The World's Largest Land Mammals

Friday, 8 April 2011

The World's Largest Land Mammals


Dinosaur extinction enabled mammals to grow to record size


Mamals Grew About 1000 Times Bigger




Researchers have demonstrated that the extinction of dinosaurs 65 million years ago paved the way for mammals to get bigger — about a thousand times bigger than they had been. The study titled, "The Evolution of Maximum Body Size of Terrestrial Mammals," released today in the prestigious journal Science, is the first to quantitatively explore the patterns of body size of mammals after the demise of the dinosaurs.

The research, funded by a National Science Foundation Research Coordination Network grant and led by University of New Mexico Biology Associate Professor Felisa Smith, brought together an international team of paleontologists, evolutionary biologists and macroecologists from universities around the world.

The goal of the research was to revisit key questions about size, specifically in mammals. "Size impacts all aspects of biology, from reproduction to extinction," said Smith. "Understanding the constraints operating on size is crucial to understanding how ecosystems work."

Building a Comprehensive Mammal-Size Database



In order to document what happened to mammals after the extinction of dinosaurs, researchers collected data on the maximum size for major groups of land mammals on each continent, including Perissodactyla, odd-toed ungulates such as horses and rhinos; Proboscidea, which includes elephants, mammoth and mastodon; Xenarthra, the anteaters, tree sloths, and armadillos; as well as a number of other extinct groups. The researchers spent three years assembling the data.

"The database is unique," said Smith "because it's comprehensive, including mammals from all continents since the extinction of the dinosaurs. We estimated body size from fossil teeth, which are the most commonly preserved parts of mammals."

A Global, Trophic Group and Lineage Pattern



Mammals grew from a maximum of about 10 kilograms when they were sharing the earth with dinosaurs to a maximum of 17 tons afterwards. The researchers found that the pattern was surprisingly consistent, not only globally but also across time and across trophic groups and lineages – that is, animals with differing diets and descended from different ancestors – as well.

Mammal Size Peaks in the Oligocene



 
The maximum size of mammals began to increase sharply about 65 million years ago, peaking in the Oligocene Epoch (about 34 million years ago) in Eurasia, and again in the Miocene Epoch (about 10 million years ago) in Eurasia and Africa. The largest mammal that ever walked the earth — Indricotherium transouralicum, a hornless rhinoceros-like herbivore that weighed approximately 17 tons and stood about 18 feet high at the shoulder – lived in Eurasia almost 34 million years ago.

"The remarkable similarity in the evolution of maximum size on the different continents suggests that there were similar ecological roles to be filled by giant mammals across the globe," said Smith. "This strongly implies that mammals were responding to the same ecological constraints."

Available Space and Climate Influence Size





The results give clues as to what sets the limits on maximum body size on land; the amount of space available to each animal and the climate they live in. The colder the climate, the bigger the mammals seem to get, as bigger animals conserve heat better. It also shows that no one group of mammals dominates the largest size class – the absolute largest mammal belongs to different groups over time and space.

"The results were striking. Global temperature and terrestrial land area set constraints on the upper limit of mammal body size," said Smith, "with larger mammals evolving when the earth was cooler and the terrestrial land area greater. Our analysis reflected processes operating consistently across trophic and taxonomic groups, and independent of the physiographic history of each continent."

The interest in the size of mammals for Smith began years ago when she was a graduate student at the University of California. "I worked on a number of islands off the coast of Baja, California where rodents had evolved into gigantic body sizes. I've been interested in size ever since."

