Brian Park | Urban Landscape Portfolio

Page 1

bp RIAN

ARK

Urban Landscape Portfolio


1

OCEAN ACIDIFICATION

2

ALLSTON AMALGAMATION

3

POSTINDUSTRIAL GRADIENTS

4

BRICK + CHESTNUT

5

ECOLOGICAL CITY

6

SELECTED WORKS


Table of Contents

Process + Master Plan + Phasing + Architecture

1

Process + Master Plan + Phasing + Architecture

2

Process + Master Plan + Phasing + Architecture

3

Process + Master Plan + Phasing + Architecture

4

Process + Master Plan + Phasing + Architecture

5

Process + Master Plan + Phasing + Architecture

6


1

3

OCEAN ACIDIFICATION


Climate change, is an inevitable force which is shifting our ideology on how to design with water, with synonymous understanding about how the pH of soils have an affect on adjacent landscapes as well urban regions. The world’s oceans have fallen by 0.1 pH units, which is approximately a 30% increase in acidity. This is extremely detrimental to our oceanic biology, not to mention our terrestrial biology. This increase in acidity is directly associated with the discharge of Carbon into our oceans. Carbon, a fulcrum of all organic matter, is acidic in nature, and it is being repeatedly released into our oceans. Increasing acidity chews away at our coral reefs, kills oysters and other mollusks, and increases the mortality of fish and ocean mammals.

4


20,000 yrs

Glacier Formation

5

14,000 yrs

Retreating Ice Sheets Carve Basins Into The Land, Depositing Minerals

4,000 yrs

Land Formation And Basins Become Filled With Meltwater


Existing River

Natural Hydrology

Levee Restrictions

Mineral Propogation

6


iment

n Ma terial

nd

Eolia

eet

Dune Sa

Land sl

ide

Debr is

Flow

Laha r

Sand Sh

Loes s Volca nic As h Mas sW astin Collu gM ater vium ial Mud flow

Mud Fla ts

Sand

e

Beach

Terrac

Alluvial Fan

Alluvial Terrace Lake Or Marine Sed

Playa

Flood Plain

Gravel

Levee

Delta

Unconsolidated Material

Sand

Water

Alluvium

Silt

Ice

Phyllonite

Tectonite

Granulite

iss

Amphibolite

iss

Migmatite

iss

s Paragneis

Orthogne

c Gneiss

Mafic Gne

Gne Biotite

s Gneis

Graniti

Felsic

s Gneis

t r Schis dspa hist te Sc silica t CalcSchis ibole ph Am fels Grano tz-fel

Quar

hist ic Sc

Pelit

st schi Blue shist Mica st Schi

ne nsto Gree lite Phyl

lite Spi

Rock

nic

alt

edia te M

Mafi c

Met abas

s

Talu

ift

ial Dr

Glac

Met avol ca

Inte rm

Till

ent dim ial Se Glac ent dim tified h Se Stra t twas dimen ial Ou al Se Glac galci ent prasu Sedim Sub/ trine t lacus cio dimen Gla ne Se l-mari cia Gla terial nic Ma ge Bio

