Using CO2 to Extract Geothermal Energy

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Move over CO2—you’ve been ousted, along with methane, as the biggest offenders of global climate change. According to a new a study by Purdue University and NASA, the major chemicals most frequently cited as leading to climate change, namely carbon dioxide and methane, are actually outclassed in their warming potential by compounds receiving less attention. The majority of “greenhouse gases” are created by humans.

The results were discovered when researchers studied more than a dozen chemicals, or greenhouse gases as classified by their warming properties defined by the Intergovernmental Panel on Climate Change. From there, the team developed a blueprint for the underlying molecular machinery of global warming. The results appeared in the November 12, 2009 issue of the American Chemical Society’s Journal of Physical Chemistry, just in time for the convergence of world leaders in Copenhagen.

Maybe more amazing than the fact that we now have a global warming blueprint is that no one else has ever before mapped climate change; yet the U.S. is in the midst of passing global climate change policy. The original hope was to have legislation in place prior to Copenhagen but in the spirit of American politics, Republicans and Democrats can’t agree on one policy—the Republicans are supporting the Waxman-Markey Bill and the Democrats are pushing the Kerry-Boxer Bill.

The Purdue/NASA study combined results from experimental observations along with computer modeling. The goal of the project was to determine which chemical and physical properties are most detrimental in causing global warming.

It turns out that the compounds, which contain fluorine atoms, are far more efficient at blocking radiation in the “atmospheric window,” according to Purdue chemistry and earth and atmospheric sciences professor Joseph Francisco, a study co-author. NASA scientist Timothy Lee was lead author of the study with Francisco and NASA postdoctoral fellow Partha Bera.

Francisco explains that the atmospheric window is the frequency in the infrared region through which radiation from Earth is released into space, helping to cool the planet. When the heat is trapped rather than released, a “greenhouse effect” occurs, and the planet becomes warmer. The majority of the chemicals that cause heat to be trapped are used by industries worldwide.

Based on the ability to trap radiation in the atmospheric window, chemicals such as sulfur and nitrogen flourides, perfluorocarbons (PFCs), hydrofluorocarbons (HFCs), and chlorofluorocarbons (CFCs) stand out. Chemicals like CO2, while harmful, don’t close the atmospheric window as quickly as these other compounds making them more dangerous.

“It’s actually rather stark,” said Francisco, “but an understanding of how the chemicals contribute to climate change on a molecular scale affords the opportunity to create benign alternatives and to test new chemicals for their global warming capability before they go to market.”

“Now you have a rational design basis,” he said.

Not sure what some of these are? Stop using aerosol cans. CFC use has decreased with the discovery that they lead to the destruction of the ozone layer. However, HFCs and PFCs are widely used in air conditioning and in the manufacturing of carpets, appliances and electronics.

The study notes that, “Although current concentrations of some of these trace gases have been found to be substantially small compared to carbon dioxide, their concentration is on the rise. With the current rate of increase, they will be important contributors in the future, according to some models.”

So CO2 and methane are not in fact the worst chemicals, but fluorine-containing compounds are actually the worst. In addition, according to Lee, “The compounds also persist longer than carbon dioxide and other major global warming agents. The concern is that, even if emitted into the atmosphere in lower quantities, the chemicals might have a powerful cumulative effect over time. Some of these chemicals don’t break down for thousands of years.”

Well I sure hope that the auto industry is working in tandem with technology companies to replace these chemicals because I’d really like to keep my air conditioning… and car stereo… and TV…

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Move over CO2—you’ve been ousted, along with methane, as the biggest offenders of global climate change. According to a new a study by Purdue University and NASA, the major chemicals most frequently cited as leading to climate change, namely carbon dioxide and methane, are actually outclassed in their warming potential by compounds receiving less attention. The majority of “greenhouse gases” are created by humans.

