Dangers Of Global Warming

Friday, August 5, 2011

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Global Warming - Burning My Iceland

Living on a tropical island, is quite unique. If you love the natural world, there are many things you could do it. I grew up in a small valley in the hills south of my island and I have known my whole life.

Field trips to a pretty fast pace of the canyon hills hundred meters is all worth it when I have to choose a place near the top only. It is a true blessing to be able to do. It is a wonderful job, too. The tops of steep hills to near the base is covered by savannah grasslands. The very steep slopes and along its base are wooded ravine. More than jungle delirium. If you look in the mountains in the distance, are the golden color of the meadows a great contrast to the dark green jungle hills. It is amazing to know how my mind that a hundred years ago, almost all of these dark hills. Jungles all the way up. Wow. And one reason why not.

Fire was a tool for humans used almost since its discovery. He also has done before. And one of the biggest weapons for hunting deer has become here in the jungles of the south. What they do is a fire. Just set a fire the flame and let it rip. Help if you would have difficulties. For once it's gone and burning in arable soil, a wonderful thing called life happens next. New shoots of grass from the hills and burned black. And the deer is probably a surprise, because they consume these tender buds. The wild hunter waits.

Oh, but all the other things that there was kindled a fire in the hills happened. Surely this is not the arsonist would have thought about it. Let us straight in the direction that things go happen. The fire is determined and set on fire. The atmosphere is the first hit. A powerful greenhouse gas (carbon dioxide), a by-product of combustion of vegetation is directly exposed to the atmosphere. But wait. We do not really feel their effects for a long time. No, not right. Global warming. Exactly. It is not surprising that the collective memory of vegetation in the world is still a significant contribution to global warming? his strike.

While in the flames, a fire are often lost in a jungle. The fire will stop, right? That is true. The last time. But the fire will not die once they walk into the jungle. He has to burn its way into a little "to run into the water and most of the jungle. You know, it will take at least one meter. Do burnout. So how can you burn burn, walking to the size of forests . The more you burn, the less the jungle. Strike two.

Now, the fire died and the hills are bare. When the rain comes, and then the soil to wash away. I have never burned washed flee a hill by the rain. Soil erosion by sedimentation in water. But that does not matter. The ocean is big. Will not hurt. In the grand scheme of the oceans, not too much. For aquatic life in rivers, coral, and the open sea populations that feed and live on these reefs, the damage is absolutely fatal. Strike three.

Add all. We have professionals on the one hand, the shot immediately after a new fire is enticing deer. It would be easier to catch. And only useful for the hunter. We are opposite on the other side, and the list is impressive.

- The air in our atmosphere gets an infusion of a potent greenhouse gas that contributes to global warming. We know without doubt that large and persistent global warming has caused and is accelerating, climate change may very well end our day.

- It is the country. Our lower jungle. This quickly leads to loss of habitat for animals. The bright green jungle of our gold and the sea of our savannas are burned from the hills of text and black. All animals, nests or caves caught fire, food, well, that's just their loss. And if it rains, we lose our topsoil. The roots in the city, burned clean. accelerated soil erosion, I despise. .

- It is the sea, rivers are included. Immediately after the soil erosion is the effect of sedimentation. This transported soil spreading. And blankets and suffocates when it finally stabilized. Sedimentation is the bearer of death for microscopic organisms, plants, fish and corals, to say the least. In the aquatic environment, is the destruction of large and extended. Imagine that your air is filled with the ashes of all time. What would be the quality of your life, what then?

He has about 700 million tons of carbon dioxide into the atmosphere every day. There is no doubt, no debate. A large percentage comes from the constant reminder of the natural landscape. We have to change the way they do things.

The survival of our race, have to stop global warming. Climate change in progress should be maintained, if not reversed. If we refuse to realize this, it will matter in fifty or a hundred years? Spread the word. Take part. We can still save.

Wednesday, August 3, 2011

Ozone Improves Biofuel Production Efficiency






It is of some interest that direct application of ozone degrades the lignin allowing the carbohydrates to be attacked and converted to sugars.  It will not be easy, but it opens another avenue.