aine Mor

nic

etav olca

Rock

Met avolc anic Met Rock arhy olite Kera toph yre

Mar ble

merat e

onglo

Metac

zite

Quart

Slate

Peat

argillit e

Meta-

ntary

edime

Coral

Metas

Rock

Calc-s ilicate Rock Serpen tiinite

um

Residiu

d

Mu Clay Or

k

ntary Roc

Sedime

Skarn

Clastic

Rock

Greisen

e

Mudston

Eclogite

Claystone

Hornfels

Bentonite

Metamorphic

Rock

Intrusive Carbon atite

Shale

Hornblendite

Black Shale

Pyroxenite

Oil Shale

Kimberlite

Argillite Siltstone

Dunite

Fine-grained Mixed Clastic Rock

Peridotite

Sandstone

Ultramfic Intrusive Rock

Arenite

Nepheline Syenite

Orthoquartzite

Alkalic Intrusive Rock

Calcarenite

Anorthosite

Arkose

Troctolite

Wacke

Norite

Graywacke

Gabbro

Medium-

Quartz Gabb

grained Mixe

ro

Monzoga

erate

bbro

Quartz

Monzoga

Gabbro

bbro

id

Olistos

Monzo

nite

Melan

Mixed Cla

stic Roc

k

Quart

ge

z Monzo

Carbo nate Rock Limest one

nite

e Syenit Quart

z Syen

ite

-fe Alkali

tone

Mixe

ldspa

Trond

d Ca

Mixe

hjemi

Tona

d Vo

Phos

phor

lkalin

Suba

lum

alum Met

Perlu

ous

Iron

lite

Exha

ite Gran

anite e Gr

inou

inou

min

ite

iorite

Pera

Evap orat e

Cher

ite Gran

te

r Syen

lite

od Gran

Chem

t

Nova cu

lite

Form

atio

n

ical

rbona te/cla sti

c Ro

lcanic

/clas

tic Ro

ite

ck

Sedi

men tary

ck

BOSTON Coastal flooding and rising sea levels bring about

Rock

impending danger to present and future development

anite s Gr

anite s Gr

ite

Coal

Dior anic

ck

ic Ro

Rock

last al/c

Volc

ed Co Mix

ian

in Boston. what if there was to leverage flooding to

ck

Tuff

ck

Ro lastic Pyroc

phyre Vitro ce Pumi

ic Ro lcan

Obsid

ccia ic Bre

Volcan

f d Tur f w Tur Ash-flo rite Ignimb

Welde

lite

dspar Rhyo

anic Rock

l Suite

Rhyolite

Alkali-fel

Felsic Volc

Bimoda

Trachyte

Alkali-feldspar Trachyte

Dacite

Rhyodacite

Intermediate Volcanic Rock

Latite

Quartz Latite

Trachyandesite

Andesite

Mafic Volcanic Rock

Trachybasalt

Basalt

anic Rock

Basalt

Tholeiite

Hawaiite

te

Alkaline

Alkalic Volc

Phonoli

bonatit e

afitite

Lava Flow

ck

Tephrit e

ic Car

Ultram

ic Ro

Volcan

Pluton

Aplite

rophy re

Porph yry

Lamp

Pegm atite Gran itoid Alka li-fe ldsp ar Gr anite Mon zodi orite

sy Vo

Glas

orite

Quar tz

zodi

orite

Mon

tz Di

Quar

7

cia

trome

Dolos

e

0 pH

Rock

ntary Brec

-grained

Diab as

0.25 Miles 14 pH

d Clastic

Conglom

Sedime Coarse

combat ocean acidification?


76,000 acreas of land reserved for new freshwater basins

8


iment

Flow

Debr is

Spi

Land sl

lite

ide

Laha r

ne nsto Gree lite Phyl

st Schi

Mud flow

Collu viu

Volca nic As h Mas sW astin gM ater m ial

n Ma terial

nd

Eolia

eet

Dune Sa

Sand Sh

Loes s

Mud Fla ts

Sand

e

Beach

Terrac

Alluvial Fan

Alluvial Terrace Lake Or Marine Sed

Playa

Flood Plain

Gravel

Levee

Delta

Unconsolidated Material

Sand

Water

Alluvium

Silt

Ice

Phyllonite

Tectonite

Granulite

iss

Amphibolite

iss

Migmatite

iss

s Paragneis

Orthogne

c Gneiss

Mafic Gne

Gne Biotite

s Gneis

Felsic

t r Schis dspa hist te Sc silica t CalcSchis ibole ph Am fels Grano s Gneis tz-fel