The results were discovered when researchers studied more than a dozen chemicals, or greenhouse gases as classified by their warming properties defined by the Intergovernmental Panel on Climate Change. From there, the team developed a blueprint for the underlying molecular machinery of global warming. The results appeared in the November 12, 2009 issue of the American Chemical Society’s Journal of Physical Chemistry, just in time for the convergence of world leaders in Copenhagen.

Maybe more amazing than the fact that we now have a global warming blueprint is that no one else has ever before mapped climate change; yet the U.S. is in the midst of passing global climate change policy. The original hope was to have legislation in place prior to Copenhagen but in the spirit of American politics, Republicans and Democrats can’t agree on one policy—the Republicans are supporting the Waxman-Markey Bill and the Democrats are pushing the Kerry-Boxer Bill.

The Purdue/NASA study combined results from experimental observations along with computer modeling. The goal of the project was to determine which chemical and physical properties are most detrimental in causing global warming.

It turns out that the compounds, which contain fluorine atoms, are far more efficient at blocking radiation in the “atmospheric window,” according to Purdue chemistry and earth and atmospheric sciences professor Joseph Francisco, a study co-author. NASA scientist Timothy Lee was lead author of the study with Francisco and NASA postdoctoral fellow Partha Bera.

Francisco explains that the atmospheric window is the frequency in the infrared region through which radiation from Earth is released into space, helping to cool the planet. When the heat is trapped rather than released, a “greenhouse effect” occurs, and the planet becomes warmer. The majority of the chemicals that cause heat to be trapped are used by industries worldwide.

Based on the ability to trap radiation in the atmospheric window, chemicals such as sulfur and nitrogen flourides, perfluorocarbons (PFCs), hydrofluorocarbons (HFCs), and chlorofluorocarbons (CFCs) stand out. Chemicals like CO2, while harmful, don’t close the atmospheric window as quickly as these other compounds making them more dangerous.

“It’s actually rather stark,” said Francisco, “but an understanding of how the chemicals contribute to climate change on a molecular scale affords the opportunity to create benign alternatives and to test new chemicals for their global warming capability before they go to market.”

“Now you have a rational design basis,” he said.

Not sure what some of these are? Stop using aerosol cans. CFC use has decreased with the discovery that they lead to the destruction of the ozone layer. However, HFCs and PFCs are widely used in air conditioning and in the manufacturing of carpets, appliances and electronics.

The study notes that, “Although current concentrations of some of these trace gases have been found to be substantially small compared to carbon dioxide, their concentration is on the rise. With the current rate of increase, they will be important contributors in the future, according to some models.”

So CO2 and methane are not in fact the worst chemicals, but fluorine-containing compounds are actually the worst. In addition, according to Lee, “The compounds also persist longer than carbon dioxide and other major global warming agents. The concern is that, even if emitted into the atmosphere in lower quantities, the chemicals might have a powerful cumulative effect over time. Some of these chemicals don’t break down for thousands of years.”

Well I sure hope that the auto industry is working in tandem with technology companies to replace these chemicals because I’d really like to keep my air conditioning… and car stereo… and TV…

Start uga_filter:

The oceans play a key role in regulating climate, absorbing more than a quarter of the carbon dioxide that humans put into the air. Now, the first year-by-year accounting of this mechanism during the industrial era suggests the oceans are struggling to keep up with rising emissions — a finding with potentially wide implications for future climate. The study appears in the November 19 issue of the journalNature.

The researchers estimate that the oceans last year took up a record 2.3 billion tons of CO2 produced from burning of fossil fuels. But with overall emissions growing rapidly, the proportion of fossil-fuel emissions absorbed by the oceans since 2000 may have declined by as much as 10%.

Some climate models have already predicted such a slowdown in the oceans’ ability to soak up excess carbon from the atmosphere, but this is the first time scientists have actually measured it. Models attribute the change to depletion of ozone in the stratosphere and global warming-induced shifts in winds and ocean circulation. But the new study suggests the slowdown is due to natural chemical and physical limits on the oceans’ ability to absorb carbon — an idea that is now the subject of widespread research by other scientists.