Ozone is a bit tricky to produce and expensive and may well limit this method to the laboratory.

However, a process protocol that starts and ends dry is a rather good beginning and leaves a lot of options open for further treatment and no immediate waste stream.

A friend of mine has been testing ozone on ores to some effect, so this is not too surprising.


New Technique Improves Efficiency Of Biofuel Production

by Staff Writers

Raleigh NC (SPX) Jul 06, 2010



Researchers at North Carolina State University have developed a more efficient technique for producing biofuels from woody plants that significantly reduces the waste that results from conventional biofuel production techniques. The technique is a significant step toward creating a commercially viable new source of biofuels.

"This technique makes the process more efficient and less expensive," says Dr. Ratna Sharma-Shivappa, associate professor of biological and agricultural engineering at NC State and co-author of the research. "The technique could open the door to making lignin-rich plant matter a commercially viable feedstock for biofuels, curtailing biofuel's reliance on staple food crops."

Traditionally, to make ethanol, butanol or other biofuels, producers have used corn, beets or other plant matter that is high in starches or simple sugars. However, since those crops are also significant staple foods, biofuels are competing with people for those crops.

However, other forms of biomass - such as switchgrass or inedible corn stalks - can also be used to make biofuels. But these other crops pose their own problem: their energy potential is locked away inside the plant's lignin - the woody, protective material that provides each plant's structural support.
Breaking down that lignin to reach the plant's component carbohydrates is an essential first step toward making biofuels.

At present, researchers exploring how to create biofuels from this so-called "woody" material treat the plant matter with harsh chemicals that break it down into a carbohydrate-rich substance and a liquid waste stream. These carbohydrates are then exposed to enzymes that turn the carbohydrates into sugars that can be fermented to make ethanol or butanol.

This technique often results in a significant portion of the plant's carbohydrates being siphoned off with the liquid waste stream. Researchers must either incorporate additional processes to retrieve those carbohydrates, or lose them altogether.

But now researchers from NC State have developed a new way to free the carbohydrates from the lignin. By exposing the plant matter to gaseous ozone, with very little moisture, they are able to produce a carbohydrate-rich solid with no solid or liquid waste.

"This is more efficient because it degrades the lignin very effectively and there is little or no loss of the plant's carbohydrates," Sharma-Shivappa says. "The solid can then go directly to the enzymes to produce the sugars necessary for biofuel production."

Sharma notes that the process itself is more expensive than using a bath of harsh chemicals to free the carbohydrates, but is ultimately more cost-effective because it makes more efficient use of the plant matter.

The researchers have recently received a grant from the Center for Bioenergy Research and Development to fine-tune the process for use with switchgrass and miscanthus grass. "Our eventual goal is to use this technique for any type of feedstock, to produce any biofuel or biochemical that can use these sugars," Sharma-Shivappa says.

The research, "Effect of ozonolysis on bioconversion of miscanthus to bioethanol," was co-authored by Sharma-Shivappa, NC State Ph.D. student Anushadevi Panneerselvam, Dr. Praveen Kolar, an assistant professor of biological and agricultural engineering at NC State, Dr. Thomas Ranney, a professor of horticultural science at NC State, and Dr. Steve Peretti, an associate professor of chemical and biomolecular engineering at NC State.

The research is partially funded by the Biofuels Center of North Carolina and was presented June 23 at the 2010 Annual International Meeting of the American Society for Agricultural and Biological Engineers in Pittsburgh, PA.

NC State's Department of Biological and Agricultural Engineering is a joint department of the university's College of Engineering and College of Agriculture and Life Sciences.

Biochar for Carbon Sequestration Study



This work is on a recent study done to evaluate the effect that adoption of biochar throughout the globe may have in terms of carbon sequestration.

The take home is that present regimes could comfortably handle up to fifteen percent of the CO2 produced and vented presently.

