Horizontal gas drilling: perfectly safe as long as it isn’t in a watershed

An an update to our May 19 post on gas leasing for the deep Marcellus Shale play, the award-winning environmental reporter for the Pittsburgh Post-Gazette, Don Hopey, has a new piece on the lease sale state-wide that goes into detail about the possible effects of this kind of gas drilling on water quality:

The environmental concerns are primarily related to water use. Conventional vertical wells can take as much as 1 million gallons and horizontal drilling operations can use 3 million gallons or more.

Although most areas of the state where the drilling has taken place so far have plenty of water, problems have occurred. Range Resources-Appalachia and Chief Oil and Gas were cited and fined by the DEP in May for violating the state Clean Streams Law by removing too much water from small streams near their deep wells in Lycoming County. Both firms are now in compliance and have filed required water management plans.

Where the water goes after it’s used may be more of a problem. Water used to fracture underground rock and pulled back to the surface can be contaminated with brine and salt, and even pick up some radioactivity, and must be treated before it can be released into state waterways.

There are only two water treatment facilities in the state that specialize in such water treatment, but drilling companies can contract with municipal water treatment facilities if they have the capacity and capability to do such treatment.

We’ve received some interesting correspondence as a result of our last post on this issue. Someone with a Texas-based email provider assured us that the energy companies were honorable, and that we’d be passing up the opportunity of a lifetime if we didn’t sign. And a local gentleman from Decker Hollow was kind enough to inquire whether we’d be interested in joining other local landowners to engage in collective bargaining with the landsmen. When we drew his attention to a then-recent article in the Centre Daily Times (no longer available on the free web), in which a landowner who had signed away his subsurface rights to a gas company talked about the damage done and warned that doing so was tantamount to selling one’s soul, our correspondent replied: “My soul belongs to Jesus Christ. My mineral rights are for sale to the highest bidder.”

If you would like to witness to your faith in regards to the greed-driven destruction of Creation, please feel free to use the comment box below.

Cicada courtship in full swing


Video link

The cicada chorus starts around 6:00 in the morning now, and goes until late afternoon, letting up only in the case of rain. Sunnier areas such as forest openings and edges are definitely more attractive to the courting cicadas.

Further online research has revealed that Brood XIV, like most other 17-year cicada broods, includes three different species, of which we have at least two. In the above video, which I shot this morning at the Far Field and the top of First Field, the first-featured species is Magicicada cassini — the one with the more metallic call. My camera unfortunately wasn’t really up to the task of capturing them in flight; they were extremely active in the small locust trees. A box turtle behind the spruce grove at the top of First Field seemed slightly freaked out, but that’s probably my own projection. In reality, she was probably thinking slow turtle thoughts about where to find her next meal.

The final portion of the video shows Magicicada septendecim, which makes the weirder and more musical of the two calls we’ve been hearing. I was surprised by the low volume of its call at close range, but probably it was just getting warmed up. Notice how the abdomen moves as it “sings.” Here’s a description of what’s involved from the University of Michigan Museum of Zoology’s Periodical Cicada Page, the source of most of my information in this post:

As in nearly all cicada species, male periodical cicadas produce “songs” using a pair of tymbals, or ridged membranes, found on the first abdominal segment. The abdomen of a male cicada is hollow and may act as a resonating chamber; the songs of individuals are loud, and large choruses can be virtually deafening. Females of most cicada species do not have sound-producing organs. Both sexes hear the sounds of the males as well as other sounds using membranous hearing organs called “tympana” found on the underside of the abdomen.

Over the course of an emergence, males congregate in “choruses” or singing aggregations, usually in high, sunlit branches. Females visit these aggregations and mate there, so choruses contain large numbers of both sexes.

As a follow-up to the previous post, my mother emailed a cicada expert at the University of Connecticut named Dave Marshall for more information about the mud turrets she collected. He replied,

No one knows for sure why the cicadas build the turrets when they do. Most of the time they do not, and yet sometimes a whole area will have them built way up several inches. Theories ranges from differences in soil moisture/recent rainfall (nymphs somehow reducing the risk of drowning) to artifacts of differential exposure to light. People were writing about this 100 years ago in USDA pubs, and we have hardly learned any more since then!