Colleagues, Coauthors and Contributors



Smith's colleagues in the project include from UNM Distinguished Professor of Biology Jim Brown, Marcus Hamilton and Jordan Okie. Other coauthors are: Alison Boyer, Daniel Costa, Tamar Dayan, Morgan Ernest, Alistair Evans, Mikael Fortelius, John Gittleman, Larisa Harding, Kari Lintulaakso, Kathleen Lyons, Christy McCain, Juha J. Saarinen, Richard Sibly, Patrick Stephens, Jessica Theodor and Mark Uhen.
source http://geology.com/press-release/largest-land-mammals/e :

Geothermal Heating systems capture heat energy beneath our feet

Thursday, 7 April 2011


 

Geothermal Heating systems

 






Beneath the surface of the earths crust lies a hidden energy source that is more
than capable of providing us with heat and hot water. Geothermal heating systems
have been designed to efficiently harvest this hidden energy source, which is
known as thermal energy. This article will give you a better understanding of
how thermal energy was created and how geothermal heating technology is able to
harvest it.

But how exactly has thermal energy come into existance?
There are a number of reasons why the ground contains heat. Heat from the suns
rays is absorbed for example. Also the earths core still continues to radiate
out heat. In some parts of the world this underground heat source is much
stronger. No matter where in the world you are however, geothermal heating
technology can quite effectively extract this hidden heat.

The concept
of tapping into heat energy that naturally occurs under ground is not new.
Thousands of years ago the Romans grasped the idea that naturally occurring hot
water heated by geothermal energy could be used to heat their spas and some of
their buildings. Collecting naturally occurring heated water and transferring it
to places to provide heat and hot water for personal use can really be thought
of as a simple geothermal heating system. In todays world, naturally heated
water beneath the earths surface is still being made full use of. Iceland for
example have developed special geothermal power stations which harvest this
energy to provide electricity to homes and businesses.

Nowadays across
the globe many homes make use of Ground Source heat pump technology which is
proving to be very reliable and efficient method of geothermal heating. As you
can probably guess from its name the Ground Source heat pump harvests heat from
beneath the earths surface and using a pumping method provides this heat
wherever it is needed. Ground source heat pumps contain a loop of pipes that are
sited beneath the ground. The loop of pipes contain a solution that can quite
easily absorb any heat energy present in the ground. The solution is pumped
continually through the loop of pipes and absorbs heat from the surrounding
ground as it flows. The solution eventually passes through the heat pumps the
heat exchanger part of the system where the heat is extracted and refined. This
collected heat is then out to use to provide heat for our homes and heat our hot
water.

Geothermal heating systems are seeing an increase in popularity
right across the globe. In general most people are very aware that they need to
change the way they do things in order to become more environmentally friendly.
Most people are also reluctant to keep forking out rediculous money to keep
their homes warm using traditional fuels such as gas and oil. That is why many
people are switching over to geothermal heating systems such as Ground Source
heat pumps to warm their homes and hot water.

If this article has been
of interest you may just want to find out a little more about the benefits of
investing in geothermal heating systems such as Ground Source heat pumps? It is
a good idea to visit the websites of the specialist companies that focus on
providing renewable heating and geothermal heating technology. One reputable and
well established company is clled EcoVision. You can easily find their website.
EcoVision specialises in geothermal heating systems as well as a whole range of
other eco-friendly technologies. The EcoVision website will provide you with all
the information you could possibly want to find out.

Source:
http://www.ArticlePros.com/author.php?Richard
Stevens


How Mine Dust is Produced


How Mine Dust is Produced









The dust from a mine is to a large degree different from the dust you find in
your home. Dust in your home is mostly made up of dead skin while mine dust is
almost exclusively a mineral in a fine powder form.
Most written definitions
of mine dust are close to the following: dust from drilling, blasting, smashing
or handling of rock. The majority of the dust made by one of these activities
are too large to stay in the air for any length of time and account for about 40
percent of all dust created at a mine site. The remainder is less than 10
micrometers in size. The majority of these particles is less than 2.5
micrometers and are produced from the exhaust of equipment used on the mining
site.
The smallest size particle is what is most hazardous to the
population's health. The larger dust particles are an eye sore and are costly to
clean up, but are less hazardous to one's health.
The smaller particles do
produce certain health hazards that include respiratory problems due to the fact
that they are in the air that is breathed in to the lungs. This can be minimized
if mining personnel were to wear masks designed to filter out the dust.