However, the real certainty is that we will be exiting the fossil fuel business over the coming century.  We are witnessing the first moves there in the massive emergence of successful wind energy production.  The real break will be fusion energy when we master that art.  In the meantime, Geothermal and solar will also emerge now at a great clip.
When we exit the fossil business also reforest the maximum open land which will massively increase the globe�s biomass, we are likely to swiftly create a CO2 deficit and will need to burn fossil fuels to make up the difference.

1.8 billion metric tons of carbon applied to land at say ten tons per acre will produce 200 million acres of fully involved terra preta soils.  This works out to be around a quarter million square miles per year.  Of course, in time we can just keep on adding carbon to fully involved soils but that then will not likely be necessary.

Also, as I have already posted, logistics and handling issues will likely make corn husbandry as the go to crop for this.  Most other crops simply produce too little usable waste.

And in spite of the ongoing chatter about using waste wood, it is not the first choice in terms of soils.  Most likely there the biochar will be screened for a fines fraction while the balance is used as a fuel for which it is well suited.

Offsetting greenhouse gas emissions using charcoal
00:11 August 11, 2010

According to a new study, as much as 12 percent of the world�s human-caused greenhouse gas emissions could be sustainably offset by producing biochar, a charcoal-like substance made from plants and other organic materials. That�s more than would be offset if the same plants and materials were burned to generate bioenergy, says the study. Additionally, biochar could improve food production in the world�s poorest regions as it increases soil fertility.

Biochar is made by decomposing biomass like plants, wood and other organic materials at high temperature in a process called slow pyrolysis � a form of incineration that decomposes organic materials by heat in the absence of oxygen. Normally, biomass breaks down and releases its carbon into the atmosphere within a decade or two. But biochar is more stable and can hold onto its carbon for hundreds or even thousands of years, keeping greenhouse gases like carbon dioxide out of the air longer.

Other biochar benefits include: improving soils by increasing their ability to retain water and nutrients; decreasing nitrous oxide and methane emissions from the soil into which it is tilled; and, during the slow pyrolysis process, producing some bio-based gas and oil that can offset emissions from fossil fuels.

The carbon-packed substance was first suggested as a way to counteract climate change in 1993. Scientists and policymakers have given it increasing attention in the past few years and this new study conducted by a collaborative team from the Department of Energy�s Pacific Northwest National Laboratory (PNNL), Swansea UniversityCornell University, and the University of New South Wales, is the most thorough and comprehensive analysis to date on the global potential of biochar.

The study
For their study, the researchers looked to the world�s sources of biomass that aren�t already being used by humans as food. For example, they considered the world�s supply of corn leaves and stalks, rice husks, livestock manure and yard trimmings, to name a few. The researchers then calculated the carbon content of that biomass and how much of each source could realistically be used for biochar production.

With this information, they developed a mathematical model that could account for three possible scenarios. In one, the maximum possible amount of biochar was made by using all sustainably available biomass. Another scenario involved a minimal amount of biomass being converted into biochar, while the third offered a middle course. The maximum scenario required significant changes to the way the entire planet manages biomass, while the minimal scenario limited biochar production to using biomass residues and wastes that are readily available with few changes to current practices.

The researchers found that the maximum scenario could offset up to the equivalent of 1.8 petagrams � or 1.8 billion metric tons � of carbon emissions annually and a total of 130 billion metric tons throughout in the first 100 years. Avoided emissions include the greenhouse gases carbon dioxide, methane and nitrous oxide. The estimated annual maximum offset is 12 percent of the 15.4 billion metric tons of greenhouse gas emissions that human activity adds to the atmosphere each year. Researchers also calculated that the minimal scenario could sequester just under 1 billion metric tons annually and 65 billion metric tons during the same period.

Making biochar sustainably requires heating mostly residual biomass with modern technologies that recover energy created during biochar�s production and eliminate the emissions of methane and nitrous oxide, the study also noted.