“The more carbon dioxide you put in, the more acidic the ocean becomes, reducing its ability to hold CO2” said the study’s lead author, Samar Khatiwala, an oceanographer at Columbia University’s Lamont-Doherty Earth Observatory. “Because of this chemical effect, over time, the ocean is expected to become a less efficient sink of manmade carbon. The surprise is that we may already be seeing evidence for this, perhaps compounded by the ocean’s slow circulation in the face of accelerating emissions.”

The study reconstructs the accumulation of industrial carbon in the oceans year by year, from 1765 to 2008. Khatiwala and his colleagues found that uptake rose sharply in the 1950s, as the oceans tried to keep pace with the growth of carbon dioxide emissions worldwide. Emissions continued to grow, and by 2000, reached such a pitch that the oceans have since absorbed a declining overall percentage, even though they absorb more each year in absolute tonnage. Today, the oceans hold about 150 billion tons of industrial carbon, the researchers estimate–a third more than in the mid-1990s.

For decades, scientists have tried to estimate the amount of manmade carbon absorbed by the ocean by teasing out the small amount of industrial carbon — less than 1 percent — from the enormous background levels of natural carbon. Because of the difficulties of this approach, only one attempt has been made to come up with a global estimate of how much industrial carbon the oceans held — for a single year, 1994.

Khatiwala and his colleagues came up with another method. Using some of the same data as their predecessors — seawater temperatures, salinity, manmade chlorofluorocarbons and other measures — they developed a mathematical technique to work backward from the measurements to infer the concentration of industrial carbon in surface waters, and its transport to deep water through ocean circulation. This allowed them to reconstruct the uptake and distribution of industrial carbon in the oceans over time.

Their estimate of industrial carbon in the oceans in 1994 — 114 billion tons — nearly matched the earlier 118 billion-ton estimate, made by Chris Sabine, a marine chemist at the National Oceanic and Atmospheric Organization in a 2004 paper in the journal Science.

Sabine, who was not involved in the new study, said he saw some limitations. For one, he said, the study assumes circulation has remained steady, along with the amount of organic matter in the oceans. “That being said, I still think this is the best estimate of the time variance of anthropogenic CO2 in the ocean available,” said Sabine. “Our previous attempts to quantify anthropogenic CO2 using ocean data have only been able to provide single snapshots in time.”

About 40 percent of the carbon entered the oceans through the frigid waters of the Southern Ocean, around Antarctica, because carbon dioxide dissolves more readily in cold, dense seawater than in warmer waters. From there, currents transport the carbon north. “We’ve suspected for some time that the Southern Ocean plays a critical role in soaking up fossil fuel CO2,” said Khatiwala. “But our study is the first to quantify the importance of this region with actual data.”

The researchers also estimated carbon uptake on land, by taking the known amount of fossil-fuel emissions and subtracting the oceans’ uptake and the carbon left in the air. They were surprised to learn that the land may now be absorbing more than it is giving off.

They say that until the 1940s, the landscape produced excess carbon dioxide, possibly due to logging and the clearing and burning of forests for farming. Deforestation and other land-use changes continue at a rapid pace today — but now, each year the land appears to be absorbing 1.1 billion tons more carbon than it is giving off.

One possible reason for the reversal, say the researchers, is that now, some of the extra atmospheric carbon — raw material for photosynthesis–may be feeding back into living plants and making them grow faster. “The extra carbon dioxide in the atmosphere may be providing a fertilizing effect,” said study coauthor Timothy Hall, a senior scientist at NASA’s Goddard Institute for Space Studies. Many other scientists are now working to determine the possible effects of increased carbon dioxide on plant growth, and incorporate these into models of past and future climates.

