Tuesday, September 20, 2011

Night Hike scheduled for November 3rd


(Click on photo to enlarge and print.)Come to a NIGHT HIKE at Moore Memorial Woods on Thursday, November 3rd from 5:30 to 8:00 PM. The Guernsey Soil & Water Conservation District will be hosting a night of fun and learning for children from six to sixteen. There will be pumpkin decorating, making turkey calls, and wildlife specialist Joe Lehman will lead a hike through the gathering dusk, explaining to the kids what is happening in the woods as the animals prepare for the long winter ahead. The evening will conclude with a weenie roast, marshmallows, and hot chocolate.

Space is limited to the first 30 kids. Please bring an adult with you, as supervision is required, and they will have just as much fun as you will! There is no charge for this event, but you do need to register by October 31st to attend. Stop by the office at 9711 East Pike during business hours M-F, or call the district at 432-5624. You will be provided with directions to the woods (east of Old Washington) when you register, or click on the page above to find the woods.

Soil Inhabitants: Beetle Mites


Oppia sp.

Vital Statistics:Length: 0.2 - 0.3 mm (could stand on the tip of your ball-point pen).
Lifespan: 6-12 months
Total Mite Population: up to 600,000 per square meter (6 in one teaspoon of soil).


Natural History:
In spite of their name, the round little beetle mites aren't insects at all. They are actually cousins of the spiders and ticks. Beetle mites are just one group of thousands of kinds of mites that live in the soil. Like most soil organisms living in a world of darkness, beetle mites have no eyes.
Mites are one of the first links in the chain of decomposers that break down organic matter into humus. Armies of mites swarm through leaf litter and the air spaces between soil grains. Each kind looks for its favorite food. Beetle mites eat nothing but fungus. They turn the fungus into pellets. Bacterial colonies coat the pellets and feed on them. The bacteria make plant nutrients from the pellets. The leftovers become part of the soil.
Beetle mites also carry fungi and bacteria with them, helping to spread these organisms through the soil. When the die, their bodies join the chain, adding minerals back to the soil.

Thursday, September 15, 2011

Many thanks to our victims, er....volunteers!

Cambridge city mayor Tom Orr
Meadowbrook teacher Matt Wentworth
Meadowbrook teacher Laura Kackley
Buckeye Trail teacher Ginny Barker
Guernsey county commissioner Steve Douglass

Thank you to all the volunteers that made the Guernsey Soil & Water Conservation District's "Pie in the Eye" for conservation a success! Our thanks to all of you who bought a chance to throw a cream pie at your favorites!
Thank you to Riesbecks, Cochran's Market, T&J Market, and Food Distributors for donations of whipped topping!
The money raised goes to support our summer Conservation Daycamp, which is in its 26th year. Still only $5 for 2 days of fun and learning!

Tuesday, September 13, 2011

Don't forget the Pie throwing tomorrow at the Fair!

On Wednesday, September 14th at 5PM, you will have a chance to throw a cream pie at your favorite target! Be sure to stop by the SWCD booth behind the grandstand - only $1 per throw, with the proceeds to benefit our Concervation Day Camp. "Con Camp" has been held every year since 1985, teaching hundreds of Guernsey county youth over the years.

Soil Inhabitants: Amoebas


Amoeba proteus



Vital Statistics:Length:0.3 mm (40 would fit between the lines on your notebook paper).
Lifespan: Can survive long inactive periods in dry, sealed capsule.
Total Protozoa Population: up to 10 billion per square meter (5 million in one teaspoon of soil).

Natural History:Soil amoebas belong to a diverse group of one-celled animals called protozoa. They roam the film of water coating each soil particle. This water layer is so thin that an amoeba can still survive in even very dry soils.
An amoeba uses its blobby tentacles both to move and to feed. It doesn't waste any time chewing its food. Its tentacles surround a food item and bring it inside its body. A single amoeba can eat thousands of bacteria each day. Amoebas eat so many bacteria that they compete with nematodes for food. Soils with lots of protozoa have fewer nematodes.
Amoebas belong to the soil recycling crew. They can't use all of the nutrients in the bacteria they eat. So a lot of the nutrients go back into the soil. Plants use these nutrients to grow.
Amoebas and other protozoa must breath oxygen. They mostly live in the top layer of soils that mix well with the air.

