WEBVTT

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ZEYNEB MAGAVI: A very,
very warm welcome,

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but I am going to turn
it over to our hosts

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here at MIT to do
the first welcome.

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CHRIS RABE: Cool.

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Can we move the slide one?

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Oh, I got it.

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OK, let's see.

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Do you want to talk
about flying the plane?

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ZEYNEB MAGAVI: Oh my gosh, I do.

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All right.

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We're going to get our--

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this is actually the perfect
slide for our little start

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here, which we
coordinated and rehearsed.

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I love this picture,
because it basically

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embodies everything that
is the organization, HEET,

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and the process of moving
forward in uncertainty.

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So we are here today with this
amazing course, which you're

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about to hear more about,
building and fixing

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the airplane while flying it.

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So I really want to know
how that picture came to be,

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but it stands.

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So to that end, I want to
acknowledge that we've never

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done this before.

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It really can't-- it can't go
wrong because of the people

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in the room.

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And we're really excited
to see where it does go.

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And we're also really excited
to learn from it, as always.

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So for example, there
is a lovely whiteboard

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outside during your coffee
breaks that has two sides to it.

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One side is, who are the people
and the ideas and the topics

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that we need to add
to this conversation?

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Please put your ideas there.

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And the other one is
just general feedback.

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Thoughts, ideas, learnings,
changes, et cetera.

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Please don't hesitate to
give us the gift of feedback.

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And now for the part we probably
should have started with, hi.

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I'm Zeyneb Magavi.

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I'm the Executive
Director of HEET.

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And HEET is a nonprofit
that has been focused

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on trying to solve climate
change for a lot of years,

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from a community level in
the beginning and scaling.

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So we'll talk more about the
topic of geothermal networks

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in a few minutes.

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But first, I want to just
express a lot of gratitude

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to all of you for being present
and here and offering yourselves

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to this conversation and
journey that might look

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a little hazardous at times.

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And also, I want to just thank
MIT, the amazing institution,

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and both Chris and Curt
for being our hosts.

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And I want to turn it over to
them to introduce themselves.

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CHRIS RABE: Thanks,
Zeyneb, So yeah,

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I'm so excited to
welcome HEET here to MIT.

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My name's Chris Rabe.

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I'm the Education Program
Director at MIT's Environmental

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Solutions Initiative.

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The education program mission is
to better understand and expand

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climate education across
both disciplinary contexts

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and institutional contexts.

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And I'd really like to make sure
that our education, our projects

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and activities are connecting
to real-world scenarios.

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So it's so exciting to
be working with HEET

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and re-envisioning the
way that energy can work.

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This is a part of a few
other collaborations.

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So we started a new course
called Environmental Justice,

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Science, and Technology.

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And that has a massive
open online version.

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And HEET participated with a
really interesting lecture.

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And then also, we're working
on some K through 12 curriculum

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in this Day of Climate
project through Open Learning.

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So it's just really exciting
to be doing both the K

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through 12 space and the higher
education space with HEET.

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So again, just so excited
for HEET to be here.

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Thank you so much.

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CURT NEWTON: Good
morning, everyone.

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My name's Curt Newton.

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I'm Director of MIT
OpenCourseWare, another

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of the co-hosts for this event.

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And we're thrilled to be
participating in this,

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not just to host, but
also because this is all

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going to flow out to the world.

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We're recording, as you know.

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We've got video set up
here to capture and then

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share back with the world this
important emerging knowledge.

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We've had the pleasure
at OpenCourseWare

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with serving this broader
mission of unlocking

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and empowering people around
the world, both learners

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and educators, for
over two decades.

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You see a screenshot
of the first engagement

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that we had with HEET, with
Zeyneb, a January session

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workshop that we
did about gas leaks.

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Part of the-- maybe
the origin story

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for what we're
getting up to here.

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And what we do at
OpenCourseWare is not just

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sharing this knowledge
again, but to do so

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in ways that encourage
practices of sharing

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and the feedback that
gets set up through this,

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through this broader
open knowledge ecosystem.