Quar

hist ic Sc

Pelit

st schi Blue shist Mica

Graniti

0.5 miles Rock

nic

alt

edia te M

Mafi c

Met abas

s

Talu

ift

ial Dr

Glac

Met avol ca

Inte rm

Till

ent dim ial Se Glac ent dim tified h Se Stra t twas dimen ial Ou al Se Glac galci ent prasu Sedim Sub/ trine t lacus cio dimen Gla ne Se l-mari cia Gla terial nic Ma ge Bio

aine Mor

nic

etav olca

Rock

Met avolc anic Met Rock arhy olite Kera toph yre

Mar ble

merat e

onglo

Metac

zite

Quart

Slate

Peat

argillit e

Meta-

ntary

edime

Coral

Metas

Rock

Calc-s ilicate Rock Serpen tiinite

um

Residiu

d

Mu Clay Or

k

ntary Roc

Sedime

Skarn

Clastic

Rock

Greisen

e

Mudston

Eclogite

Claystone

Hornfels

Bentonite

Metamorphic

Rock

Intrusive Carbon atite

Shale

Hornblendite

Black Shale

Pyroxenite

Oil Shale

Kimberlite

Argillite Siltstone

Dunite

Fine-grained Mixed Clastic Rock

Peridotite

Sandstone

Ultramfic Intrusive Rock

Arenite

Nepheline Syenite

Orthoquartzite

Alkalic Intrusive Rock

Calcarenite

Anorthosite

Arkose

Troctolite

Wacke

Norite

Graywacke

Gabbro

Medium-

Quartz Gabb

grained Mixe

ro

Monzoga

erate

bbro

Quartz

Monzoga

Gabbro

bbro

id

Olistos

Monzo

nite

Melan

Quart

z Monzo

nite

e Syenit Quart

z Syen

ite

-fe Alkali

tone

Mixe

ldspa

Trond

d Ca

Mixe

hjemi

Tona

d Vo

Phos

phor

lkalin

Suba

lum

alum Met

Perlu

ous

Iron

lite

Exha

ite Gran

anite e Gr

inou

inou

min

ite

iorite

Pera

Evap orat e

Cher

ite Gran

te

r Syen

lite

od Gran

Chem

stic Roc

k

t

Nova cu

lite

Form

atio

n

ical

rbona te/cla sti

c Ro

lcanic

/clas

tic Ro

ite

ck

Sedi

men tary

ck

GRAND RAPIDS Regional planning combats flooding, but is there a

Rock

way to transfer water sources externally from the

Coal

ian

Tuff

lastic Pyroc

ce

Pumi

phyre

Vitro

ck ic Ro last al/c ed Co Mix Rock ck anic ic Ro Volc lcan

sy Vo

Glas

Obsid

Rock

ccia ic Bre Volcan

f d Tur f w Tur Ash-flo rite Ignimb

Welde

l Suite Bimoda anic Rock Felsic Volc lite dspar Rhyo Alkali-fel

Alkali-feldspar Trachyte

Dacite

Rhyodacite

Rhyolite

Intermediate Volcanic Rock

Latite

Quartz Latite

Trachyte

Trachyandesite

Andesite

Mafic Volcanic Rock

Trachybasalt

Basalt

anite s Gr

anite s Gr

anic Rock

Basalt

Tholeiite

Hawaiite

te

Alkaline

Alkalic Volc

Phonoli

bonatit e

Lava Flow

ck

ic Car

Tephrit e Ultram afitite

ic Ro

Volcan

Pluton

Aplite

Porph yry Lamp rophy re

Pe gm atite Gran itoid Alka li-fe ldsp ar Gr anite onzo dior ite

tz M

orite

Quar

zodi

orite

Mon

tz Di

Quar

9

Mixed Cla

ge

Carbo nate Rock Limest one

ite

0 pH

cia

trome

Dolos

Dior

0.5 Miles 14 pH

Rock

ntary Brec

-grained

Diab ase

0.5 miles

d Clastic

Conglom

Sedime Coarse

grand river to redistribute minerals to adjacent agricultural lands?