Friday, September 9, 2011

Soil Inhabitants: Bacteria



Vital Statistics:Length: 0.001 - 0.005 mm (over 1,000 could fit across the head of a pin).
Lifespan: Divides into two new bacteria as often as every 20 minutes.
Total Bacterial Population: Up to 1,000 trillion per square meter (5 billion in one teaspoon of soil).

Description & Natural History:All life in the soil depends on its smallest residents. Single-celled bacteria are the oldest living things. And they power the entire ecosystem. They may have boring shapes, but they do ore different biochemical jobs than any other kind of organism.
Thousands of species of bacteria fill the soil. Most are decomposers. They recycle the energy stored in dead organic matter back into plant food. Other bacteria make nutrients with the help of host plants. For example, bacteria living in the roots of plants like peas and clover turn nitrogen from the air into fertilizer. A few bacteria can get energy from minerals instead of organic matter. Some of these can even feed on chemical pollution.
Bacterial colonies make slime that helps them stick to soil particles. The slime also sticks soil particles to each other. These goopy clumps help hold water in the soil. Plant roots can easily grow through the spaces between these clumps.
The familiar, earthy odor of rich, damp soil is the smell of bacteria at work.

Tuesday, September 6, 2011

Soil Inhabitants: Night crawler



Lumbricus terrestris

Vital Statistics:
Length: 9-30 cm (would fit in your hand).
Lifespan: 3-6 years
Total Earthworm Population: up to 300 per square meter (several in each shovel of soil).

Natural History:Our largest and most common species of earthworm is not native to North America. Night crawlers stowed away with European settlers bringing their favorite plants. Since then they've spread everywhere people have gone.
Earthworms have no teeth. That doesn't stop them from eating just about any dead organic matter they come across. They also swallow soil as they burrow. The microscopic animals in each bite of soil become worm food, too. An earthworm's gut is a great place for bacteria to grow. Earthworm castings add more bacteria back to the soil than the worm eats. More bacteria mean healthier soil. Together, all the worms in an area the size of a football field can eat about four tons of earth a year! All this adds to the humus in the soil.
It's a myth that earthworms come to the surface when it rains because they are drowning. Some scientists think that this behavior helps worms migrate to new territory or to find a mate. But no one knows for sure why they do it.

Thursday, September 1, 2011

Soil Inhabitants: Eastern mole


Scalopus aquaticus

Vital Statistics:Size: 13-20 cm long, including tail (would fit inside a can of peas).
Lifespan: 3 years
Population: Several per acre.

Natural History:Moles use their webbed feet and strong shoulder muscles to literally swim through the soil. Unlike their cousins the shrews, moles are almost blind. They use their sense of smell and the ability to feel vibrations to find food and navigate.
Gardeners blame moles for ruining plants. But they don't actually eat plant roots or bulbs. Instead, they're hungry for earthworms and insect larvae. Moles help control populations of harmful insects. Digging is hard work. So an active mole must eat about half its entire body weight each day.
Moles dig their tunnels in open pastures, meadows, and woodlands. They like moist, sandy loam soil the best. A mole looking for food will tunnel just under the surface. Its digging helps loosen the soil and allows air in. Moles also dig deeper permanent tunnels and burrows. They use these for sleeping, raising young, and traveling to food sources.

Tuesday, August 30, 2011

Take a pie in the eye for conservation

Cambridge Mayor Tom Orr


Guernsey County Commissioner Steve Douglass


Meadowbrook teacher Laura Kackley



Meadowbrook FFA teacher Matt Wenworth




Buckeye Trail FFA teacher Ginny Barker



This year at the Guernsey county fair an old fashioned pie throwing contest will take place. The Guernsey Soil and Water Conservation District is sponsoring the contest, with proceeds slated for conservation education. People from around the community have volunteered to "take a pie in the eye." Now is your chance to help too. Whether it’s a vendetta you have for them or just for fun, come wing a pie at our contestants. The contest will be held on Wednesday evening during the fair at the Guernsey Soil and Water booth, located behind the grandstand. One chance to throw is only a dollar. Where else can you get this type of satisfaction for a buck?!? The event runs from 5:00 to 6:30 with different targets every 15 minutes, so check the above line up to select your victim.