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So HEET, for
instance, putting all

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of these resources
in an open library

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and gathering together in a
really nimble, generative way,

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create this knowledge new.

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I'm recalling here at
MIT in January 2020,

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just before all kinds
of stuff got shut down,

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we hosted here some
design charrettes

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to start this process.

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And just what a
thrill it is to us

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to be part of this
journey together.

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And just to let you
know, if you're not

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familiar with OpenCourseWare,
the reach of this content

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is considerable
around the world.

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70% of our visitors come
from outside North America.

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So the interest around
the world that's

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developing in
these technologies,

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we want to plug into that.

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Our website gets millions
of visits every year.

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And our YouTube channel
where the videos also live

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is also a really important
point of engagement.

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With over 5.5 million
subscribers on our YouTube

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channel, it's the
largest subscriber base

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of any educational
institution out in the world.

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So rest assured that what
we come up with today,

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flowing out to the world is
going to reach a lot of people.

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And it's really
going to, I think,

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further the work that we're all
trying to get up to, so welcome.

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ZEYNEB MAGAVI: But don't
hesitate to talk after that.

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[LAUGHS]

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ISABEL VARELA: Thank you.

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My name is Isabel Varela,
Science Director at HEET.

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And I wanted to
briefly share, this

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is the HEET team that
is here to help you.

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If you have any questions, don't
hesitate to reach out to us.

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We've put together an
incredible program.

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HEET takes the aim to look
at for solving a problem.

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Identify all the
stakeholders that

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need to be involved to
make that change happen.

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And this two-day
course reflects that.

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As you see, we have eight
sessions for each day,

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and they vary from, what is the
challenge that we need to solve?

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What are the policies that need
to be implemented to do that?

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What are the
learnings that we can

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get from the geothermal networks
that are implemented today?

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What are the design principles
that should be applied?

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And learn from case studies.

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We are excited that
you're here, and we

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hope you get most out of
this course and participate.

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Your participation makes
the course more lively.

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ZEYNEB MAGAVI: And--

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ISABEL VARELA: We have
an incredible lineup

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of 28 speakers that are here.

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Some of them have come
from around the country

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to be here in these two days.

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And we have organizations
represented from universities,

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gas utilities,
regulators, design firms

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and community-based
organizations.

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So thank you for
all the speakers

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that are here and making
this course happen.

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CURT NEWTON: Just a quick
note about the nature

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of the recordings that
we're going to be doing.

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So what we'll be
sharing with the world

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will be the talks, and just
the videos of the talks.

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There's a really important
Q&A interaction segment

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that will happen for
each of the sessions,

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and we will not be sharing those
straight out with the world.

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We want to have a frank,
completely unconstrained

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conversation here in the room.

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Our hope is,
though, that we will

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be sharing some kind of notes
and takeaways, some summaries

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and syntheses, from
those conversations.

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But rest assured, unless
you are a speaker up here,

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we're not expecting you
to show up in these videos

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that we share on OCW.

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If you have any concerns
or questions about that,

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please reach out to me.

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Be in touch.

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But hopefully, that's all right.

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OK.

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ZEYNEB MAGAVI: Yeah.

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And our format is
that each session

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is going to have a few
brief presentations.

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Every single one of the
speakers could likely

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speak for hours on
any one of the topics,

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and we're so aware of that.

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But we also thought that
the most valuable thing

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here in the room is the
interaction between.

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So for many speakers, there
will be a longer recorded

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piece of content that's
attached to the courseware.

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But in the room, we're going to
keep the presentations brief so

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that we can get to that part of
interacting between and talking

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and interacting with all of you.

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And we've got a Slido--

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it's a little app that we'll
introduce in a second--

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for you to engage so
we can get more voices

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involved more quickly so that we
can get the conversation going.

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And then I've said this already.

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I'm going to say it again.

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This is our first go at this.

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I love that you mentioned the
previous wonderful events.

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The first one was a
hackathon to design a tool

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to measure gas leaks.

