October 2018 – Greenacres Foundation

29 Oct 2018

Research Peter Wheeler 0 comment

Heard but not seen

The past week has been a little busy in Indian Hill so we finally got a chance to do our third and final covey call count today. It sounds like the coveys are located around one specific area so this time I didn’t want to take any chances and not hear them. Jennifer and I split up again but stayed within sight of one another (once the sun came up) so we were both in the area where the quail were heard the first and second time. Finally I heard it! The covey call that had been eluding me the first two trips was just south of where I was sitting. After the sun came up Jennifer and I both agreed on the direction that I heard the sound, however she also heard one to the northeast of where we were. We thought we would try flushing the birds to try to see if we could get a count so we headed toward the edges of the field. We had no luck getting the birds to flush out of their coveys but we both feel pretty confident that we at least have some quail walking about the Lewis Township property. Now the goal is to see if we can increase our quail populations through improved habitat establishment and quail-beneficial management practices. Call counts and quail monitoring will be an ongoing practice for our research team. We are already looking forward to some early chilly mornings next October.

29 Oct 2018

Learn Peter Wheeler 0 comment

Horsehair Worms

There’s something about long, thin worms that puts people on edge. Even I hesitated to pick up this little guy because of the fear of parasitic worms. Don’t worry, these horsehair worms (Gordius robustus) are not some parasitic nematode ready to crawl up your nose and take over your body. Well actually, I should clarify. You’re safe if you are a human. Even your pets are safe. However, if you’re an arthropod, you might be in trouble. The mature adults (like you see in the picture) aren’t the ones causing problems. It’s the babies you have to look out for, and you won’t even see them coming!

Adult females lay MILLIONS of eggs in the water. The minuscule (~0.01 inches) larvae are ingested by certain bugs for food. A hard covering (cyst) protects the larva, then dissolves after entering the gut of its host. Many macroinvertebrates become hosts because they live in aquatic habitats. Other common hosts are crickets, grasshoppers, and beetles because they eat macroinvertebrates, thus becoming the new host to the horsehair worm. As a horsehair worm develops into an adult over a few weeks or months, the host becomes the ‘walking dead’. Because adult horsehair worms require water to leave their host, the zombie host bug is triggered to find water, where it meets its demise. Most of us have seen witches melting from water in the Wizard of Oz, but here’s a new visual for you: death by worm breaking through a body cavity. And if you really want a good visual, search for horsehair worms on youtube. You’ll find all sorts of videos of them crawling out of crickets, spiders, cockroaches, and other arthropods. Maybe save it for Halloween.

One legend behind their name is that people believed the hairs from a horse’s mane or tail would fall into the water bucket and come to life. In reality, a cricket or host had hopped up to the water bucket, prompting a horsehair worm to break free in the water source. They are also referred to as Gordian worms because they twist and squirm into ‘Gordian knots’. In addition to having a very remarkable life cycle, horsehair worms are important for keeping our pest population in check. I encourage you to go on a hike and keep an eye out for any strange behavior from arthropods around water.

~Tracy

18 Oct 2018

Research Peter Wheeler 0 comment

Chilly mornings in the field

Today Jennifer and I got another early start to do some covey call counts and hopefully hear the coveys that our resident bird expert Joe heard a couple of days ago. It was another clear and chilly morning and this time I was a little more prepared by bringing a fold up camp chair. I found out that standing still in the middle of a field in 20 degree weather can be hard on your back! With a head lamp, chair, and a thermos of hot tea, we walked back to the same location where Joe was situated on our previous visit. We still thought it would be a good idea to split up and go on opposite sides of the tree line, hoping we could better locate the direction in which the covey calls were coming from. I kept looking at my cell phone to be prepared for when 7:14am approached so I could be extra focused. 7:14am came and went, then 7:29am. Next thing I know, the sun is up. Maybe Joe didn’t hear them…or maybe it’s just me? When Jennifer and I met back at the tree line where we separated she excitedly said “did you hear them!?” Nope. Well…I guess it is me. Next time we go to Lewis Township I’m sitting right where Jennifer and Joe were located so I can get in on the action too! Good news is, Jennifer was pretty sure it was a covey call so we’re one step closer to confirming we have some quail populations. And once again, as you can see in the picture, it was another beautiful early morning – a great way to start the day.

16 Oct 2018

Research Jennifer Mansfield 0 comment

Healthy Soil Holds Water

Healthy Soil Holds Water

In addition to testing the soil itself, we collect other types of information. Water infiltration is a measure of how quickly 1 inch of water will enter the soil. Metal rings are driven into the ground, water poured into the ring and the timer begins. Without stable soil aggregates the pores collapse and water will not move into the soil. Stable soil aggregates (produced by biology) maintain the pore structure and water moves into the soil. Our newest property in Lewis Township (Brown County, OH) has historically been used for soybean crops. Many of the areas tested there had standing water in the ring after 30 minutes. In contrast, some of the pastures in Indian Hill had the inch of water move into the soil in less than 2 minutes.

Soil compaction is another measurement we make on our fields. High soil compaction negatively impacts root growth and water infiltration. A penetrometer is the tool we use to measure soil compaction. The tip of the penetrometer is pushed into the ground and the depth at which 300 psi is reached is recorded. At the Lewis Township site that depth averaged between 11.4 to 16.8 inches.

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