OCEAN ACIDIFICATION
how does this affect our aquatic and terrestrial species?
BRIAN PARK | SUEN 7130 RESEARCH STUDIO: RESILIENT CITY | PROFESSOR SCOTT BISHOP
lin e
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by 2050, we may no longer have any consumable shellfish, and our coral reefs will dissapear, along with 25% of all marine/aquatic species
50%
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BRIAN PARK | SUEN 7130 RESEARCH STUDIO: RESILIENT CITY | PROFESSOR SCOTT BISHOP
Mississippi river our arable lands are being depleted due to increasing acidity of our waterways and insufficient replenishment of minerals critical to sustainaing our riparian, prairie, amphibian, mollusk, and aquatic species
BRIAN PARK | SUEN 7130 RESEARCH STUDIO: RESILIENT CITY | PROFESSOR SCOTT BISHOP
precedents
Fargo
louisiana bayou
levees and barriers have been put in place starting at the south end of the river, which alters the path of water during regional and coastal flooding events.
netherlands
The fm diversion is a method of protecting fargo from regional flooding, by diverting water from the mouth along embankments and river inlets.
boston
grand rapids
Chicago
coastal flooding and rising sea levels bring about impending danger to present and future development in boston. what if there was to leverage flodding to combat ocean acidification?
regional planning combats flooding, but is there a way to transfer water sources externally from the grand river to redistribute minerals to adjacent agricultural lands?
The delta programme helps protect against regional flooding and secure freshwater. dikes and sand dunes help maintain water flows throughout the nation.
the calumet river is a highly polluted stream of water which feeds into the mouth of the missouri river. what if we could decontaminate the river in redistributing minerals to the mississippi river?
BRIAN PARK | SUEN 7130 RESEARCH STUDIO: RESILIENT CITY | PROFESSOR SCOTT BISHOP
bifurcate
divert
tier
prototypes
tiered landscapes allow for the collection of water along embankments, splitting the nutrient collection and sedimentation which occurs along major break points along rivers
tiered landscapes allow for meadowlands to grow in areas of high carbon deposition, and offer more carbon sequestration than traditional riperian corridors.
water flow along channels are managed by diverting water along natural berm structures to less fertile lands, while maintaing nutrients to already fertile lands
bermed landscapes allow for the manipulation of water retention, thereby allowing for the propogation of seagrass and restoration of amphibian habitats.
attenuate
rippled landscapes with nutrient-penetrable soils and assorted filter fabrics along river systems to increase carbon containment and regulate the flow of water while minimizing the suspension of fine-grained minerals
culture
coastal shellfish communities and aquaculture is critical to marine biology, and by creating areas for these communities to prosper can aid in the disintegrating population of shellfish.
BRIAN PARK | SUEN 7130 RESEARCH STUDIO: RESILIENT CITY | PROFESSOR SCOTT BISHOP
boston 2016
prime forest lands and coastal waters are exisitng characteristics of boston’s riverfront landscapes
s
e 1/8 Mil
BRIAN PARK | SUEN 7130 RESEARCH STUDIO: RESILIENT CITY | PROFESSOR SCOTT BISHOP
grand rapids 2016
prime agricultural lands and an high-energy river are a distinguishable characteristic of grand rapids’ riverfront landscape
es
1/8 Mil
BRIAN PARK | SUEN 7130 RESEARCH STUDIO: RESILIENT CITY | PROFESSOR SCOTT BISHOP
chicago 2016
prime agricultural lands and a polluted calumet river are characteristics of chicago’s riverfront landscape
s
e 1/8 Mil
BRIAN PARK | SUEN 7130 RESEARCH STUDIO: RESILIENT CITY | PROFESSOR SCOTT BISHOP
boston 2100
pocket landscapes through river diversions and oyster reefs are an integral component to the controlled movement of water along the charles, the atlantic coastline and newly established tributaries
s
e 1/8 Mil
BRIAN PARK | SUEN 7130 RESEARCH STUDIO: RESILIENT CITY | PROFESSOR SCOTT BISHOP
grand rapids 2100
tiered landscapes and diversion channels are an integral component to the controlled movement and energy of the grand river and its newly established tributaries
s
e 1/8 Mil
BRIAN PARK | SUEN 7130 RESEARCH STUDIO: RESILIENT CITY | PROFESSOR SCOTT BISHOP
chicago 2100
bifurcated and attenuated landscapes help reduce the pollution levels of the calumet, while also channeling the water to adjacent productive landscapes
s
e 1/8 Mil
BRIAN PARK | SUEN 7130 RESEARCH STUDIO: RESILIENT CITY | PROFESSOR SCOTT BISHOP
IAL
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boston
76,000 acreas of land reserved for new freshwater basins
creating freshwater basins using channel diversion strategies and pocket wetlands can assist in the distribution of water from the charles. oyster reef coastal implementation also allows for the success of coastal ecologies
BRIAN PARK | SUEN 7130 RESEARCH STUDIO: RESILIENT CITY | PROFESSOR SCOTT BISHOP
e
e
syen
ite
o