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And the second one
was a charette.

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And now we're
trying this content.

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So you will be part of
making it wonderful today,

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so please don't
hesitate to participate.

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All right.

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ISABEL VARELA: One last
comment for housekeeping.

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We have breakfast in
the morning outside.

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We'll have coffee breaks.

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We'll have lunch outside.

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Food is allowed to come
here if you want to.

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Restrooms are here
immediately to the right,

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and there's another one in
the hallway to the left.

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ZEYNEB MAGAVI: Thank you.

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And Isabel planned
this incredibly.

00:10:53.360 --> 00:10:54.810 align:middle line:90%
So-- [LAUGHS]

00:10:54.810 --> 00:10:55.310 align:middle line:90%
[APPLAUSE]

00:10:55.310 --> 00:10:56.090 align:middle line:90%
ISABEL VARELA: With the team.

00:10:56.090 --> 00:10:56.700 align:middle line:90%
With the team.

00:10:56.700 --> 00:10:57.300 align:middle line:90%
ZEYNEB MAGAVI: Yeah, yeah, yeah.

00:10:57.300 --> 00:10:57.985 align:middle line:90%
With the team.

00:10:57.985 --> 00:11:00.720 align:middle line:90%
[LAUGHS] All right.

00:11:00.720 --> 00:11:03.480 align:middle line:84%
So one of the things
that we always do--

00:11:03.480 --> 00:11:05.975 align:middle line:84%
and I know Curt is
always in on this--

00:11:05.975 --> 00:11:06.750 align:middle line:90%
it's open.

00:11:06.750 --> 00:11:11.370 align:middle line:84%
So your backgrounds here in the
room are all over the spectrum.

00:11:11.370 --> 00:11:13.230 align:middle line:84%
We think that's
beautiful and exciting.

00:11:13.230 --> 00:11:15.147 align:middle line:84%
And one of the things
we're going to try to do

00:11:15.147 --> 00:11:19.820 align:middle line:84%
is make sure that we
move between introductory

00:11:19.820 --> 00:11:20.970 align:middle line:90%
and advanced.

00:11:20.970 --> 00:11:23.570 align:middle line:84%
And it may be a fire
hose, but that's

00:11:23.570 --> 00:11:25.790 align:middle line:90%
why we're providing coffee.

00:11:25.790 --> 00:11:29.150 align:middle line:84%
So I get to start us
off with two quick ideas

00:11:29.150 --> 00:11:30.890 align:middle line:84%
for the entire two
days, and then we

00:11:30.890 --> 00:11:32.750 align:middle line:84%
have the most
amazing panel to get

00:11:32.750 --> 00:11:39.560 align:middle line:84%
going at a very high-scale
level of the whole world.

00:11:39.560 --> 00:11:46.740 align:middle line:84%
So our new tagline
at the moment at HEET

00:11:46.740 --> 00:11:49.710 align:middle line:90%
is think thermal together.

00:11:49.710 --> 00:11:51.720 align:middle line:84%
It kind of embodies
a lot of the pieces

00:11:51.720 --> 00:11:54.180 align:middle line:84%
that we've been learning
over the past few years

00:11:54.180 --> 00:11:58.140 align:middle line:84%
as we move forward with
networking, ground source heat

00:11:58.140 --> 00:11:59.950 align:middle line:90%
pumps, or geothermal heat pumps.

00:11:59.950 --> 00:12:04.140 align:middle line:84%
And that idea of
getting a problem

00:12:04.140 --> 00:12:08.470 align:middle line:84%
solved by working together,
that's always been there.

00:12:08.470 --> 00:12:13.900 align:middle line:84%
But the piece where we realized,
as we spoke about geothermal,

00:12:13.900 --> 00:12:17.340 align:middle line:84%
that thermal energy
itself wasn't always

00:12:17.340 --> 00:12:21.270 align:middle line:84%
on the table in the
climate solution space,

00:12:21.270 --> 00:12:23.800 align:middle line:84%
that people weren't thinking,
they weren't measuring,

00:12:23.800 --> 00:12:26.080 align:middle line:84%
they weren't talking
about thermal energy.