Friday, August 26, 2011

What is your soil IQ?


1. Name some organisms that live in the soil?
2. Guess: How many tons of organic matter can an earthworm digest in one year?
3. What is organic matter?
4. How many years does it take to form one inch of topsoil?
5. What is the most productive soil layer?
6. What are the two causes of soil erosion?
7. Each distinctive layer in soil is called what
8. True or False: Soil texture is the percentage of sand, silt, and clay.
9. True or False: No-till is a farming practice that leaves the soil
undisturbed prior to planting.
10. What is soil called that is deposited by wind or water?

Click to enlarge answer key

Tuesday, August 23, 2011

CRIMINAL CASES SOLVED USING EARTH MATERIALS

The Federal Bureau of Investigations (FBI) has collected and studied soil samples, minerals, and other Earth material for criminal investigations since 1935 and thousands of cases involving Earth materials are studied in the United States each year. Throughout the world soil is usually collected at crime scenes, is routinely studied at crime labs, and is often used as physical evidence during crime trials.
Following are some real-life stories of crimes that were solved using Earth materials, thorough investigative work, and dedicated, professional scientists who studied soils and geology to become knowledgeable in their field. So you see, there really is more to soil than what's under foot!

A crime had been committed in the foothills of the Rocky Mountains, near Denver, Colorado. One month later a burning vehicle was found at a dump in New Jersey (on the East Coast of the United States). Soil samples were taken from the fender of the burning car and were studied by Forensic Geologists. Analyses of the soil samples showed there were four layers of soil that had built up under the burning car's fender. The outer, most recently deposited layer of soil was from the New Jersey dumpsite. The three inner layers of soil contained minerals from the Rocky Mountain Front area near Denver, Colorado

Forensic geologists obtained 360 soil samples from the Rocky Mountain Front area to compare them with those found under the fender of the burning car in New Jersey. Soil samples were also taken from the victims ranch. One of the three inner layers of soil under the suspect's car's fender matched the soil sample Forensic Geologists obtained at the crime scene. The second inner layer of soil under the suspect's car fender matched the soil sample Forensic Geologists obtained at the victim's ranch. The first inner layer of soil did not match any of the 360 soil samples taken by the Forensic Geologists but was determined to have originated from the Denver area. The suspect was convicted and jailed based upon the results using soil sample comparisons.

In the case of stolen potatoes on the east coast of the United States, a suspect who possessed the questionable potatoes was convicted of stealing them once analysis of the soil on the potatoes determined that the superphosphate in the soil that was clinging to the potatoes matched the soil from the farm where the potatoes were grown. The farm's soil contained a significant build up of phosphate because the farm was heavily fertilized with nitrogen, potash, and phosphate (phosphate doesn't leach out of the soil as readily as potash and nitrogen).

In another case, tobacco was reported stolen from a farm. Soil samples were taken from the farm where the tobacco had been stolen, and samples were also taken from the leaves of the stolen tobacco and from the suspect's farm. Soil comparison studies indicated that the soil on the stolen tobacco leaves did not match the soil samples taken from the suspect's farm, but matched soil samples taken from the farm where the tobacco was reported stolen. The suspect was arrested based upon the resulting soil sample comparisons.

Microscopic fossils called diatoms were once very prominent on Earth, and collectively deposited to form a sedimentary rock called diatomaceous earth. Some manufaturers use diatomaceous earth for insulating safes, that are used to store valuables. Burglary crimes have been solved by examining white specks from suspects' hair and clothing to determine that the specks were actually diatoms that came from broken safes at crime scenes, and not dandruff as the suspects had claimed.

If you would like to learn more about the interesting and exciting world of soil, check with your local library or on the World Wide Web. You just might learn something you'd never thought about before!

Information contained in"Secrets Hidden in Soil" was derived from "Forensic Geology" by R. Murray and J. Tedrow, Rutgers University Press, 1975. ISBN 0-8135-0794-4. Also, special thanks to Dr. Richard Arnold, USDA, Natural Resource Conservation Service/Soil Survey Division, Washington, D.C.