Scientists have discovered a new type of hot spring along the banks of a volcanic lake in the Philippines. These “terrestrial smokers” are cousins to submarine black smokers, hydrothermal vents on the seafloor that spew plumes of hot, nutrient-rich water and often support rich communities of life.

Terrestrial smokers might represent a missing piece of the heat budgets for many active volcanoes around the world. Getting those budgets right might help scientists better forecast the size and timing of future eruptions at volcanoes with crater lakes. Although one expert not involved with the report cautioned it might take many years of observations at multiple sites to make meaningful improvements in forecasts.

Perhaps of more immediate interest, because of their unique chemical properties, the newly discovered hot springs might harbor life forms new to science.

The team, led by Bayani Cardenas, associate professor in the Jackson School of Geosciences, discovered the springs along the banks of a crater lake inside the still active Taal Volcano, about 31 miles from Manila. Cardenas speculates that terrestrial smokers may exist in many other parts of the world where bodies of cool surface water sit atop geothermal sources, for example in rivers at Yellowstone National Park and the Newberry caldera in Oregon.

Terrestrial smoker discovered in Taal Volcano, Philippines

Terrestrial smoker discovered in Taal Volcano, Philippines. Bottom image, taken at the same spot with an infrared camera, makes heat visible.

Based on their observations and computer simulations, the researchers conclude that cool lake water seeps into the lake bed near the shore, mixes with hot, shallow groundwater and then rises back to the surface in a loop or convection cell. The water coming out of the spring flows underground at a rate of hundreds of meters per day, as compared to about a third of a meter per day for water in the High Plains of the central U.S. So much lake water is cycled through these convective cells that the entire contents of the lake are recycled in a matter of days.

“I was astounded when I calculated the flow rates,” said Cardenas. “I was running around wondering if I should hand back my Ph.D. But we rechecked everything and consulted other colleagues and now we’re confident in our results.”

The report was published Jan. 21 in the journal Geophysical Research Letters.

The team first noticed the hot springs in images taken with an infrared camera. Frame by frame analysis of the video allowed them to estimate a flow rate of about 2 centimeters per second.

Next, the team measured the temperature of groundwater at a range of depths in the sediment and at regular distances from the lake shore to map out a cross section. At that point, Cardenas saw his first signs that convection might be involved. Drawing contour lines to indicate zones of similar temperatures, he saw an unexpected pattern. Instead of horizontal lines that show a gradual increase in temperature with increase in depth, the lines were mostly vertical.

“You only get vertical temperature contours when waters are convecting, so that was the first give away,” he said. “You get this in textbooks. Theory tells you it happens. But there are not a lot of measurements in the field. So, even that I was happy with.”

Finally, he developed a simple computer model that matched the observed results and confirmed the presence of convective flow.

Bayani Cardenas (left) captures infrared video

Bayani Cardenas (left) captures infrared video of a newly discovered terrestrial smoker in Taal Volcano, Philippines

Scientists have theorized the existence of such convective cells, but this is the first direct evidence of their existence.

The spring water emerges at up to 60 degrees Celsius (140 degrees Fahrenheit), yet the springs are invisible to the unaided eye.

“If you actually stand there, it’s very quiet. It’s calm except for some wind,” said Cardenas. “You wouldn’t even know there’s water gushing out from the banks.”

Yet in infrared video, chaotic plumes of red and yellow swirl and push out into a field of blue.

The lake water is fairly acidic (with a pH of about 2 or 3) and the groundwater is only slightly acidic (pH of about 5). The two mix over a very short distance to form spring water.

“And when you have large pH contrasts like that, and metals and nutrients dissolved in the water, there are often lots of interesting things happening with bacteria there,” said Cardenas. “We just uncovered the hydraulics, the mechanics behind it, but now that we know there are these waters that are mixing there quite vigorously, there’s much more work that can be done.”

Main Crater Lake, Taal Volcano, Philippines

Main Crater Lake, Taal Volcano, Philippines

Also See: Terrestrial smokers: Thermal springs due to hydrothermal convection of groundwater connected to surface waterGeophysical Research Letters, Jan. 21, 2012