It is now Day 9 and we have all but completed
our mission. We remain inside the caldera we arrived at yesterday
with a clear view of three majestic peaks. This morning we revisited
Volcan Miravalles in order to sample
gases at the Miravalles Geothermal Plant.
In the afternoon we drove out of the vast, windblown savanna of
the caldera floor and entered the dry forest on the flanks of active
Volcan Rincon de la Vieja. In a national park known as Las Pailas,
we hiked past a broad
waterfall cascading down the face of a prominent basaltic
lava flow. We collected gases from hot springs and an effervescent
pond, and observed a boiling
mud pot known as the "volcancito."
The
dry forest is yet another of Costa Rica's many woodland
habitats. Desiccated by high winds that blow relentlessly across
the savanna, the dry forest is a unique habitat dominated by a gigantic
variety of fig tree. These have enormous
trunks that fan out into convoluted root systems that crawl
across the ground, enmeshing the forest floor in a matrix of roots
and rocks. Vines drape downward and creepers reach upward, seeming
at times to grip the forest in a stranglehold. Various shrubs and
succulents occur throughout the understory, comprising a habitat
known to gardeners as a zeriscape. The forest abounds with wildlife
such as turkeys, jays, vultures, iguanas, and snakes. Troupes of
monkeys
were frolicking in the canopy. Despite reports that these monkeys
are known to throw fecal matter at onlookers, they didn't seem bothered
by our presence. We were also delighted to finally see the giant
blue "morpha" butterfly, a national symbol of Costa Rica.
Today's scientific reports begin with Toby's account of sampling
geothermal gases:
The geothermal reservoir at Miravalles is a vast underground area
that contains water and dissolved gases at high temperatures (above
200°C) and pressures. Geothermal wells tap the reservoir, which
lies at a depth of roughly 1,500 meters, and the hot water is brought
to turbines on the surface via large diameter pipes. These pipes
have valves that allowed us to collect the gas samples. Because
the pressure in the pipes is very high, an ICE employee attached
a steam separator to the valve, thereby reducing the outlet pressure
to about three bars (the pressure of a bicycle tire). We collected
good samples representative of gases dissolved in the geothermal
reservoir.
Toby's student, Mindy Zimmer continues:
After we sampled the wells at Miravalles, we headed for the national
park at Rincon de la Vieja. Though the hike was easy, we had to
be careful once we reached the hot springs. The constant venting
of volcanic gases has significantly altered the landscape,
so the ground is very unstable. After picking our way through the
rocks, we found a good site
to sample. The water was very acidic and hot (83°C), demonstrating
the constant activity of the volcano.
We mentioned before that the volcanic gases contain sulphuric acid,
and my pants are dramatic proof. I sat down near some hot springs
yesterday, and less than 24 hours later, holes had appeared
in my pants! I think this gives new meaning to the phrase
"hot seat."
|