Khatiwala says there are still large uncertainties, but in any case, natural mechanisms cannot be depended upon to mitigate increasing human-produced emissions. “What our ocean study and other recent land studies suggest is that we cannot count on these sinks operating in the future as they have in the past, and keep on subsidizing our ever-growing appetite for fossil fuels,” he said.

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The oceans play a key role in regulating climate, absorbing more than a quarter of the carbon dioxide that humans put into the air. Now, the first year-by-year accounting of this mechanism during the industrial era suggests the oceans are struggling to keep up with rising emissions — a finding with potentially wide implications for future climate. The study appears in the November 19 issue of the journalNature.

The researchers estimate that the oceans last year took up a record 2.3 billion tons of CO2 produced from burning of fossil fuels. But with overall emissions growing rapidly, the proportion of fossil-fuel emissions absorbed by the oceans since 2000 may have declined by as much as 10%.

Some climate models have already predicted such a slowdown in the oceans’ ability to soak up excess carbon from the atmosphere, but this is the first time scientists have actually measured it. Models attribute the change to depletion of ozone in the stratosphere and global warming-induced shifts in winds and ocean circulation. But the new study suggests the slowdown is due to natural chemical and physical limits on the oceans’ ability to absorb carbon — an idea that is now the subject of widespread research by other scientists.

“The more carbon dioxide you put in, the more acidic the ocean becomes, reducing its ability to hold CO2” said the study’s lead author, Samar Khatiwala, an oceanographer at Columbia University’s Lamont-Doherty Earth Observatory. “Because of this chemical effect, over time, the ocean is expected to become a less efficient sink of manmade carbon. The surprise is that we may already be seeing evidence for this, perhaps compounded by the ocean’s slow circulation in the face of accelerating emissions.”

The study reconstructs the accumulation of industrial carbon in the oceans year by year, from 1765 to 2008. Khatiwala and his colleagues found that uptake rose sharply in the 1950s, as the oceans tried to keep pace with the growth of carbon dioxide emissions worldwide. Emissions continued to grow, and by 2000, reached such a pitch that the oceans have since absorbed a declining overall percentage, even though they absorb more each year in absolute tonnage. Today, the oceans hold about 150 billion tons of industrial carbon, the researchers estimate–a third more than in the mid-1990s.

For decades, scientists have tried to estimate the amount of manmade carbon absorbed by the ocean by teasing out the small amount of industrial carbon — less than 1 percent — from the enormous background levels of natural carbon. Because of the difficulties of this approach, only one attempt has been made to come up with a global estimate of how much industrial carbon the oceans held — for a single year, 1994.

Khatiwala and his colleagues came up with another method. Using some of the same data as their predecessors — seawater temperatures, salinity, manmade chlorofluorocarbons and other measures — they developed a mathematical technique to work backward from the measurements to infer the concentration of industrial carbon in surface waters, and its transport to deep water through ocean circulation. This allowed them to reconstruct the uptake and distribution of industrial carbon in the oceans over time.

Their estimate of industrial carbon in the oceans in 1994 — 114 billion tons — nearly matched the earlier 118 billion-ton estimate, made by Chris Sabine, a marine chemist at the National Oceanic and Atmospheric Organization in a 2004 paper in the journal Science.

Sabine, who was not involved in the new study, said he saw some limitations. For one, he said, the study assumes circulation has remained steady, along with the amount of organic matter in the oceans. “That being said, I still think this is the best estimate of the time variance of anthropogenic CO2 in the ocean available,” said Sabine. “Our previous attempts to quantify anthropogenic CO2 using ocean data have only been able to provide single snapshots in time.”

About 40 percent of the carbon entered the oceans through the frigid waters of the Southern Ocean, around Antarctica, because carbon dioxide dissolves more readily in cold, dense seawater than in warmer waters. From there, currents transport the carbon north. “We’ve suspected for some time that the Southern Ocean plays a critical role in soaking up fossil fuel CO2,” said Khatiwala. “But our study is the first to quantify the importance of this region with actual data.”