100,000 acreas of land reserved for new freshwater basins

10


Unconsolidated Material

iment

n Ma terial

nd

Eolia

eet

Dune Sa

Spi

ide

Land sl

lite

Debr is

Flow

Laha r

Sand Sh

Loes s Volca nic As h Mas sW astin Collu gM ater vium ial Mud flow

Mud Fla ts

Sand

e

Beach

Terrac

Alluvial Fan

Alluvial Terrace Lake Or Marine Sed

Playa

Flood Plain

Gravel

Levee

Delta

Sand

Water

Alluvium

Silt

Ice

Phyllonite

Tectonite

Granulite

iss

Amphibolite

iss

Migmatite

iss

s Paragneis

Orthogne

c Gneiss

Mafic Gne

Gne Biotite

Graniti

Felsic

s Gneis

tz-fel

Quar

Pelit

ne nsto Gree lite Phyl

st Schi

st schi Blue shist Mica

hist ic Sc

t r Schis dspa hist te Sc silica t CalcSchis ibole ph Am fels Grano

s Gneis

RATIO OF ACIDITY TO ALKALINITY IN SOIL PH OVER BEDROCK DEPTH Rock

nic

alt

edia te M

Mafi c

Met abas

s

Talu

ift

ial Dr

Glac

Met avol ca

Inte rm

Till

ent dim ial Se Glac ent dim tified h Se Stra t twas dimen ial Ou al Se Glac galci ent prasu Sedim Sub/ trine t lacus cio dimen Gla ne Se l-mari cia Gla terial nic Ma ge Bio

aine Mor

nic

etav olca

Rock

Met avolc anic Met Rock arhy olite Kera toph yre

Mar ble

merat e

onglo

Metac

zite

Quart

Slate

Peat

argillit e

Meta-

ntary

edime

Coral

Metas

Rock

Calc-s ilicate Rock Serpen tiinite

um

Residiu

d

Mu Clay Or

k

ntary Roc

Sedime

Skarn

Clastic

Rock

Greisen

e

Mudston

Eclogite

Claystone

Hornfels

Bentonite

Metamorphic

Rock

Intrusive Carbon atite

Shale

Hornblendite

Black Shale

Pyroxenite

Oil Shale

Kimberlite

Argillite Siltstone

Dunite

Fine-grained Mixed Clastic Rock

Peridotite

Sandstone

Ultramfic Intrusive Rock

Arenite

Nepheline Syenite

Orthoquartzite

Alkalic Intrusive Rock

Calcarenite

Anorthosite

Arkose

Troctolite

Wacke

Norite

Graywacke

Gabbro

Medium-

Quartz Gabb

grained Mixe

ro

Monzoga

erate

bbro

Quartz

Olistos

Monzoga

Monzo

nite

Melan

Quart

z Monzo

nite

e Syenit Quart

z Syen

ite

-fe Alkali

tone

Mixe

ldspa

Trond

d Ca

Mixe

hjemi

Tona

d Vo

Phos

phor

lite

od Gran

Chem

bbro

lum

alum Met

Perlu

ite

lkalin

Suba ite Gran

te

r Syen

iorite

Pera

Evap orat e

Cher

Iron

stic Roc

k

t

Nova cu

lite

Form

atio

n

ical

rbona te/cla sti

c Ro

lcanic

/clas

tic Ro

ite

ck

Sedi

men tary

ck

CHICAGO The Calumet River is a highly polluted stream of

Rock

water which feeds into the mouth of the missouri

anite e Gr

anite s Gr anite s Gr inou

inou

min

ous

ite Gran

ite

Coal

Dior

lite

Exha

Diab ase anic

ic Ro

Rock

last al/c

Volc

ed Co Mix ck

river. what if we could decontaminate the river in

ck

ic Ro lcan

sy Vo

Tuff

ck

Ro lastic Pyroc

ce

Pumi

phyre

Vitro

ian Obsid

ccia ic Bre

Volcan

f d Tur f w Tur Ash-flo rite Ignimb

Welde

Rhyolite

Trachyte

Alkali-feldspar Trachyte

Dacite

Rhyodacite

Intermediate Volcanic Rock

Latite

Quartz Latite

Trachyandesite

Andesite

Mafic Volcanic Rock

Trachybasalt

Basalt

anic Rock

Basalt

Tholeiite

Hawaiite

te

Alkaline

Alkalic Volc

Phonoli

bonatit e

afitite

Lava Flow l Suite Bimoda anic Rock Felsic Volc lite dspar Rhyo Alkali-fel

ck

Tephrit e

ic Car

Ultram

ic Ro

Volcan

Pluton

Aplite

Porph yry Lamp rophy re

Pegm atite Gran itoid Alka li-fe ldsp ar Gr anite onzo dior ite

tz M

Glas

Quar

zodi orite

orite

Mon

tz Di

Quar

11

Mixed Cla

ge

Carbo nate Rock Limest one

RATIO OF ACIDITY TO ALKALINITY IN SOIL PH OVER BEDROCK DEPTH 0 pH

trome

Dolos

1 Mile 14 pH

cia

-grained

id

0.5 miles

Rock

ntary Brec

Gabbro

0.5 miles

d Clastic

Conglom

Sedime Coarse

redistributing minerals to the Mississippi River?