Another method dust can be minimized on the mining site is by utilizing a
dust suppression system. This is where water is sprayed over piles of rocks and
the ground, particularly in the loading areas. These particles will be absorbed
by the water thus become too heavy to remainin the air and eventually drop back
onto the ground from which they came
The large trucks that are used in the
mining area are also responsible for kicking up a great deal of dust, but most
of that is fugitive dust from the ground soil and not the mine
dust.


Source:
http://www.ArticlePros.com/author.php?Mark
Sierra

Mapping the future with LiDAR

Mapping the future with LiDAR








Everyone’s heard of RaDAR – the process of mapping a three dimensional
environment with radio waves – but what about LiDAR? The former is an acronym
referring to the practice of Radio Detection and Ranging, whereby radio waves
are bounced off objects and recorded as they return, enabling a cartographer or
mapping instrument to build up a picture of an environment, including the
distance between things and their relative heights. LiDAR uses laser pulses to
achieve the same objective: the difference being that Light Detection and
Ranging uses much shorter wavelengths than its radio wave counterpart, which
means that smaller objects can be more accurately mapped and elevations more
successfully delineated.
One of the most useful applications of LiDAR, in
the cartographic world, is its ability to return detailed information on the
“face structure” of a terrain: which is to say, the actual contours of the
ground beneath things like trees and plant growth. LiDAR technology has been
used extensively to accurately depict the location of fault lines between
tectonic plates – an immensely useful tactic for geographers trying to build
working predictive structures that can provide early warning on possible
earthquake hotspots. The laser pulses (usually emitted from aircraft carrying
portable equipment) deliver information that is cross referenced with GPS
readouts to provide a comprehensive map of ground elevation and terrain.

LiDAR is also capable of delivering intensive atmospheric information –
something its radio wave counterpart is incapable of doing. Because the laser
pulses involved have a much shorter wavelength than RaDAR imaging, they can be
calibrated to bounce back off different densities of vapour, cloud particle, and
so on. That means that the “thinness” of the air can be measured, which allows
cartographers to generate maps carrying huge amounts of atmospheric detail.
Ultimately, LiDAR is capable of producing maps that give impressive images both
of real ground topology (rather than treeline elevations or building cover) and
atmospheric characteristics. That makes the technology invaluable for scientific
and geologic mapping of an area – ideal, for example, for companies who wish to
enter into building or excavation projects in a particular location. In effect,
the laser images of that location provide a previously impossible look at the
basic geographic characteristics of the area – its rock strata, terrain
configuration and likely weather patterns.
The technology has been adopted
by civilian mapping companies, who are starting to create incredibly detailed
maps of UK cities using Light Detection and Ranging equipment. Famously, UK
cartography outfit Get Mapping has been using LiDAR for several years now to map
elevation for construction projects and environmental agencies. The Light
Detection and Ranging equipment being used by civilian outfits is normally
shared from dedicated companies or Government bodies who have the funding and
expertise to run the aircraft and equipment needed to make the maps.
On an
increasingly claustrophobic island, where space is at a premium and new building
projects seem essential to house our people and bolster our economy, the
technology represented by Light Detection and Ranging is fast becoming
indispensable. The UK can’t afford to indulge in construction projects whose
progress is halted by unforeseen difficulties of terrain: and with this
technology on its side, it doesn’t have to.

Source:
http://www.ArticlePros.com/author.php?Getmapping
Plc

Mapping the future with LiDAR

Soil - The World Beneath Your Feet

Soil - The World Beneath Your Feet





There is a complex invisible world beneath your feet and it is necessary to make
an effort to develop an appreciation of how the state of the soil affects plant
growth.

Soil is a mixture of tiny rock particles, living organisms,
chemicals and the remains of dead plants and animals. Spaces between the
particles will also contain a certain amount of air and water depending on the
type of soil.