The researchers also estimated carbon uptake on land, by taking the known amount of fossil-fuel emissions and subtracting the oceans’ uptake and the carbon left in the air. They were surprised to learn that the land may now be absorbing more than it is giving off.

They say that until the 1940s, the landscape produced excess carbon dioxide, possibly due to logging and the clearing and burning of forests for farming. Deforestation and other land-use changes continue at a rapid pace today — but now, each year the land appears to be absorbing 1.1 billion tons more carbon than it is giving off.

One possible reason for the reversal, say the researchers, is that now, some of the extra atmospheric carbon — raw material for photosynthesis–may be feeding back into living plants and making them grow faster. “The extra carbon dioxide in the atmosphere may be providing a fertilizing effect,” said study coauthor Timothy Hall, a senior scientist at NASA’s Goddard Institute for Space Studies. Many other scientists are now working to determine the possible effects of increased carbon dioxide on plant growth, and incorporate these into models of past and future climates.

Khatiwala says there are still large uncertainties, but in any case, natural mechanisms cannot be depended upon to mitigate increasing human-produced emissions. “What our ocean study and other recent land studies suggest is that we cannot count on these sinks operating in the future as they have in the past, and keep on subsidizing our ever-growing appetite for fossil fuels,” he said.

Start uga_filter:

As part of developing new energy resources that don’t emit carbon dioxide, the DOE is funding 9 trials that use supercritical CO2 to extract more geothermal energy.


The idea started in 2000 at Los Alamos National Laboratory; when physicist Donald Brown thought of pumping geothermal fluid using supercritical CO2 – a pressurized form that is part gas, part liquid; instead of water.  Theoretically this should flow more freely through rock than water, because it is less viscous than water.

Then, six years later; in modeling the technology Lawrence Berkeley hydro-geologist Karsten Pruess projected that not only should it perform as expected but that it would also yield a 50% hotter geothermal resource.

Now the DOE is funding this promising research with $16 million in nine trials to see if this will work in the real world.

The funding is to be shared by nine carbon dioxide-related projects led by Lawrence Berkeley National Laboratory and other national labs and universities, and the Californian combinatorial chemistry firm Symyx Technologies that screens about a million potential materials a year using advanced computer modeling.

Brown’s idea was that the density difference between the supercritical CO2 pumped down and the hotter gas coming up would make the gas cycle better by a siphoning action, so the pumping process would use less energy.

Symyx project leader and materials scientist Miroslav Petro wants to make sure that supercritical carbon dioxide plays nicely with rock and minerals. It could form a super-dissolving “acidic soda water” that dissolves minerals from rocks.

Sequestering the carbon would be the big bonus. It could be a large amount: 70 years worth of CO2 emissions from a 500 megawatt coal power plant.

Written by Susan Kraemer

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As part of developing new energy resources that don’t emit carbon dioxide, the DOE is funding 9 trials that use supercritical CO2 to extract more geothermal energy.


The idea started in 2000 at Los Alamos National Laboratory; when physicist Donald Brown thought of pumping geothermal fluid using supercritical CO2 – a pressurized form that is part gas, part liquid; instead of water.  Theoretically this should flow more freely through rock than water, because it is less viscous than water.

Then, six years later; in modeling the technology Lawrence Berkeley hydro-geologist Karsten Pruess projected that not only should it perform as expected but that it would also yield a 50% hotter geothermal resource.

Now the DOE is funding this promising research with $16 million in nine trials to see if this will work in the real world.

The funding is to be shared by nine carbon dioxide-related projects led by Lawrence Berkeley National Laboratory and other national labs and universities, and the Californian combinatorial chemistry firm Symyx Technologies that screens about a million potential materials a year using advanced computer modeling.

Brown’s idea was that the density difference between the supercritical CO2 pumped down and the hotter gas coming up would make the gas cycle better by a siphoning action, so the pumping process would use less energy.