48,000 acreas of land reserved for new freshwater basins

12


INLAND RIVER STRATEGIES

BIFURCATE

DIVERT

ATTENUATE

Tiered landscapes allow for the collection of water along embankments, splitting the

Water flow along channels are managed by diverting water along natural berm structures

Rippled landscapes with nutrient-penetrable soils and filter fabrics along river

nutrient collection and sedimentation which occurs along major break points along rivers

to less fertile lands, while maintaing nutrients to already fertile lands

systems to increase carbon containment and regulate the flow of water while minimizing the suspension of fine-grained minerals

13


COASTAL STRATEGIES

TIER

POCKET

CULTURE

Tiered landscapes allow for meadowlands to grow in areas of high carbon deposition,

Bermed landscapes allow for the manipulation of water retention, thereby

Coastal shellfish communities and aquaculture are critical to marine biology, and by

and offer more carbon sequestration than traditional riperian corridors.

allowing for the propogation of seagrasses and restoration of amphibian habitats.

creating areas for these communities to prosper, can aid in the disintegrating population of shellfish.

14


BOSTON 2016 Prime forest lands and coastal waters are exisitng characteristics of Boston’s riverfront landscapes

1/8 MI

15


BOSTON 2100 Pocket landscapes through river diversions and oyster reefs are an integral component to the controlled movement of water along the Charles River, the Atlantic coastline and newly established tributaries

1/8 MI

16


GRAND RAPIDS 2016 Prime agricultural lands and an high-energy river are a distinguishable characteristic of Grand Rapids’ riverfront landscape

1/8 MI

17


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

1/8 MI

18


CHICAGO 2016 Prime agricultural lands and a polluted Calumet River are characteristics of Chicago’s riverfront landscape

1/8 MI

19


CHICAGO 2100 Bifurcated and attenuated landscapes help reduce the pollution levels of the Calumet River, while also channeling the water to adjacent productive landscapes

1/8 MI

20


Tiered Riparian Buffer Bifurcated Landscape

Culture Reefs

Pocket Wetlands

21


22


2

ALLSTON AMALGAMATION


Lower Allston

MBTA Lines Legacy Rails Existing Infrastructure

, with a boundary between the Charles River and the Mass Pike. Essentially, my project deals with the physical disconnection of the entire neighborhood of Lower Allston to the rest of Boston. Additionally, Harvard University purchased much of the land in Lower Allston, leading consistently to new development. New development and continued purchase of land by Harvard has angered the bulk of the lower-income, partly foreign ethnic neighborhood, and as a result there has been a social schism of sorts between the residential and institutional communities. Finally, several areas of Lower Allston feature industrial or unused spaces which leads to vacant lands within the neighborhood. These vacant lots and construction areas also evoke a sense of disconnection within the community, which is evident by the misuse, or ‘under-population’ of these certain areas.

24


ALLS TON CO

ION ECT NN

CULTURAL NODE

25

WATERFRON T

MBTA Lines Amalgamation Zones Harvard Development

MBTA Lines Park Paths New Streetscapes


Sound/Sight Berms Public Open Space Harvard Connector

West Station New Development

26


27


28


29


30


31


32






3

POSTINDUSTRIAL GRADIENTS


WAY P O I N T A RT IFAC T MATE RI AL

Post-industrial gradients focuses on creating complexity within industrial reclamation. Through the implementation of both temporary and permanent programs the site will transform to a performative and collaboratively working landscape.