—Dave

Return of the 17-year cicadas

17-year cicada

Walking into the house after dark, I snap on the light and notice a thumb-sized lump under my shirt, right above my navel. It’s moving, though I don’t feel anything. I lift the shirt and there, clinging to the other side of the green cotton, is a periodical cicada. I pull it off, carry it outside and give it a toss. A dry rattle as it flutters off into the night. Maybe those strange red eyes can see in the dark.

For seventeen years — an eternity for most insects — they’ve been living completely in the dark, the cicadas of Brood XIV. Silent, wingless, and pale as ghosts they have burrowed from root to root, sucking on the milk of trees. Then in late April they began to experience subtle changes in their bodies, growing new muscles, and feeling a sudden strong urge to burrow upwards. Rather than push the dirt behind them like a mole or pass it through their bodies like a worm, their powerful forelegs pushed and compacted the newly thawed earth into half-inch cylinders as they climbed.

They dug to within an inch or less of the surface, making visible mounds in the mud and leaf duff in wetter areas. Skunks and other predators dug some of them up, and for weeks we were puzzled by what turned out to be dried sections of their bore-holes scattered all over our trails. My mother took to collecting these strange artifacts in a shoebox in her study; we couldn’t remember ever seeing anything like it. If we weren’t such rationalists, we might’ve thought the Little People were taking a crash course in pottery.

periodical cicada tubes

The nymphs sat in their burrows and waited for the onset of warm nights, a wait that might have lasted only a couple weeks some years, but this year — THE year, as far as they were concerned — it was closer to six. Four days ago I saw my first red-eyed cicada on a dead raspberry cane and realized that the emergence had begun.

Yesterday — the morning after I carried a cicada in under my shirt — I waded slowly through the thick air of our first heat wave since last April, up to the crest of the ridge above my house and southwest along the trail. It sounded as if our closest neighbor in the valley were operating some kind of machinery, I thought, but couldn’t quite figure out what — an eerie metallic buzz. Then I realized: it’s them. They’re here! I picked my way down to where the slope turned steep, but still the sound was below me, coming from an open area that had been logged about a decade before. The sunny, southeast exposure must have led the cicadas there to emerge earlier than those elsewhere on the mountain.

It occurred to me that there might be some activity on the powerline right-of way. I always associate powerlines with cicadas, in part because their calls have such an electronic quality. But in fact because the powerline opening is several degrees warmer than the surrounding woods, the night before last had indeed been a scene of mass ecdysis there, the nymphs emerging from their burrows, crawling a foot or two up into the vegetation, and climbing right out of the center of their wingless thoraces. By dawn, all would’ve darkened from white to bluish gray with red-veined wings. When I arrived on the scene at mid-morning, nearly every lowbush blueberry and scrub oak shrub was dotted with adult cicadas, and some of them were beginning to take short, clumsy flights, like remote-controlled toy airplanes piloted by inexperienced hands.

I found one two-foot-tall scrub oak as heavily ornamented as a Christmas tree. When I squatted with my camera for a closer look, I noticed the translucent brown larval shells, or exuviae, clinging to the undersides of the leaves. I couldn’t help thinking that whatever whacked-out evangelical preacher first dreamed up that Rapture business must’ve witnessed a 17-year cicada emergence.

cicada exuviae

By this afternoon, I was beginning to hear them from the treetops right outside my door. I walked back up to the powerline to see if I could find any singing at close enough range to film, but they’d all moved on — up into the treetops, I suppose. I also noticed, however, an alarming number of half-inch-diameter holes stippling the ground almost everywhere in the woods mdash; there must be few species of native trees they don’t patronize. The ecological consequences of their aeration of the forest soil must be immense.

Things are going to get pretty loud here in the coming days, I think. As the aforelinked webpage puts it, “Soon after emerging, males begin their constant ‘singing’ while females remain silent. The sound made by adult males is sometimes haunting and eerie.”