Symyx project leader and materials scientist Miroslav Petro wants to make sure that supercritical carbon dioxide plays nicely with rock and minerals. It could form a super-dissolving “acidic soda water” that dissolves minerals from rocks.

Sequestering the carbon would be the big bonus. It could be a large amount: 70 years worth of CO2 emissions from a 500 megawatt coal power plant.

Written by Susan Kraemer

Start uga_wp_footer_track: Start uga_get_tracker Start uga_in_feed Ending uga_in_feed: Start uga_track_user Start uga_get_option: ignore_users uga_options: array ( 'internal_domains' => 'www.humacon.org,humacon.org', 'account_id' => 'UA-10399907-2', 'enable_tracker' => true, 'track_adm_pages' => false, 'ignore_users' => true, 'max_user_level' => '8', 'footer_hooked' => true, 'filter_content' => true, 'filter_comments' => true, 'filter_comment_authors' => true, 'track_ext_links' => true, 'prefix_ext_links' => '/outgoing/', 'track_files' => true, 'prefix_file_links' => '/downloads/', 'track_extensions' => 'gif,jpg,jpeg,bmp,png,pdf,mp3,wav,phps,zip,gz,tar,rar,jar,exe,pps,ppt,xls,doc', 'track_mail_links' => true, 'prefix_mail_links' => '/mailto/', 'debug' => true, 'check_updates' => true, 'version_sent' => '1.6.0', 'advanced_config' => true, ) Ending uga_get_option: ignore_users (1) Start uga_get_option: max_user_level uga_options: array ( 'internal_domains' => 'www.humacon.org,humacon.org', 'account_id' => 'UA-10399907-2', 'enable_tracker' => true, 'track_adm_pages' => false, 'ignore_users' => true, 'max_user_level' => '8', 'footer_hooked' => true, 'filter_content' => true, 'filter_comments' => true, 'filter_comment_authors' => true, 'track_ext_links' => true, 'prefix_ext_links' => '/outgoing/', 'track_files' => true, 'prefix_file_links' => '/downloads/', 'track_extensions' => 'gif,jpg,jpeg,bmp,png,pdf,mp3,wav,phps,zip,gz,tar,rar,jar,exe,pps,ppt,xls,doc', 'track_mail_links' => true, 'prefix_mail_links' => '/mailto/', 'debug' => true, 'check_updates' => true, 'version_sent' => '1.6.0', 'advanced_config' => true, ) Ending uga_get_option: max_user_level (8) Tracking user with level 0 Ending uga_track_user: 1 Start uga_get_option: account_id uga_options: array ( 'internal_domains' => 'www.humacon.org,humacon.org', 'account_id' => 'UA-10399907-2', 'enable_tracker' => true, 'track_adm_pages' => false, 'ignore_users' => true, 'max_user_level' => '8', 'footer_hooked' => true, 'filter_content' => true, 'filter_comments' => true, 'filter_comment_authors' => true, 'track_ext_links' => true, 'prefix_ext_links' => '/outgoing/', 'track_files' => true, 'prefix_file_links' => '/downloads/', 'track_extensions' => 'gif,jpg,jpeg,bmp,png,pdf,mp3,wav,phps,zip,gz,tar,rar,jar,exe,pps,ppt,xls,doc', 'track_mail_links' => true, 'prefix_mail_links' => '/mailto/', 'debug' => true, 'check_updates' => true, 'version_sent' => '1.6.0', 'advanced_config' => true, ) Ending uga_get_option: account_id (UA-10399907-2) Ending uga_get_tracker: Start uga_insert_html_once: footer, Footer hooked: HTML inserted: Location is FOOTER Inserting HTML End uga_insert_html Ending uga_wp_footer_track: Start uga_shutdown Start uga_in_feed Ending uga_in_feed: Start uga_track_user Start