00:12:26.080 --> 00:12:27.780 align:middle line:84%
So I'm going to
just briefly start

00:12:27.780 --> 00:12:31.320 align:middle line:84%
by getting us to take a moment
to put on our thermal energy

00:12:31.320 --> 00:12:35.760 align:middle line:84%
glasses, and then I'm going to
do a little bit of housekeeping

00:12:35.760 --> 00:12:39.790 align:middle line:84%
on language-- so
that terminology,

00:12:39.790 --> 00:12:42.360 align:middle line:84%
and then we'll move
to our first panel.

00:12:42.360 --> 00:12:45.340 align:middle line:90%
So think thermal.

00:12:45.340 --> 00:12:46.960 align:middle line:90%
Let's start with that part.

00:12:46.960 --> 00:12:48.760 align:middle line:90%
This is an image.

00:12:48.760 --> 00:12:51.430 align:middle line:84%
If you use a thermal camera,
which actually, we've recently

00:12:51.430 --> 00:12:56.150 align:middle line:84%
purchased for the sheer fun of
it, if you use a thermal camera,

00:12:56.150 --> 00:12:58.150 align:middle line:90%
you see things differently.

00:12:58.150 --> 00:13:01.100 align:middle line:84%
Our eyes don't do that,
which may be why we don't--

00:13:01.100 --> 00:13:03.100 align:middle line:90%
we ignore it so often.

00:13:03.100 --> 00:13:07.280 align:middle line:84%
But there is a huge amount of
thermal energy in our Earth.

00:13:07.280 --> 00:13:10.280 align:middle line:84%
And really, if you stop and
think about climate change,

00:13:10.280 --> 00:13:14.440 align:middle line:84%
what is climate change except
a thermal energy regulation

00:13:14.440 --> 00:13:16.390 align:middle line:90%
problem?

00:13:16.390 --> 00:13:20.050 align:middle line:84%
And so if that's what it is,
and we talk about the rising

00:13:20.050 --> 00:13:24.070 align:middle line:84%
temperature in air, well,
the kind of stunning thing

00:13:24.070 --> 00:13:27.820 align:middle line:84%
is that there are a bunch
of papers calculating

00:13:27.820 --> 00:13:30.130 align:middle line:84%
how much thermal
energy the Earth

00:13:30.130 --> 00:13:35.050 align:middle line:90%
has absorbed since, say, 1960.

00:13:35.050 --> 00:13:41.335 align:middle line:84%
And it's 630 times,
approximately,

00:13:41.335 --> 00:13:44.550 align:middle line:84%
all of the energy
humanity uses every year.

00:13:44.550 --> 00:13:49.260 align:middle line:84%
So I was delighted to learn
a new metric of energy,

00:13:49.260 --> 00:13:51.480 align:middle line:90%
the zettajoule.

00:13:51.480 --> 00:13:55.180 align:middle line:84%
Apparently, humanity uses
half a zettajoule a year,

00:13:55.180 --> 00:13:56.850 align:middle line:90%
all the energy we use.

00:13:56.850 --> 00:14:05.070 align:middle line:84%
And every year, our oceans alone
are absorbing five zettajoules.

00:14:05.070 --> 00:14:10.020 align:middle line:84%
So that's a kind of stunning,
gut-wrenching challenge.

00:14:10.020 --> 00:14:12.730 align:middle line:84%
But if you start to think
about thermal energy,

00:14:12.730 --> 00:14:15.730 align:middle line:84%
if you start to look at it,
if you start to measure it,

00:14:15.730 --> 00:14:19.580 align:middle line:84%
it's also an
extraordinary opportunity.

00:14:19.580 --> 00:14:22.560 align:middle line:84%
It's a massive amount
of energy all around us

00:14:22.560 --> 00:14:25.620 align:middle line:90%
that we have been ignoring.