After around ten days of cacophony and orgiastic mayhem, the females will begin laying their eggs and the next cycle of this longest-lived of North American insects will begin. Rather than sow their seeds in the earth, as one might expect, they instead plant them in the treetops, long ovipositors slicing like harrow blades into the twigs of trees and shrubs from nearly 80 different species. Each female lays some two dozen eggs per slit, and repeats the process until all her 400-600 eggs are gone. Where two weeks before, the adult cicadas emerged from slits in the backs of their former selves, now they insert their future offspring into slits cut into what will become their nurse-trees.

The true opposite of ecdysis, I suppose, is death, and a month from now the ground should be littered with cicada carcasses. By the time the white, ant-sized cicadas hatch in late August and drop to the ground, most traces of their parents should be gone.

Needless to say, birds, squirrels, and virtually every other macrofaunal inhabitant of the forest will have a heyday, feasting on this almost literal fat of the land. Early European settlers in eastern North America marvelled at the teeming wildlife, almost all of which have by now been sadly diminished, if not persecuted to extinction, with the exception of a few superabundant pest species such as tent caterpillars and white-tailed deer. The mass emergence of the 17-year cicadas is one of the last great spectacles of its kind.

–Dave

Cross-posted to Via Negativa. For more on periodical cicadas — much, much more — see the Cicada Mania blog. For an MP3 of the singing, go here. And since I was just talking about nature documentaries yesterday, I’d be remiss if I didn’t mention the fine film “Return of the 17 Year Cicadas” on YouTube.

“None Dwell in Their Tents”

tent caterpillar on black birch trunk

Let their habitation be desolate; and let none dwell in their tents.
Psalm 69:25 (KJV)

Eastern tent caterpillars (Malacosoma americanum) are a common sight this time of year, especially in their last instar, after they abandon their tents. They stray onto the porches and wander over the furniture, looking for protected places in which to pupate. On a visit this past Monday, my three-year-old niece Elanor decided that they were cute — not typically my own reaction — and began petting them, prompting the caterpillars to arch their heads back like housecats. Yesterday afternoon, I watched one crawling up the neck and across the face of a box turtle, which merely shut one eye while the caterpillar took its measure.

tent caterpillar tree (black cherry)

The tents began appearing at the end of April in unusual numbers, especially on black cherry trees, which are the favorite food source for tent caterpillars and occur in unnatural abundance across Pennsylvania due to 150 years of clearcut logging practices and the reversion of old fields and pastures. Black cherry is a common first-succession tree species in many forest types, and thanks in part to its relative unpalatability to white-tailed deer, it can form almost pure stands in many areas that would have formerly hosted oak-hickory, beech-hemlock, or mixed deciduous forests. Here in Plummer’s Hollow, many of our southeast-facing slopes are dominated by black cherry stands, and I figured they’d be completely defoliated by this time.

blossoming black cherry

Instead, Sapsucker Ridge is white with blossoms, filling the air with an ambrosial scent. One finds only a few black cherries as badly defoliated as the one in the second photo; the tree above is more typical. Though dotted with tents, only scattered branches have actually been stripped of their leaves.

dead tent

A closer look reveals that most of these tents are filled with dead caterpillars. The few still alive twitch spasmodically. What happened? I’d guess that the unusually cold, wet weather over the past few weeks is at fault. Nighttime temperature routinely dropped into the low 40s this month, and sometimes even into the high 30s; daytime temperatures rarely exceeded the mid-50s; and rain was almost constant for the first three weeks of the month. Not only would the cold have shut down their temperature-sensitive digestive systems for prolonged periods, but the rain would have kept them confined to their silken tents, and the two together would’ve made them much more susceptible to starvation and disease. According to the Wikipedia article on tent caterpillars,

The tent is constructed at a site that intercepts the early morning sun. The position of the tent is critical because the caterpillars must bask in the sun to elevate their temperatures above the cool ambient temperatures that occur in the early spring. Studies have shown that when the body temperature of a caterpillar is less than about 15 °C [59 °F], digestion cannot occur. The tent consists of discrete layers of silk separated by gaps and the temperature in these compartments varies markedly. Caterpillars can adjust their body temperatures by moving from one compartment to another. On cool mornings they typically rest in a tight aggregate just under a sunlit surface of the tent. … Later on in the spring, temperatures may become excessive at mid day and the caterpillars may retreat to the shaded outside surface of the tent to cool down.