Biochar and bioenergy

Instead of making biochar, biomass can also be burned to produce bioenergy from heat. Researchers found that burning the same amount of biomass used in their maximum biochar scenario would offset 107 billion metric tons of carbon emissions during the first century. The bioenergy offset, while substantial, was 23 metric tons less than the offset from biochar.

Researchers attributed this difference to a positive feedback from the addition of biochar to soils. By improving soil conditions, biochar increases plant growth and therefore creates more biomass for biochar productions. Adding biochar to soils can also decrease nitrous oxide and methane emissions that are naturally released from soil.



However, the researchers say a flexible approach including the production of biochar in some areas and bioenergy in others would create optimal greenhouse gas offsets. Their study showed that biochar would be most beneficial if it were tilled into the planet�s poorest soils, such as those in the tropics and the Southeastern United States.

Those soils, which have lost their ability to hold onto nutrients during thousands of years of weathering, would become more fertile with the extra water and nutrients the biochar would help retain. Richer soils would increase the crop and biomass growth � and future biochar sources � in those areas. Adding biochar to the most infertile cropland would offset greenhouse gases by 60 percent more than if bioenergy were made using the same amount of biomass from that location, the researchers found.

On the other hand, the authors wrote that bioenergy production could be better suited for areas that already have rich soils - such as the Midwest � and that also rely on coal for energy. Their analysis showed that bioenergy production on fertile soils would offset the greenhouse gas emissions of coal-fired power plants by 16 to 22 percent more than biochar in the same situation.



Sustainability

The study also shows how sustainable practices can make the biochar that creates these offsets.

�The scientific community has been split on biochar,� says PNNL�s Jim Amonette. �Some think it�ll ruin biodiversity and require large biomass plantations. But our research shows that won�t be the case if the right approach is taken.�

The researchers� estimates of avoided emissions were developed by assuming no agricultural or previously unmanaged lands will be converted for biomass crop production. Other sustainability criteria included leaving enough biomass residue on the soil to prevent erosion, not using crop residues currently eaten by livestock, not adding biochar made from treated building materials to agricultural soils and requiring that only modern pyrolysis technologies � those that fully recover energy released during the process and eliminate soot, methane and nitrous oxide emissions � be used for biochar production.

�Roughly half of biochar�s climate-mitigation potential is due to its carbon storage abilities,� Amonette said. �The rest depends on the efficient recovery of the energy created during pyrolysis and the positive feedback achieved when biochar is added to soil. All of these are needed for biochar to reach its full sustainable potential.�

The study, "Sustainable biochar to mitigate global climate change," appears in the journal Nature Communications.

Friday, July 29, 2011

Global Warming & Effects

Global warming and ozone layer depletion has been a concern during the last two decades and has recently become a very prominent global issues and topics. While many opponents oppose the existence of the greenhouse effect, evidence can be seen throughout nature.

Your Role In Global Warming

The damage already done to the atmosphere is irreversible, but we can make changes now to protect the Earth's atmosphere in the future. If we reduce the amount of fuel we burn, by making changes in our lifestyle, we can reduce the amount of damage done to the atmosphere. Here, you will discover what role you can take to mitigate the effects of global warming on our world.

Monday, December 27, 2010

Flower Power Made Our Climate Grow




This is a startling and completely unexpected result. I am totally cognizant of the powerful role of transpiration in sustaining rainfall over ecology.  The great tropical rainforests are convincing demonstrations.  It is core to my proposal to restore the Sahara and the Asian dry lands.

That it was way more difficult before flowering plants was not obvious at all.

This suggests that upland habitat was typically dryer and way more extensive everywhere except local wetlands.  Suddenly Northern Australia looks like home for dinosaurs and the whole remnant ecosystem.

This also suggests that flowering plants are way more proficient at absorbing carbon.

The rainforests would likely have been hugely constrained to their best drainage and wetlands with intervening dry highlands.  The deserts may not have been much larger but plenty of land would have been seriously marginal.  Again think about Australia.