00:14:25.620 --> 00:14:28.150 align:middle line:84%
And we have the
technology to tap it,

00:14:28.150 --> 00:14:31.740 align:middle line:84%
which is what we're here
to talk about today.

00:14:31.740 --> 00:14:37.110 align:middle line:84%
A recent report from the IEA had
a rather stunning statement that

00:14:37.110 --> 00:14:39.430 align:middle line:84%
kind of defines part
of our two days,

00:14:39.430 --> 00:14:42.380 align:middle line:84%
that "The technical potential
of geothermal would be more than

00:14:42.380 --> 00:14:44.400 align:middle line:84%
enough to meet
all heat demand--"

00:14:44.400 --> 00:14:47.150 align:middle line:84%
that's all heat demand, and
they're not even talking about

00:14:47.150 --> 00:14:47.750 align:middle line:90%
cooling--

00:14:47.750 --> 00:14:49.682 align:middle line:84%
"in Africa, China,
Europe, Southeast Asia,

00:14:49.682 --> 00:14:50.640 align:middle line:90%
and the United States."

00:14:50.640 --> 00:14:52.340 align:middle line:84%
So I read that and I thought,
well, what about those other

00:14:52.340 --> 00:14:52.840 align:middle line:90%
places?

00:14:52.840 --> 00:14:57.110 align:middle line:90%


00:14:57.110 --> 00:15:00.650 align:middle line:84%
But I also want to just add
into the conversation, not just

00:15:00.650 --> 00:15:05.960 align:middle line:84%
that geothermal energy that's
in the world all around us,

00:15:05.960 --> 00:15:10.320 align:middle line:90%
but also the energy we waste.

00:15:10.320 --> 00:15:15.020 align:middle line:84%
All that energy we do use,
combust, burn, et cetera,

00:15:15.020 --> 00:15:18.470 align:middle line:90%
the majority of it is wasted.

00:15:18.470 --> 00:15:21.750 align:middle line:84%
And a large, large portion
of that is thermal energy.

00:15:21.750 --> 00:15:24.350 align:middle line:84%
So that is where we
can think about yet

00:15:24.350 --> 00:15:28.400 align:middle line:84%
another untapped
resource all around us.

00:15:28.400 --> 00:15:29.100 align:middle line:90%
All right.

00:15:29.100 --> 00:15:33.020 align:middle line:84%
So taking the optimistic part
of, wow, there's thermal energy

00:15:33.020 --> 00:15:34.970 align:middle line:84%
all around us, this
is really exciting,

00:15:34.970 --> 00:15:37.370 align:middle line:84%
what we're here to do
today for two days is talk

00:15:37.370 --> 00:15:42.670 align:middle line:84%
about the technology we believe
is there and ready for us

00:15:42.670 --> 00:15:46.930 align:middle line:84%
to tap it and turn
it into a solution.

00:15:46.930 --> 00:15:51.374 align:middle line:84%
Talking about that technology
sometimes has some challenges.

00:15:51.374 --> 00:15:54.680 align:middle line:84%
[LAUGHS] We try to
bring everyone together.

00:15:54.680 --> 00:15:57.520 align:middle line:84%
Lots of different groups have
lots of different language.

00:15:57.520 --> 00:16:00.190 align:middle line:84%
This is the HEET
approach that we've

00:16:00.190 --> 00:16:05.050 align:middle line:84%
been talking about earlier
with many other events.

00:16:05.050 --> 00:16:07.300 align:middle line:84%
You're now part of
it being in the room.

00:16:07.300 --> 00:16:09.580 align:middle line:84%
So coming together
around what we

00:16:09.580 --> 00:16:12.380 align:middle line:84%
mean when we say things
is one way to start,

00:16:12.380 --> 00:16:14.530 align:middle line:90%
get us all on the same page.