Entymologist Vincent G. Dethier’s wonderful and evocative classic, The World of the Tent-Makers: A Natural History of the Eastern Tent Caterpillar (University of Massachusetts Press, 1980) describes in Chaper 13 (appropriately enough) the battery of predators and diseases that keep this native insect in check. He details the spread of a deadly virus from colony to colony, then adds:

As if that were not enough the unusually wet late spring had been kind to molds, mildews, smuts, blasts, and bacteria. A particularly virulent spore-forming species of bacterium struck many of the colonies. … The enormous population of tent caterpillars had been cropped by weather, starvation, ants, bugs, parasites, fungi, viruses, bacteria, and misadventure in general. It had been a particularly trying year. Summer had hardly begun and the die had already been cast for the year to come. There would be fewer moths, fewer egg masses, and fewer colonies of the next generation.

So a spring that spells bad news for many farmers is good news for the wood products industry, which relies heavily on black cherry in Pennsylvania. Unlike fall webworms, which come too late in the season to have much of an impact on the trees they defoliate, tent caterpillars can greatly stress the trees they defoliate during their periodic outbreaks.

As global climate change plays hob with our weather patterns, it will be interesting to watch the effects on insect outbreaks, and over the long term, on forest succession. For example, if black cherries continue to predominate as many foresters would like, more-frequent icestorms would have a much greater impact than they would if less brittle species such as red oaks and tulip poplars took their place. Warm winters are said to promote the spread of pest insects, but what about warm winters followed by cold springs? I’d heard that the state was due for some pretty large gypsy moth outbreaks this summer as well, but here in Plummer’s Hollow, at least, their caterpillars are few and far between.

–Dave
Cross-posted to Via Negativa.

Gas lease proposal: “You may already be a sucker!”

gas lease proposal 1

gas lease proposal 2

gas lease proposal 3

Alert readers will have already discovered several amusing things about this missive, which arrived unsolicited in this morning’s mail:

  • Though purporting to be a lease proposal for Blair County in the subject line and first paragraph, it references the neighboring Cambria County in the “terms and conditions.” One might take this for a simple copy-and-paste error, except that the reference is specifically to the “initial bonus consideration” of $500.00 per acre. I’m not a lawyer, but it doesn’t take a whole lot of imagination to picture them saying, after one had already signed such a proposal in great anticipation of instant wealth (it would amount to over $300,000 for us), “Sorry, your land isn’t in Cambria County, so we don’t owe you anything!”
  • “The royalty rate in the lease will be 1/8.” Uh, 1/8 of what, exactly? More weasel words designed to trap the unwary — or just extremely vague/sloppy language from people who do this for a living?
  • It hardly takes any more time and ink to type “Carrizo” than CRZO, but the stock-ticker symbol is used throughout. Is this an attempt to garner respectability, to intimidate, or both?
  • “CRZO’s activity in the area” could be harmed by the disclosure of the terms. Gee, I can’t imagine how!
  • If not signed and returned by May 12, “the offer shall immediately become null and void.” OH NO, PAPPY, WE’RE SCREWED! QUICK, CALL ‘EM UP AND BEG FOR AN EXTENSION!
  • Despite being dated May 5, the letter is actually postmarked 16 May 2008.
  • The stamp cancelation text quotes John Adams: “Let us dare to read, think, speak, and write.” Yes, let’s.

The Google Finance page for Carrizo (linked above) makes note of their “acreage in shale plays in … the Marcellus in Pennsylvania/New York.” That is what’s at issue here: a deep deposit of natural gas that may be accessable from various parts of the Ridge-and-Valley geologic province, not just the Allegheny Plateau to our west and north where the shallower gas plays occur. As the New York Times put it last month:

A layer of rock here [in Pennsylvania] called the Marcellus Shale has been known for more than a century to contain gas, but it was generally not seen as economical to extract. Now, improved recovery technology, sharply higher natural gas prices and strong drilling results in a similar shale formation in north Texas are changing the calculus. A result is that a part of the country where energy supplies were long thought to be largely tapped out is suddenly ripe for gas prospecting. […]

Natural gas in the Marcellus and other shale formations is sometimes found as deep as 9,000 feet below the ground, a geological and engineering challenge not to be underestimated. The shales are sedimentary rock deposits formed from the mud of shallow seas several hundred million years ago. Gas can be found trapped within shale deposits, although it is too early to know exactly how much gas will be retrievable.