Albert Einstein once said that "Time and space are modes in which we think and not conditions in which we live�. Eternity is not a continuous line of time but one that extends forever. This identification of time as figurative, yet spatially literal, entities are ever present in our site. Industrial occupation has been a defining agenda which has shaped the character and identity of the site within the last 120 years. Baseline shifts in political and economic factions led to the disintegration of industrial infrastructure throughout the site’s history, leaving behind traces of programmatic legacy.

34


SHIPPING

SHIPPING DEVELOPMENT

REMEDIATION

REMEDIATION WATER COLLECTION

HABITATS

HABITATS

STORAGE

STORAGE

VEGETATION

VEGETATION

2144

2124

2 1 04

2 08 4

2 064

2 04 4

INDUSTRIAL

DEVELOPMENT

WATER COLLECTION

35

2 02 2

2 02 0

1 990

1 97 3

1 964

1 94 2

1 93 1

1 907

1 8 92

INDUSTRIAL


PAST

FUTURE

36


I NDUS TRI A L L AND ( $$$$$)

37

ON LY AVA I L A B L E US E S (+++++)

I ND U S T R I A L L A ND ($$$$$ )

N EW PA RA DIGMS (+ + + + + )


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RD

RD

PA DDL E BOAR DI NG

SOF

RD

D

D

TER

WA

SP

DE

E

R

US

PUBL IC ART

HA

HAR

LAN

WA

D

TER

SE

NS

TE

CL

HA

ST O RM WATER M ANAGE M E NT

T

T

T

T

+ LAN

WA

SP

AR

DE

US

E

T

HA

BOAT I NG

SOF

SOF

SOF

SOF

TER

D

TER

AR

CL

NS

COMMUNITY G ARDEN

RD

RD

WA

+ LAN

WA

SP

SE

NS

DE

T RE ES

HA

HA

D

T

TER

D

DE

E

R

SOF

T

KAYAKING

T

T

LAN

SOF

WA

+ LAN

SE

TE

SE

SOF

T

T

T

T

T

T

T

SOF

SOF

SOF

SOF

SOF

SOF

SOF

D

D

RD

RD

RD

RD

RD

RD

HA

HA

HA

HA

HA

HA

HAR

HAR

T

T

T

T

T

T

T

T

SOF

SOF

SOF

SOF

SOF

SOF

SOF

SOF

T

T

T

T

T

T

T

T

SOF

SOF

SOF

SOF

SOF

SOF

SOF

SOF

HA

RD

D

RD

RD

RD

RD

HAR

HA

HA

HA

HA

D

RD

HAR

HA

D

D

D

D

D

D

D

D

LAN

LAN

LAN

LAN

LAN

LAN

LAN

LAN

T

T

T

T

T

T

T

T

SOF

SOF

SOF

SOF

SOF

SOF

SOF

SOF

TER

TER

TER

TER

TER

TER

TER

TER

WA

WA

WA

WA

WA

WA

WA

WA

D

D

D

D

D

D

D

D

+ LAN

+ LAN

+ LAN

+ LAN

+ LAN

+ LAN

+ LAN

+ LAN

TER

TER