Rocks near the earth’s surface are slowly broken down in
nature by a process called weathering. Eventually small particles such as sand,
silt and clay are formed. These particles create the environment for billions of
mostly tiny organisms to live. Larger organisms such as earthworms and insects
are also found in soil. A healthy soil is teeming with life.

The main
aim as a hobby farmer is thus to try to improve soil health by good management.
Poor management can lead to a loss of fertility and degradation of the soil. In
extreme cases the valuable topsoil can also be blown or washed away. In the end
poor soils lead to low quality crops lacking in nutrition.

Below are
examples of some checks I plan to carry out on my farm with the aim of improving
soil fertility.

1) Carry out a pH test in different places. This test
will determine if the soil is acid, alkaline or neutral. Most plants prefer a pH
level around 6.5. Should the pH level be too (below 6) corrections can be made
by adding lime. Should the pH be too high (above 7) this can be lowered by
adding plenty of organic matter and mulch. Extremely alkaline soils can be
changed by adding ground sulphur.

2) Check the soil texture of the soil
by rubbing some moist soil between your fingers. This will help to determine the
type of soil present. Sandy soils will have a coarse feel. These soils dry
quickly. Adding lots of organic matter will improve sandy soils. Very sandy soil
can also be improved by adding clay. If the soil feels sticky when rubbed it
contains too much clay. Clay soils drain slowly and are difficult to work when
wet. Adding gypsum will help in most cases. Should the soil have a good balance
of sand, silt and clay you will be blessed with a loamy soil. These soils are
generally easy to manage and do not require treatments.

3) Check the
level of organic matter in the soil. This can be done by shaking a handful of
soil in a jar and seeing how much organic matter floats to the surface. If only
a thin layer is present on the surface, lots of organic matter needs to be
added. This means more microorganisms can be sustained, these in turn will
release essential health giving chemicals needed by plants.

The above
tests are simple to carry out and much information is available on these topics.
Further tests require equipment or a soil testing company to analyse the soil.
These include salinity, especially if bore water is used. Individual soil
nutrient levels for Nitrogen, Phosphorous and Potassium as well as trace element
levels can also be measured. Other aspects such as fertilizer application and
cultivation practices to maintain soil structure also need attention.


Soil care requires years of experience and looking to older gardeners
will give you lots of essential tips. Also, experienced gardeners can often
identify soil problems by looking at the general appearance of plants. Getting a
spade and digging around will give you information about conditions such as
waterlogging and excessive dryness.

Do all you can to look after your
soil and allow your plants to carry out the magic task of turning fertilizers
and compost into healthy and nutritious food.

Source:
http://www.ArticlePros.com/author.php?Ben
Tan

Causes and remedies of Earthquakes

Tuesday, 5 April 2011

Causes and remedies of


 Earthquakes







An Earthquake is a sudden movement of the ground that releases the elastic
energy stored within the rocks, creating destructive seismic waves. The word
“seismicâ€‌ comes from the Greek word “seismosâ€‌ meaning an earthquake.
These quakes are not isolated events. They come with smaller shocks, called
aftershocks, with smaller effects. An earthquake is caused when two sides of a

large fracture in the rocks within the earth slide past each other. This
fracture is called a fault, which may be microscopic or thousands of kilometers
in length, while their width is usually a few millimeters or a few meters in
size.The size of an earthquake depends on the area of the fault that ruptured,
and the distance through which the rocks on the two sides of the fault slide
past one another.Small earth quakes are caused by small faults or small parts of