IAL
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ANIC
ASH MA SS WA STIN COLL GM UVIU ATE MU M RIA DFL L OW
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black shale
pyroxenite
oil shale
kimberlite
argillite
siltstone
dunite
fine-grained mixed clastic rock
peridotite
sandstone
ultramfic intrusive rock
arenite
nepheline syenite
orthoquartzite
alkalic intrusiv
e rock
calcarenite
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grand rapids
100,000 acreas of land reserved for new freshwater basins
due to the immense energy of the grand river, diversion channels and tiered landscapes along new tributaries allow for the distribution of regional and local stormwater to be contained in a larger framework both within and outside the city limits
BRIAN PARK | SUEN 7130 RESEARCH STUDIO: RESILIENT CITY | PROFESSOR SCOTT BISHOP
e
e
syen
ite
o
IAL
ANIC ASH MA SS WA STIN COLL GM UVIU ATE MU M RIA DFL L OW AR
S
La
sp
nd
sl
DE
ide
BR
IS F
LAH
gr
ilit
e
LO W
VOLC
E
AN M
SAND
SHEE T
DUNE
SAND
LOES
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TERR AC
EOLI
DELTA
ALLUVI AL FAN ALLUV IAL TER RACE LAKE OR MA RINE SE DIMEN PLAYA T
FLOOD PLAIN
GRAVEL
LEVEE
UNCONSOLIDATED MATERIAL
SILT
SAND
water
ALLUVIUM
ice
phyllonite
tectonite
ite
granulite
lite amphibo
migmat
s e gneis
s gneis mafic gneiss ortho eiss paragn
eiss eiss itic gn
biotit
ic gn
gran
fels
ss gnei
ist t sch his esc blu ist ash ist ist mic sch sch tic par peli elds hist tz-f e sc quar icat -sil lc hist ca e sc ibol amph s ofel gran
e llit
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ns
to
y ph
ne
ATER
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alt
me
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RIF
LD
CIA
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ma
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me
k
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an
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me
me dia te
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int
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str
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lo
cia gla
calc -si lic ate ro ck serp en tiinite meta sedi ment ary met rock a-ar gill ite e
slat
peat l
cora
iuum
resid
clay
d
or mu
rock
entary
skarn
sedim
c rock
clasti
greisen
dstone
te
eclogi
mu
claystone
ls
hornfe
rock
metamorph ic
bentonite
shale
intrusive
carbonatite e
hornblendit
black shale
pyroxenite
oil shale
kimberlite
argillite
siltstone
dunite
fine-grained mixed clastic rock
peridotite
sandstone
ultramfic intrusive rock
arenite
nepheline syenite
orthoquartzite
alkalic intrusiv
e rock
calcarenite
anorthosite
arkose
troctolite
wacke
norite
graywa cke
gabbro
medium-g
rained
quartz
conglo
mixed
gabbro
monzoga
merat
entary
-graine
quartz gabb
bbro
monz
ogabbr
roid
olist
ome
monz
nge
onite
quar
onat
tz mo
syen
tz sy
ton me
ert
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rbon
ate/
clas
lcan
ic/c
e
ic ro
ate
rock
ck
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por
tic
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ock
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ro
n
ock
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an
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pum
turf
rock
eccia
br anic
turf
rite
volc
flow
ignimb
ded
trachyte
flow lava ite al su bimod ck nic ro volca felsic olite par rhy -felds alkali
rhyodacite
e rhyolit
trachyte
alkali-feldspar
dacite
intermediate volcanic rock
latite
quartz latite
trachyandesite
andesite
mafic volcanic rock
trachybasalt
basalt
tholeiite
hawaiit e
alkali ne bas alt alkali c volca nic ro ck olite
phon
teph rite ultr amaf itite anic carb onat ite rock
onic
volc
ash-
wel
te
plut
hyry
apli
hyre
mineral composition of illinois
roph
vit
e
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lit
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ex
dia
ite
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ne
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lum
an
gr
sg
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ior
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min
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per
iro
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ck
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tic ro
ck
ston
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mix pho chem
d clas
e ro
tone
dolo
c rock
breccia
d mixe
ostr
mela
carb limes
clasti
e
sedim coar se
chicago
48,000 acreas of land reserved for new freshwater basins
bifurcated landscapes allow for the channelization of water from the calumet river to be intercepted by a large freshwater basin south of the city, mitigating polluted waters and allowing for the flow of water to be redirected before entering the mississippi river
BRIAN PARK | SUEN 7130 RESEARCH STUDIO: RESILIENT CITY | PROFESSOR SCOTT BISHOP
e
e
syen
ite
o
carbon channel
tiered riparian buffer
bifurcated landscape culture reefs
pocket wetlands BRIAN PARK | SUEN 7130 RESEARCH STUDIO: RESILIENT CITY | PROFESSOR SCOTT BISHOP