TER

TER

TER

TER

TER

TER

WA

WA

WA

WA

WA

WA

WA

WA

SP

AR

AR

SE

SE

SE

SE

SE

SE

SE

SE

AR

AR

AR

AR

AR

AR

SP

SP

SP

SP

SP

SP

SP

DE

DE

DE

NS

NS

E

E

E

E

E

E

E

E

NS

NS

NS

NS

NS

NS

DE

DE

DE

DE

DE

CL

CL

CL

US

US

TE

TE

R

R

R

R

R

R

R

R

TE

TE

TE

TE

TE

TE

US

US

US

US

US

US

CL

CL

CL

CL

CL

DE

DE

DE

NS

NS

E

E

E

E

E

E

E

E

NS

NS

NS

NS

NS

NS

DE

DE

DE

DE

DE

CL

CL

CL

US

US

TE

TE

R

R

R

R

R

R

R

R

TE

TE

TE

TE

TE

TE

US

US

US

US

US

US

CL

CL

CL

CL

CL

SP

AR

AR

SE

SE

SE

SE

SE

SE

SE

SE

AR

AR

AR

AR

AR

AR

SP

SP

SP

SP

SP

SP

SP

CL

CL

CL

US

US

TE

TE

R

R

R

R

R

R

R

R

TE

TE

TE

TE

TE

TE

US

US

US

US

US

US

CL

CL

CL

CL

CL

MI

NI

NI

MA

MA

L

L

L

MA

MA

MA

MA

MA

MA

NI

NI

NI

NI

NI

NI

MI

MI

MI

MI

MI

MI

MI

ME

ME

AL

AL

AL

AL

AL

DI

DI

AL

AL

AL

DI

DI

DI

DI

DI

DI

ME

ME

ME

ME

ME

L

L

L

L

L

ME

MA

XI

XI

MA

MA

L

L

L

MA

MA

MA

MA

MA

MA

XI

XI

XI

XI

XI

XI

MA

MA

MA

MA

MA

MA

MA

L

L

L

L

L

ME

DI

DI

MI

MI

AL

MI

AL

MI

AL

NI

NI

MA

MA

L

L

L

MA

MA

MA

MA

MA

MA

NI

NI

NI

NI

NI

NI

MI

AL

MI

AL

MI

AL

MI

AL

AL

DI

DI

DI

DI

DI

DI

ME

ME

ME

ME

ME

ME

ME

L

L

L

L

L

AC T I VITY PAT HS

SOF

SOF

T

D

T

TER

TER

AR

US

CON CERT SPACE

SOF

RD

LAN

SOF

WA

WA

SP

CL

AR

SH RUBS

RD

HA

RD

D

T

D

E

SP

SN OW/SA LT ST ORAGE

HA

T

T

HA

LAN

SOF

+ LAN

NS

T

D

F IS HI NG

T

SOF

SOF

T

RD

D

TER

TER

DE

SOF

HAR

CIRCULATION + AM E NIT I E S

H ARD P L AY SPAC ES

SOF

RD

SOF

HA

LAN

WA

WA

SE

IN TERACTIVE GAMES

HA

T

T

T

T

AR

T

TEM P ORARY DOC K

T

SOF

SOF

SOF

SOF

SP

SOF

WAT E R PROGR AM S

SP ORTS FIEL DS

SOF

RD

RD

RD

S EAT IN G

HA

HA

HA

CONTA INER STORAGE

T

T

T

REM EDIAT IVE P R O G RA MS

LOOKOU T VIEW S

SOF

SOF

SOF

SO CIAL PRO GR AM S

SECO ND T IE R

LAYCERART EDE DIS SIA TNRIBUTION M EDI A NS SOFT PLAY S PAC ES E L E VAT E D WAL KWAYS ADV ENT URE PL AYGRO UND PU BL IC RES TROOM EDU CATION AL WAY FIN DIN G

