.18M11.15M12.13M
Jun 0510.09M11.00M12.02M
Jun 049.99M10.87M11.93M
Jun 039.87M10.74M11.84M
Jun 029.75M10.64M11.74M
Jun 019.64M10.58M11.65M
May 319.53M10.54M11.56M
May 309.43M10.49M11.47M
May 299.36M10.43M11.37M
May 289.30M10.35M11.27M
May 279.23M10.27M11.17M
May 269.16M10.20M11.08M
May 259.09M10.14M10.99M
May 248.98M10.07M10.89M
May 238.86M10.01M10.79M
May 228.73M9.94M10.68M
May 218.61M9.85M10.57M
May 208.52M9.76M10.45M
May 198.43M9.66M10.33M
May 188.36M9.56M10.24M
May 178.30M9.46M10.14M
May 168.25M9.34M10.03M
May 158.16M9.20M9.92M
May 148.06M9.09M9.82M
May 137.96M8.99M9.69M
May 127.85M8.88M9.58M
May 117.72M8.77M9.46M
May 107.61M8.67M9.35M
May 097.50M8.55M9.23M
May 087.39M8.40M9.12M
May 077.28M8.26M9.00M
May 067.17M8.13M8.88M
May 057.06M8.02M8.77M
May 046.96M7.91M8.65M
May 036.86M7.80M8.52M
May 026.77M7.69M8.41M
May 016.66M7.59M8.29M
Apr 306.56M7.48M8.17M
Apr 296.48M7.35M8.06M
Apr 286.38M7.24M7.95M
Apr 276.28M7.12M7.83M
Apr 266.19M7.00M7.71M
Apr 256.09M6.86M7.59M
Apr 245.98M6.74M7.48M
Apr 235.89M6.62M7.37M
Apr 225.80M6.50M7.27M
Apr 215.71M6.39M7.18M
Apr 205.64M6.27M7.09M
Apr 195.59M6.15M6.99M
Apr 185.52M6.00M6.88M
Apr 175.45M5.86M6.78M
Apr 165.38M5.73M6.66M
Apr 155.30M5.59M6.55M
Apr 145.19M5.46M6.43M
Apr 135.10M5.33M6.31M
Apr 125.02M5.20M6.18M
Apr 114.94M5.09M6.06M
Apr 104.86M4.97M5.93M
Apr 094.79M4.86M5.81M
Apr 084.71M4.77M5.71M
Apr 074.63M4.68M5.62M
Apr 064.54M4.61M5.53M
Apr 054.46M4.52M5.44M
Apr 044.37M4.42M5.35M
Apr 034.26M4.31M5.27M
Apr 024.16M4.20M5.18M
Apr 014.04M4.06M5.11M
Mar 313.93M3.93M5.04M
Mar 303.86M3.81M4.97M
Mar 293.77M3.68M4.89M
Mar 283.68M3.54M4.81M
Mar 273.57M3.40M4.72M
Mar 263.44M3.28M4.63M
Mar 253.28M3.20M4.54M
Mar 243.14M3.12M4.46M
Mar 233.02M3.06M4.37M
Mar 222.92M3.01M4.28M
Mar 212.84M2.95M4.20M
Mar 202.78M2.88M4.12M
Mar 192.72M2.81M4.03M
Mar 182.66M2.74M3.95M
Mar 172.61M2.68M3.88M
Mar 162.55M2.62M3.80M
Mar 152.49M2.57M3.73M
Mar 142.44M2.52M3.65M
Mar 132.40M2.48M3.59M
Mar 122.34M2.43M3.51M
Mar 112.27M2.39M3.44M
Mar 102.21M2.34M3.37M
Mar 092.13M2.29M3.31M
Mar 082.04M2.24M3.25M
Mar 071.97M2.19M3.20M
Mar 061.93M2.15M3.16M
Mar 051.91M2.11M3.12M
Mar 041.89M2.07M3.07M
Mar 031.88M2.03M3.02M
Mar 021.87M2.01M2.98M
Mar 011.85M1.99M2.94M
Feb 281.83M1.98M2.89M
Feb 271.83M1.98M2.86M
Feb 261.82M1.98M2.83M
Feb 251.82M1.98M2.81M
Feb 241.81M1.98M2.81M
Feb 231.80M1.99M2.81M
Feb 221.79M1.99M2.81M
Feb 211.79M2.02M2.81M
Feb 201.81M2.03M2.82M
Feb 191.82M2.05M2.82M
Feb 181.85M2.08M2.84M
Feb 171.86M2.11M2.86M
Feb 161.88M2.14M2.89M
Feb 151.88M2.18M2.93M
Feb 141.89M2.22M2.97M
Feb 131.91M2.24M3.02M
Feb 121.93M2.26M3.06M
Feb 111.96M2.31M3.10M
Feb 101.98M2.35M3.15M
Feb 092.01M2.41M3.20M
Feb 082.03M2.47M3.25M
Feb 072.06M2.54M3.30M
Feb 062.09M2.60M3.36M
Feb 052.12M2.66M3.41M
Feb 042.16M2.71M3.47M
Feb 032.19M2.77M3.52M
Feb 022.23M2.82M3.57M
Feb 012.26M2.86M3.63M
Jan 312.30M2.89M3.68M
Jan 302.35M2.94M3.73M
Jan 292.42M2.99M3.78M
Jan 282.48M3.04M3.84M
Jan 272.56M3.11M3.89M
Jan 262.65M3.19M3.96M
Jan 252.71M3.26M4.04M
Jan 242.78M3.34M4.12M
Jan 232.85M3.41M4.18M
Jan 222.90M3.48M4.26M
Jan 212.96M3.57M4.34M
Jan 203.02M3.66M4.42M
Jan 193.09M3.75M4.51M
Jan 183.17M3.87M4.62M
Jan 173.24M3.96M4.73M
Jan 163.32M4.05M4.87M
Jan 153.39M4.13M5.01M
Jan 143.45M4.20M5.14M
Jan 133.51M4.27M5.27M
Jan 123.59M4.38M5.41M
Jan 113.67M4.49M5.54M
Jan 103.76M4.59M5.69M
Jan 093.86M4.70M5.85M
Jan 083.97M4.83M6.02M
Jan 074.09M4.95M6.18M
Jan 064.22M5.09M6.34M
Jan 054.35M5.27M6.51M
Jan 044.49M5.45M6.67M
Jan 034.64M5.62M6.84M
Jan 024.79M5.82M7.01M
Jan 015.00M6.02M7.19M

Antarctica’s sea ice extent on August 24, 2023 was 1.42 million square kilometers smaller than the year before. When compared to the median extent for that date from 1980 to 2010, it was 2.07 million square kilometers smaller.

Keep in mind that July and August are the coldest months in Antarctica. Its position on the South Pole gives it a very long winter ranging from the end of February to the end of September, with ice building up before melting temperatures arrive in October.

Antarctica Sea Ice and the Rest of the World

Even though the continent is thousands of kilometers from most of Earth’s land and populace, its ice has an important impact on the rest of the planet.

Antarctica’s large ice sheet is able to reflect a lot of sunlight in sunnier months, reducing the amount absorbed by the ocean. The wider its extent builds up over the winter, the more sunlight and heat it is able to reflect.

It’s also important to consider that this ice comes from a regular pattern of freezing and melting ocean water. The more ice is lost to the oceans compared to what accumulates in a given year, the higher sea levels rise around the world.

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