00:16:14.530 --> 00:16:20.962 align:middle line:84%
And the first thing we have is
a little quick intro visual,

00:16:20.962 --> 00:16:22.670 align:middle line:84%
which many of you may
have already seen--

00:16:22.670 --> 00:16:24.820 align:middle line:90%
I apologize if you have--

00:16:24.820 --> 00:16:28.960 align:middle line:84%
explaining the technology of
networking geothermal heat

00:16:28.960 --> 00:16:31.003 align:middle line:90%
pumps in a very basic level.

00:16:31.003 --> 00:16:33.170 align:middle line:84%
Tomorrow, you're going to
get a very advanced level.

00:16:33.170 --> 00:16:33.963 align:middle line:90%
For now, this is--

00:16:33.963 --> 00:16:34.630 align:middle line:90%
[VIDEO PLAYBACK]

00:16:34.630 --> 00:16:36.005 align:middle line:84%
NARRATOR: Right
beneath our feet,

00:16:36.005 --> 00:16:37.840 align:middle line:84%
the Earth is soaking
up energy from the sun,

00:16:37.840 --> 00:16:40.200 align:middle line:84%
and it's been doing
this for a long time.

00:16:40.200 --> 00:16:42.710 align:middle line:84%
Near the surface, the
ground warms and cools

00:16:42.710 --> 00:16:45.020 align:middle line:84%
with the seasons,
but lower down, it

00:16:45.020 --> 00:16:46.860 align:middle line:90%
stays at a constant temperature.

00:16:46.860 --> 00:16:51.190 align:middle line:84%
In Massachusetts, that's 55
degrees Fahrenheit year round.

00:16:51.190 --> 00:16:54.450 align:middle line:84%
This stored temperature is a
source of renewable energy.

00:16:54.450 --> 00:16:57.410 align:middle line:84%
It can be accessed to heat
or cool a single building

00:16:57.410 --> 00:16:59.280 align:middle line:90%
without using fossil fuels.

00:16:59.280 --> 00:17:02.570 align:middle line:84%
But did you know we can also
connect entire communities

00:17:02.570 --> 00:17:05.060 align:middle line:84%
to that renewable
source in the ground?

00:17:05.060 --> 00:17:06.680 align:middle line:90%
How does it work?

00:17:06.680 --> 00:17:10.460 align:middle line:84%
It starts with underground pipes
in the streets, sort of like gas

00:17:10.460 --> 00:17:12.810 align:middle line:84%
pipes, but filled
only with water.

00:17:12.810 --> 00:17:15.560 align:middle line:84%
The water absorbs the ground
temperature of the Earth

00:17:15.560 --> 00:17:17.799 align:middle line:90%
and delivers it to buildings.

00:17:17.799 --> 00:17:20.339 align:middle line:84%
Pipes connect buildings with
different heating needs,

00:17:20.339 --> 00:17:22.290 align:middle line:90%
so energy is never wasted.

00:17:22.290 --> 00:17:24.530 align:middle line:84%
Instead, it's exchanged
between buildings

00:17:24.530 --> 00:17:26.670 align:middle line:84%
or stored in the ground
until it's needed.

00:17:26.670 --> 00:17:30.350 align:middle line:84%
Inside, a heat pump moves
heat in or out, according

00:17:30.350 --> 00:17:32.480 align:middle line:90%
to the temperature you want.

00:17:32.480 --> 00:17:35.850 align:middle line:84%
This system of pipes can
connect like LEGO blocks,

00:17:35.850 --> 00:17:39.180 align:middle line:84%
gradually moving us
all from gas to geo,

00:17:39.180 --> 00:17:42.430 align:middle line:84%
giving us cleaner air,
efficient heating and cooling,

00:17:42.430 --> 00:17:43.700 align:middle line:90%
and a healthier planet.

00:17:43.700 --> 00:17:46.550 align:middle line:84%
The idea for this
networked geothermal system

00:17:46.550 --> 00:17:49.910 align:middle line:84%
run at a utility scale
originated at HEET,

00:17:49.910 --> 00:17:51.726 align:middle line:90%
a climate solutions nonprofit.

00:17:51.726 --> 00:17:52.888 align:middle line:90%
[END PLAYBACK]

00:17:52.888 --> 00:17:53.930 align:middle line:90%
ZEYNEB MAGAVI: All right.