big faults. These last only for a fraction of a second and usually unnoticed, as
the rocks on either side of the faults are not displaced much. The larger ones
are caused due to faults which are tens to thousands of kilometers long, taking
minutes and the displacement of the rocks is around tens of meters. Earthquakes
are caused because the earth is regularly cooling since it was born, the seismic
wave being one of its ways to release the elastic energy. Earthquakes are
generally categorized into three types: Tectonic, Volcanic and Artificial.
Tectonic earth quakes are the most devastating, and unfortunately the most
unpredictable. The volcanic quakes are seldom important or devastative, but they
help predict the eruption of volcanoes. The artificial ones are caused due to
human activities, like pumping fuels deep into the earth or due to
explosives,
and several other reasons. MEASUREMENT OF EARTHQUAKES: The most popular scale
used to measure earthquakes is the Richter scale, named after Charles Francis
Richter (US).This scale measures the energy released at the focus of the quake,
read through a seismograph which gives the direction and force of the quakes. An
earthquake of size 8 is 10 times more devastative than size 7, 100 times more
destructive than 6, and so on. the frequency of earthquakes decreases
as the
magnitude increases, as the earth experiences about 800 earth quakes of size 5-6
, but only one or two quakes of size 8-9. EARTHQUAKE EFFECTS: Earthquakes cause
great loss of life by causing damage to buildings, bridges, dams, etc. they can
trigger devastating landslides. Fires can begin due to leaks in Gas plants and
electrical lines. Earth quakes can also generate tidal waves, or the tsunamis,
capable of destroying entire townships. These quakes also cause liquefaction of
soils, which makes soil lose almost all its strength, which makes it function

like quicksand. This material is capable of swallowing an entire building within
itself. Earthquakes around the world cost around 15,000 lives per year. Several
countries like the United States of America, China, Japan and Russia are most
actively participating in seismological research, trying to predict future
earthquakes.

Source:

Hydro Renewable Source of Energy

Hydro Renewable Source of Energy
 
Author: Fabricio Guerrero, approved at 10.04.2008


 
Among the renewable
energy sources that produce electricity, hydropower is the most common one. It
calculated for a 7 % of total U.S. electricity generation. It is among the
oldest resource of energy and was used many years ago to revolve a paddle wheel
for reason such as grinding grain. The first U.S. hydroelectric power plant
opened on the Fox River near Appleton, Wisconsin, on September 30, 1882. Before
that, coal was the solitary fuel used to produce electricity. Since the supply
of hydropower is water, hydroelectric power plants must be situated on a water
resource. Consequently, when the expertise to broadcast electricity over
stretched distances was urbanized, hydropower happens to be extensively
used.

Mechanical energy is consequent to the directing, harnessing, or
channeling moving water. The quantity of obtainable energy in moving water is
dogged by its run or drop. In any of the above case the process remains the
same. The watercourses through a pipe, or then pushes against the blades and
turns it in a turbine to whirl a generator to generate electricity. In a
run-of-the-river system, the energy of the current relate to the needed
pressure, while in a storage system, water is mounted up in tanks formed by
dams, and released when the requirement for power is elevated.

It is not
as much expensive as fossil fuels and does not add to the greenhouse effect.
Contrary to other renewable resources like the sun or wind, water can be
accumulated which makes it a better alternative to create electricity. Rivers,
dams and waterfalls can be used to produce hydro-electricity. Hydroelectric
posting is built where there is running water. The most widespread are located
in dams, where water can be stored sufficiently.

Hydroelectricity makes
available approximately 10% of the electricity spawned in Australia and 18% all
over the world. Hydro-power is the principal source of renewable energy. It
supplies more than 97% of energy formed by renewable sources. Other renewable
sources accounts for a mere 3% of the production.

The basic in which it
scores over other renewable sources are:

Hydroelectricity emits no gas or
waste.
It is more consistent than solar and wind power as water can be
stored and there is additional of it,
Hydroelectric stations are economical
to manage.

However, they do have their own set of problems that can
sometimes create lot problems:

Large dams acquire bulky areas of land and
can lead fish and other animals to displace.
Plant life can be affected by
alter in water value.
The power positions are costly to construct.

To
learn much more about the different types of
renewable energy
sources
, visit
http://renewable-energy-sources-info.blogspot.com/ where
you'll find this and much more, including biodiesel, biofuel, Bioethanol,
biomass,geothermal and many more renewable energy sources




source :http://www.softensive.com/show.php?cat=18&art=6407