uga_get_option: ignore_users uga_options: array ( 'internal_domains' => 'www.humacon.org,humacon.org', 'account_id' => 'UA-10399907-2', 'enable_tracker' => true, 'track_adm_pages' => false, 'ignore_users' => true, 'max_user_level' => '8', 'footer_hooked' => true, 'filter_content' => true, 'filter_comments' => true, 'filter_comment_authors' => true, 'track_ext_links' => true, 'prefix_ext_links' => '/outgoing/', 'track_files' => true, 'prefix_file_links' => '/downloads/', 'track_extensions' => 'gif,jpg,jpeg,bmp,png,pdf,mp3,wav,phps,zip,gz,tar,rar,jar,exe,pps,ppt,xls,doc', 'track_mail_links' => true, 'prefix_mail_links' => '/mailto/', 'debug' => true, 'check_updates' => true, 'version_sent' => '1.6.0', 'advanced_config' => true, ) Ending uga_get_option: ignore_users (1) Start uga_get_option: max_user_level uga_options: array ( 'internal_domains' => 'www.humacon.org,humacon.org', 'account_id' => 'UA-10399907-2', 'enable_tracker' => true, 'track_adm_pages' => false, 'ignore_users' => true, 'max_user_level' => '8', 'footer_hooked' => true, 'filter_content' => true, 'filter_comments' => true, 'filter_comment_authors' => true, 'track_ext_links' => true, 'prefix_ext_links' => '/outgoing/', 'track_files' => true, 'prefix_file_links' => '/downloads/', 'track_extensions' => 'gif,jpg,jpeg,bmp,png,pdf,mp3,wav,phps,zip,gz,tar,rar,jar,exe,pps,ppt,xls,doc', 'track_mail_links' => true, 'prefix_mail_links' => '/mailto/', 'debug' => true, 'check_updates' => true, 'version_sent' => '1.6.0', 'advanced_config' => true, ) Ending uga_get_option: max_user_level (8) Tracking user with level 0 Ending uga_track_user: 1 Footer hook was executed Start uga_get_option: footer_hooked uga_options: array ( 'internal_domains' => 'www.humacon.org,humacon.org', 'account_id' => 'UA-10399907-2', 'enable_tracker' => true, 'track_adm_pages' => false, 'ignore_users' => true, 'max_user_level' => '8', 'footer_hooked' => true, 'filter_content' => true, 'filter_comments' => true, 'filter_comment_authors' => true, 'track_ext_links' => true, 'prefix_ext_links' => '/outgoing/', 'track_files' => true, 'prefix_file_links' => '/downloads/', 'track_extensions' => 'gif,jpg,jpeg,bmp,png,pdf,mp3,wav,phps,zip,gz,tar,rar,jar,exe,pps,ppt,xls,doc', 'track_mail_links' => true, 'prefix_mail_links' => '/mailto/', 'debug' => true, 'check_updates' => true, 'version_sent' => '1.6.0', 'advanced_config' => true, ) Ending uga_get_option: footer_hooked (1) Start uga_get_option: debug uga_options: array ( 'internal_domains' => 'www.humacon.org,humacon.org', 'account_id' => 'UA-10399907-2', 'enable_tracker' => true, 'track_adm_pages' => false, 'ignore_users' => true, 'max_user_level' => '8', 'footer_hooked' => true, 'filter_content' => true, 'filter_comments' => true, 'filter_comment_authors' => true, 'track_ext_links' => true, 'prefix_ext_links' => '/outgoing/', 'track_files' => true, 'prefix_file_links' => '/downloads/', 'track_extensions' => 'gif,jpg,jpeg,bmp,png,pdf,mp3,wav,phps,zip,gz,tar,rar,jar,exe,pps,ppt,xls,doc', 'track_mail_links' => true, 'prefix_mail_links' => '/mailto/', 'debug' => true, 'check_updates' => true, 'version_sent' => '1.6.0', 'advanced_config' => true, ) Ending uga_get_option: debug (1) -->