00:17:53.930 --> 00:17:55.888 align:middle line:84%
I'm going to really
quickly go through language

00:17:55.888 --> 00:17:58.420 align:middle line:84%
and then get out of here so we
can start this amazing panel.

00:17:58.420 --> 00:18:00.670 align:middle line:84%
The word geothermal,
if any of you

00:18:00.670 --> 00:18:04.740 align:middle line:84%
are thinking about
Iceland and hot lava,

00:18:04.740 --> 00:18:07.495 align:middle line:90%
that's the stuff on the left.

00:18:07.495 --> 00:18:12.370 align:middle line:84%
This is one way to try to
clarify that geothermal

00:18:12.370 --> 00:18:15.160 align:middle line:84%
is like the last name of
a family of technologies

00:18:15.160 --> 00:18:21.010 align:middle line:84%
and energies both, and that the
one we are talking about today

00:18:21.010 --> 00:18:22.460 align:middle line:90%
is on the right.

00:18:22.460 --> 00:18:26.170 align:middle line:84%
It is-- networked
geothermal heat pumps can

00:18:26.170 --> 00:18:28.780 align:middle line:84%
provide heating
and cooling is what

00:18:28.780 --> 00:18:30.500 align:middle line:90%
is typically called shallow.

00:18:30.500 --> 00:18:34.810 align:middle line:84%
You'll hear people
use the word shallow.

00:18:34.810 --> 00:18:40.870 align:middle line:84%
But for the usual person, 1,000
or 1,200 doesn't sound shallow,

00:18:40.870 --> 00:18:42.930 align:middle line:90%
but I promise, that's shallow.

00:18:42.930 --> 00:18:46.330 align:middle line:84%
And then it is
ambient temperature.

00:18:46.330 --> 00:18:48.720 align:middle line:84%
In other words, kind of
the average temperature

00:18:48.720 --> 00:18:50.320 align:middle line:90%
of the air and the ground.

00:18:50.320 --> 00:18:53.460 align:middle line:90%
Not super hot in any way.

00:18:53.460 --> 00:18:55.590 align:middle line:84%
And one of the
things that's really

00:18:55.590 --> 00:18:58.710 align:middle line:84%
critical about this type
of geothermal energy

00:18:58.710 --> 00:19:00.820 align:middle line:90%
is that it is everywhere.

00:19:00.820 --> 00:19:03.360 align:middle line:90%


00:19:03.360 --> 00:19:06.400 align:middle line:84%
You'll hear people talking
about the word district.

00:19:06.400 --> 00:19:10.120 align:middle line:84%
And certainly, this is a
form of district energy.

00:19:10.120 --> 00:19:14.680 align:middle line:84%
And the traditional naming
system goes by generation.

00:19:14.680 --> 00:19:16.600 align:middle line:84%
First generation,
second generation.

00:19:16.600 --> 00:19:19.560 align:middle line:84%
And the type we are
discussing today

00:19:19.560 --> 00:19:23.130 align:middle line:90%
primarily is fifth generation.

00:19:23.130 --> 00:19:28.560 align:middle line:84%
And the next more
advanced level of this

00:19:28.560 --> 00:19:32.520 align:middle line:84%
is, OK, so why are we
calling it a network then?

00:19:32.520 --> 00:19:37.260 align:middle line:84%
And our proposal,
which is not universal,

00:19:37.260 --> 00:19:40.910 align:middle line:84%
but there is kind of an
emerging nomenclature,

00:19:40.910 --> 00:19:45.050 align:middle line:84%
is that within fifth
generation, if it

00:19:45.050 --> 00:19:48.350 align:middle line:84%
has a single pipe,
decentralized and renewable and

00:19:48.350 --> 00:19:53.465 align:middle line:84%
combustion-free, then it is
a thermal energy network.