Flower Power Makes Tropics Cooler, Wetter


ScienceDaily (July 19, 2010) � The world is a cooler, wetter place because of flowering plants, according to new climate simulation results published in the journal Proceedings of the Royal Society B. The effect is especially pronounced in the Amazon basin, where replacing flowering plants with non-flowering varieties would result in an 80 percent decrease in the area covered by ever-wet rainforest.

The simulations demonstrate the importance of flowering-plant physiology to climate regulation in ever-wet rainforest, regions where the dry season is short or non-existent, and where biodiversity is greatest.

"The vein density of leaves within the flowering plants is much, much higher than all other plants," said the study's lead author, C. Kevin Boyce, Associate Professor in Geophysical Sciences at the University of Chicago. "That actually matters physiologically for both taking in carbon dioxide from the atmosphere for photosynthesis and also the loss of water, which is transpiration. The two necessarily go together. You can't take in CO2 without losing water."

This higher vein density in the leaves means that flowering plants are highly efficient at transpiring water from the soil back into the sky, where it can return to Earth as rain.

"That whole recycling process is dependent upon transpiration, and transpiration would have been much, much lower in the absence of flowering plants," Boyce said. "We can know that because no leaves throughout the fossil record approach the vein densities seen in flowering plant leaves."

For most of biological history there were no flowering plants -- known scientifically as angiosperms. They evolved about 120 million years ago, during the Cretaceous Period, and took another 20 million years to become prevalent. Flowering species were latecomers to the world of vascular plants, a group that includes ferns, club mosses and confers. But angiosperms now enjoy a position of world domination among plants.

"They're basically everywhere and everything, unless you're talking about high altitudes and very high latitudes," Boyce said.

Dinosaurs walked the Earth when flowering plants evolved, and various studies have attempted to link the dinosaurs' extinction or at least their evolutionary paths to flowering plant evolution. "Those efforts are always very fuzzy, and none have gained much traction," Boyce said.

Boyce and Lee are, nevertheless, working toward simulating the climatic impact of flowering plant evolution in the prehistoric world. But simulating the Cretaceous Earth would be a complex undertaking because the planet was warmer, the continents sat in different alignments and carbon- dioxide concentrations were different.

"The world now is really very different from the world 120 million years ago," Boyce said.

Building the Supercomputer Simulation

So as a first step, Boyce and co-author with Jung-Eun Lee, Postdoctoral Scholar in Geophysical Sciences at UChicago, examined the role of flowering plants in the modern world. Lee, an atmospheric scientist, adapted the National Center for Atmospheric Research Community Climate Model for the study.

Driven by more than one million lines of code, the simulations computed air motion over the entire globe at a resolution of 300 square kilometers (approximately 116 square miles). Lee ran the simulations on a supercomputer at the National Energy Research Scientific Computing Center in Berkeley, Calif.

"The motion of air is dependent on temperature distribution, and the temperature distribution is dependent on how heat is distributed," Lee said. "Evapo-transpiration is very important to solve this equation. That's why we have plants in the model."

The simulations showed the importance of flowering plants to water recycling. Rain falls, plants drink it up and pass most of it out of their leaves and back into the sky.

In the simulations, replacing flowering plants with non-flowering plants in eastern North America reduced rainfall by up to 40 percent. The same replacement in the Amazon basin delayed onset of the monsoon from Oct. 26 to Jan. 10.

"Rainforest deforestation has long been shown to have a somewhat similar effect," Boyce said. Transpiration drops along with loss of rainforest, "and you actually lose rainfall because of it."

Studies in recent decades have suggested a link between the diversity of organisms of all types, flowering plants included, to the abundance or rainfall and the vastness of tropical forests. Flowering plants, it seems, foster and perpetuate their own diversity, and simultaneously bolster the diversity of animals and other plants generally. Indeed, multiple lineages of plants and animals flourished shortly after flowering plants began dominating tropical ecosystems.

The climate-altering physiology of flowering plants might partly explain this phenomenon, Boyce said. "There would have been rainforests before flowering plants existed, but they would have been much smaller," he said.

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