The Times article refers to the rush to sign leases as a feeding frenzy, and from what we hear, that’s not too far off the mark. Reportedly, some folks in Sinking Valley have already signed leases offering as little as $5.00 per acre! Other offers have gone as high as $600 per acre.

It probably goes without saying that we will never sign away any subsurface rights here on our property. In addition to very real concerns about groundwater contamination (Marcellus shale contains uranium), the main problem with gas drilling is habitat fragmentation. The Pennsylvania Department of Conservation and Natural Resources recently caved to pressure and opened up 75,000 acres of state forest land to gas drilling, reversing an earlier ban. Their claim is that the greater spacing between wells will lead to less forest fragmentation than would be the case with ordinary, shallow-well drilling, but environmentalists such as the Allegheny Defense Project’s Ryan Talbott, quoted in the linked article, respond that since the pads will be much larger, the difference is neglible. And it’s hard to see how more widely spaced clearings would reduce the number of roads and pipeline right-of-ways very much. Such linear corridors are the worst for spreading invasive plant species and giving access to nest predators on interior forest-dwelling birds, not to mention all-terrain vehicles (maybe that’s what the DCNR spokesflack meant by “other forest uses”).

Many interior forest species are already in steep decline, and it simply isn’t worth endangering them for what might be, at most, the equivalent of two years of total U.S. consumption if every recoverable cubic foot were exploited. We’re appalled that the official stewards of our state wildlands would consider trashing them to feed America’s fossil fuel addiction.

Well, people with dollar signs in their eyes are rarely given to honest discourse, be they state officials or “independent petroleum landmen.” But one thing is certain: geology-speak is really, really cool.

Bedding in the Marcellus is moderately well developed and fissile. Its upper reaches are marked by anoxic dark shales which indicate the Kačák Event, a late Eifelian stage marine anoxic event also associated with an extinction event. […]

The black and gray shales of the Hamilton Group mark the first terrigenous sediments deposited by the erosion of the Acadian Mountains. These sediments were deposited in the Acadian foredeep basin early in the Acadian orogeny, as part of a deep water sequence that continued to form the overlying Brallier Formation and Harrell Formation. The Marcellus Shale was formed from the very first sediments deposited in this very deep, sediment starved, anoxic trough. The dark shale is composed of flysch, a fine mud deposited in the deep water, burying the underlying Onondoga limestone beds.

It would be nice if the Kačák Event were the last extinction to be associated with these deposits.

–Dave

2008 International Migratory Bird Day

indigo bunting in the rainIt was 46 degrees and raining when I awoke at 6:00 a.m., but the birds sang anyway, especially the two male Baltimore orioles competing for a female in our yard. I managed to count 19 species from our veranda and front porch before breakfast, including an eastern kingbird that had first appeared at the edge of First Field on Thursday. Later in the morning, carrying an umbrella, trying to protect my binoculars from the rain, keeping my feet dry, and staying warm, all while counting birds, was no fun. However, I added 15 more species to my list, including many singing indigo buntings in the field and wood thrushes in the woods. Worm-eating warblers, ovenbirds, black-throated green warblers, hooded warblers and even a black-throated blue warbler also sang. About the only birds I saw were those in the fields. The rest I counted by ear.

After a rest and a change into dry clothes and boots, I went more happily out in the sunny afternoon. Down our road I walked to get Acadian flycatchers and common grackles. Then I climbed up to the former clearcut where I hit the jackpot — a migratory flock of warblers that included many American redstarts. I also heard both a cerulean warbler and a northern parula. By the time I reached home, at 5:30 p.m., I had 55 species — a respectable total for a solo performance. Then, after dinner, I looked at my mertensia patch for a ruby-throated hummingbird and there he was. And, right on schedule, our resident whippoorwill called outside at 8:45 p.m. As usual, the eastern towhees (13) and red-eyed vireos (12) were the most abundant species or at least singers. Hooded warblers won the warbler contest at eight, closely followed by American redstart (7). Wood thrushes (8) scarlet tanagers (8) and indigo buntings (7) also made a good showing, and I did have many wonderful sightings of the tanagers and buntings.