00:19:53.465 --> 00:19:55.250 align:middle line:84%
And if that thermal
energy network

00:19:55.250 --> 00:19:58.010 align:middle line:84%
is tapping geothermal
energy, which

00:19:58.010 --> 00:20:00.140 align:middle line:84%
changes some of the
outcomes, then you

00:20:00.140 --> 00:20:03.400 align:middle line:84%
could also call it a
geothermal energy network.

00:20:03.400 --> 00:20:05.150 align:middle line:84%
That's what we're going
to use, but you'll

00:20:05.150 --> 00:20:08.460 align:middle line:84%
hear speakers use a lot
of different terminology.

00:20:08.460 --> 00:20:12.110 align:middle line:84%
I just wanted to give you
a quick lay of the land.

00:20:12.110 --> 00:20:15.710 align:middle line:84%
And our last task
before we begin

00:20:15.710 --> 00:20:18.720 align:middle line:84%
is if you could please
take out your phone,

00:20:18.720 --> 00:20:22.250 align:middle line:84%
we have this QR
code you can scan.

00:20:22.250 --> 00:20:26.640 align:middle line:84%
And it should work pretty
easily to get you on to Slido.

00:20:26.640 --> 00:20:31.100 align:middle line:84%
And now you have
your first quiz.

00:20:31.100 --> 00:20:32.550 align:middle line:90%
We did say class, right?

00:20:32.550 --> 00:20:35.900 align:middle line:90%


00:20:35.900 --> 00:20:36.400 align:middle line:90%
Don't worry.

00:20:36.400 --> 00:20:37.950 align:middle line:90%
There's actually no test.

00:20:37.950 --> 00:20:44.250 align:middle line:90%
But let's see how you do.

00:20:44.250 --> 00:20:45.710 align:middle line:90%
Yeah, I made it too easy.

00:20:45.710 --> 00:20:55.545 align:middle line:90%


00:20:55.545 --> 00:20:58.740 align:middle line:84%
So if you have any
trouble getting on,

00:20:58.740 --> 00:21:02.220 align:middle line:84%
Eric standing back
there is happy to help.

00:21:02.220 --> 00:21:05.400 align:middle line:84%
ERIC: Yeah, you can also
open your web browser

00:21:05.400 --> 00:21:09.483 align:middle line:84%
and just go to slido.com and
then type in the code key

00:21:09.483 --> 00:21:10.150 align:middle line:90%
once you get it.

00:21:10.150 --> 00:21:13.318 align:middle line:90%


00:21:13.318 --> 00:21:14.360 align:middle line:90%
ZEYNEB MAGAVI: All right.

00:21:14.360 --> 00:21:36.770 align:middle line:90%


00:21:36.770 --> 00:21:38.680 align:middle line:84%
I like watching them
go out and back.

00:21:38.680 --> 00:21:41.010 align:middle line:90%
[LAUGHS] That's how I think.

00:21:41.010 --> 00:21:44.210 align:middle line:90%


00:21:44.210 --> 00:21:45.560 align:middle line:90%
All right.

00:21:45.560 --> 00:21:47.030 align:middle line:90%
Are we good?

00:21:47.030 --> 00:21:50.660 align:middle line:84%
Everyone on Slido now
for the rest of the day?

00:21:50.660 --> 00:21:52.300 align:middle line:90%
OK.

00:21:52.300 --> 00:22:00.200 align:middle line:84%
So yes, the group
wisdom is prevailing.

00:22:00.200 --> 00:22:03.320 align:middle line:84%
The type of geothermal
energy we're discussing today

00:22:03.320 --> 00:22:08.390 align:middle line:84%
is ambient, shallow,
and everywhere,

00:22:08.390 --> 00:22:12.470 align:middle line:90%
which is a lovely feature.

00:22:12.470 --> 00:22:13.170 align:middle line:90%
All right.

00:22:13.170 --> 00:22:17.600 align:middle line:84%
So we're going to take
a second and begin

00:22:17.600 --> 00:22:21.100 align:middle line:90%
our first conversation.

00:22:21.100 --> 00:22:32.000 align:middle line:90%