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HomeMy WebLinkAboutCOM 0744.006 2022-2024 P /Fc Res.t10-21{ G.v r"t y LE t1i Y HAM 20211 R -Li Ali 11: 2 Aloha Kakou. My name is Paul Kuykendall. I'm a farmer that lives on lower Pohoiki Road. I'm a co-founder of the Waihu 0 Puna Makai Watershed Coalition. Our kuleana is to malama the watershed and the nearshore waters of Puna. I'm testifying in support of Resolution 443-24 to fund a USGS study of the lower Puna watershed. We don't have rivers in lower Puna , other than rivers of lava, but we have a fresh water lens that sits on top of seawater just under the surface of the ground. This freshwater lens, which sits just below very porous rock, supplies water for our homes and farms through private wells and eventually flows to the shore, where it fills ponds and flows into the near-shore ocean. environment. This freshwater and the nutrients it carries feeds the endemic opae 'ula shrimp that live in ponds and fish that live in the near-shore reefs. When geothermal steam or brine are released at or near the surface mauka of lower Puna either intentionally or accidentally , the heavy metals and other contaminants seep into the ground and flow directly into our freshwater lens, negatively affecting people, plants, animals and fish. There are two incidents in Puna's history of geothermal development that concern us about contamination of our watershed. The first incident was the HGP-A geothermal well, drilled in 1976. The first geothermal plant in Puna, HGP-A was presented as a strictly experimental, 6-month project. This is significant, because the EIS for the project identified mercury, among other heavy metals, as a major toxin in the geothermal brine that would be open-vented from the well into the air and onto the ground in unlined ponds. The EIS stated that since it was only a 6 month test, the load on the environment would be acceptable. The "Environmental Assessment of the Hawaii Geothermal Project Well Flow Test Program," published in November 1976, states: Heavy metals, notably mercury, are also evolved in an aerosol state from geothermal fluids. Mercury tends to accumulate over long periods of time in plants and can be concentrated in higher levels of the food chain. (my emphasis) Nevertheless, no significant accumulation is IIrr'',, ff Comm. No. '1"`'�. (0 Ref. To: Ref. pate ,.NA ® 5 2024 expected during the six-month well test. " (my emphasis). The so-called six-month test went on open-venting geothermal toxins, which included heavy metals, for eight years. In 1982, despite commitments to the public that the test would be experimental, a three-megawatt commercial power plant went on line, run by HELCO. No community meetings were held explaining the change and no permits were issued by the county. The geothermal power plant continued for a total of eight years and was shut down in 1989. During its operation, HGP-A dumped the toxic geothermal brine into unlined ponds that fouled the air, land and seeped into groundwater. Due to the toxins in the geothermal brine, the site eventually became an EPA superfund site. This was Puna's first experience of geothermal power production. The second experience was the 1991 Puna Geothermal Venture Drilling well blow out at well KS-8. Mayor Lorraine Inouye declared a state of emergency. Hawaii County commissioned Goddard & Goddard Engineering to study the impact. The study found: • Local H2S concentrations were elevated above health significance levels and correlated with health complaints. • Regional H2S transport of the KS8 venting plume cloud was documented by visual sightings, regional and local wind assessments, and the chronology and position of health complaints extending beyond 10 miles (16 km). • Estimates of emissions, other air toxics, and impacts are known to be of significant public health concern. During the blow out, geothermal brine and steam flowed uncontrolled for 31 hours. This brine seeped into the ground. This was bad enough, but it turned out that the contamination was worse than we thought. A USGS study in 1994 stated, "Although the uncontrolled steam discharge at the KS 8 wellhead lasted for only 31 hours, temperature measurements indicate that steam continued to leak upward past the 13-inch casing shoe at 2,128 ft until the well was finally quenched and plugged several months later. (my emphasis)" This indicates the well was contaminating soil and groundwater months. HGPA and the 1991 well blowout are two reasons we are concerned about geothermal contamination of our freshwater resource. In 2013, the Adler Report, commissioned by Hawaii County , recommended USGS study whether the wells, ponds and the watershed in lower Puna showed any signs of geothermal contamination. In 2015, that study was conducted by USGS, but did not provide sufficient evidence to unequivocally indicate or rule out adverse effects from geothermal energy production. Unfortunately, it was unable to fulfill some of its objectives such as testing water wells down-gradient from PGV and testing off-shore springs. The study recommended that future studies "focus on the hot groundwater wells,... and on offshore vents of warm water, using underwater sampling techniques as necessary" In December, 2020, the Waihu 0 Puna Watershed Coalition wrote a letter to Mayor Roth requesting a follow up study. Since then, we have been working with the community and Ashley to develop a more comprehensive study, which will include additional testing sites and additional tests for contaminants. The study this resolution describes will include consultations with community members regarding water sample sites and allow them to accompany USGS field teams for the sample collection to foster observational learning, build local knowledge in scientific methods, and foster community understanding and trust in the study's methodologies. The study will help establish baseline water quality data and inform plans for regular water quality monitoring in future years. Mahalo to the council for considering this resolution and mahalo to Ashley for working with the community to develop this proposal. We appreciate this. opportunity to turn questions about our watershed quality into answers about the current state of our wells, ponds and near shore waters. These answers will guide future actions to protect our most precious resources in lower Puna—our water, our people and our `Aina. Aloha, Paul Kuykendall Waihu 0 Puna Watershed Coalition