© Marcia Bonta

Compare last year’s IMBD report.

How much carbon does our forest sequester?

locomotiveThe cover story in the current (Spring 2008) issue of OnEarth magazine, called The Giving Trees, includes some important information about the value of intact, mature forests. The author, Sharon Levy, describes something called the eddy flux method of measuring the flows of carbon dioxide and water vapor into and out of forests. Devices mounted on towers in forest stands measure winds and gas exchanges at incredible levels of detail and accuracy.

For anyone who might be a little fuzzy on the chemistry involved here, Levy offers a brief refresher course:

Plants take in CO2 and harness the energy of the sun to drive the chemical reaction that melds carbon with water, producing the substance of stem and leaf and releasing oxygen. When darkness or drought bring this process of photosynthesis to a halt, plants respire, just as humans do. That is, plants breathe in oxygen and exhale CO2. But over the long life span of trees in an undisturbed forest, huge reservoirs of carbon are stored for great stretches of time in the organic matter in soil as well as in living wood.

Most relevant to Plummer’s Hollow, Levy describes measurements of the intake and storage of carbon done at the Harvard Forest, in Petersham, Massachusetts, starting in 1989. The stand that scientists measured, predominantly an oak-maple forest, had been flattened by a hurricane in 1938. In the first year of the study, the 50-year-old forest was absorbing 0.8 tons of carbon per acre per year.

Previous calculations by ecologists had suggested that a forest of that age should be reaching its maximum ability to absorb carbon, but measurements at the Harvard Forest 15 years later showed that the rate of carbon sequestration had doubled. In other words, a 65-year-old forest absorbed 1.6 tons of carbon per acre per year. Other studies suggest that much older forests may continue to store carbon as they age — the older the trees, probably, the more and more carbon they store.

The idea the author is driving at is that there may be some very convincing arguments, in addition to familiar ones about wildlife habitat and water conservation, for preserving a lot of forest lands uncut. Older forests help in the fight against global warming.

The Harvard Forest is of course not Plummer’s Hollow, but we also own a mostly oak-maple forest. Excluding about 80 acres out of our 650 acres of land, where a savage cutting was performed 16 years ago before we could buy it, and excluding another 70 acres of recent blowdowns, open meadows, talus slopes, and places that have been selectively logged in the last 30 years, we still have at least 500 acres of forest ranging from 80 to 120 years old.

A 15- to 20-acre section of Laurel Ridge inside and above the large deer exclosure is closer to 200 years old, but much of the remaining 500 acres was last cut in the late 19th or very early 20th centuries. Thus, if the comparison to the Harvard Forest is roughly valid, I would speculate that the forest land in Plummer’s Hollow may be capturing 800 tons of carbon per year, and perhaps quite a bit more.

But other than showing that the property captures so many tons of carbon per year, how does this stack up against the amount of carbon we as a family contribute to the atmosphere through our annual activities? A variety of websites provide simple calculators so people can input data relating to their daily lives — home heating, transportation, consumption of goods — and get an estimate of how much carbon they contribute to the global atmospheric problem.

Ignoring the carbon footprint of the Guest House and its occupant, but including our one jet flight this year, the Carbon Footprint Calculator adds together a variety of estimates and comes up with a figure of 14.134 tons per year. The calculator provided by the Nature Conservancy returns a figure of 42 tons of carbon per year. A third calculator shows that we contribute 10.2 tons per year. Averaging those three calculations we come up with 22 tons per year.

The conclusion: our (mostly) healthy, moderately old, primarily hardwood forest offsets the carbon footprint of roughly 36.3 households with a reasonably low-consumption lifestyle like ours. Or to express it another way, we could live 25 times more extravagantly, wasting resources wildly, and still be net savers of carbon simply by preserving our private forest from being logged.

Not to sound greedy, but if state and federal governments are serious about combating global warming, perhaps forest landowners should get tax credits for not cutting their woods, comparable to the subsidies long enjoyed by farmers who enroll arable land in the Conservation Reserve Program.

— Bruce Bonta