URBAN BEAC H

H A BITAT S

INTERAC TIVE ART

40


=

=

SEC OND TIER

LAY ERED DIS T RIBUTION

=

C IRC ULAT I ON + AM EN ITI ES

FIR

T ST

IER

C IR C UL AT IO N + A M EN IT I ES

=

S

WAT ER PROGRAM S

FIR

T ST

IER

=

REM EDIAT IVE P ROGRAM S

F

T IRS

TIE

R

41

F

T IRS S FIR

TIE TT

R IER

IE DT

R

WATER PRO GR A M S

S

N ECO

IE DT

R

REM E DIAT IV E PR O GR A M S

=

O SEC

SOC IAL P ROGRAM S

=

N ECO

ND

TIE

R

S O C IA L PRO G RA M S

=

S

N ECO

IE DT

R


42

L AYE RED DI S T RI BUT I O


43


44

MATER IAL

ARTI FACT

WAYPOIN T

MATER IAL

ARTI FAC T

WAYPOIN T

MATER IAL

ARTI FAC T

WAY PO INT

ARTIFACT

WAYP OINT

M ATERIAL

M ATERIAL

ARTIFACT

WAYP OINT

ART IFACT

M AT ERIAL

WAYP OINT

ART IFACT

M AT ERIAL

WAYP OINT

M AT ERIA L

A RT IFACT

WAYP O INT


45


46


4

THE ECOLOGICAL CITY


Mountai n & Polar R egion

Fo res t & Wo o dl a n d s

A g ri c u ltu ra l/d r y L a n d s

I n la n d Wate r

U r b a n R e a lm

Coas tal & Mar ine

+ 1 0 ,0 0 0

+ 100

0

- 75

Within the Ecological City,

water is the critical infrastructure by which the urban context survives by. Cities near water allow for water transportation, which is generally faster than land transportation. Cities with access to water trading routes could deliver great amounts of goods for trade with other coastal cities, which means more money and trade goods for both settlements, and allowed for cultural mixing. Landlocked cities, on the other hand, were limited to land trade routes only, which tended to be slower and in some cases more costly. Rivers, Lakes and the Ocean provide food and other resources, which help the population of coastal cities to grow and expand faster than landlocked settlements. While inland cities could only rely on agriculture, foraging and hunting, coastal cities also had access to the flora and fauna that lived on the water bodies next to them. Plus, fresh, drinkable water is necessary for people to thrive, and building a city next to a fresh water source was a huge advantage over settlements built in other places, where they had to look for water sources, or build aqueducts to bring water to them. 48


A > 10%

49

B 4 - 10%

C 2 - 4%

D < 4%

E < 2%

F < 2%

G 2 - 4%


L and Erosio n Co a s t s

Su b a e r i a l D e p o si ti o n s

Mar ine D epos ition

Drow n ed River Va l l eys

D rown e d G la c i a l Va lleys

D el ta Coas t

A l l uv ial P l ain/ Fan C oas t

B ar r ier/be ac h Plain

Mu dfl at

Ka rs t C o a s t

R o c k C o a st

Gl acial D epos it C oas t

D une

Vol canic/fau lt Coast

Beac h roc k

50


LP LA

LA

LA

LA LA

IT

LA

LA

LA

LP

LP

LP

LP

LP

LA

L on g-term Stewardsh ip

IT

IT JV LA LP

51

Social Infras tr uctures IT

JV

IT

LA

C

C

A nd D evel opment IT

JV

Settl ement P l anning

D evel opment

A n d C o n se nt

TC

CB

Infras tr uctural

Ma ste r P la n n i n g

C

S ite Asse m b l y

CC TC

CC

TC

TC

CC

TC

TC

TC TC

TC

CC

I n sti tu ti o n s Jo i nt Ve ntu re s L o c a l A u th o r ities L o c a l Pe o p le

TC CC CB C

Tow n C ouncil Community C ompany Community B uil ders Cons tr uction


Si g ni fi c a nt Influence

TC

LA

LP

LP

LP

LP

LP

LA LA

LA

LA LA

IT

LA

LP

L on g-term Stewardsh ip

IT

LA

Social Infras tr uctures IT

JV

IT

LA

C

C

A nd D evel opment IT

JV

Settl ement P l anning

D evel opment

A n d C o n se nt

TC

CB

Infras tr uctural

Ma ste r P la n n i n g

C

S ite Asse m b l y

CC TC

CC

LA

CC

TC

TC

TC

CC

TC

TC

TC

Mo d e rate Influe nce

Mo d e rate Influe nce

Si g ni fi c a nt Influence IT JV LA LP

I n sti tu ti o n s Jo i nt Ve ntu re s L o c a l A u th o r ities L o c a l Pe o p le

TC CC CB C

Tow n C ouncil Community C ompany Community B uil ders Cons tr uction

52


Water Ma n a g em ent

Water Dis t rib u t io n

Water Qu a l it y

S to rmwater Ma n a g em ent

Ha bitat s

Eco sys tem s

A ir Qu a l it y

En erg y S ys tem s

Tra n s po rtat io n

In du s t ry

Inf ra s t ru ct u re

Wa s te Ma n a g em ent

Co nt rol l ed Devel o p m ent

Lo ca l A dm in is t rat io n

S tate A d m in is t rat io n

Pa rt icip ate | Neg ot iate| Del iberate

53 P r io r ity O f Hig hway Infra s tr ucture

P r io r ity O f Po r t Infra s tr ucture

P r io r ity O f R a il Infr us tr ucture

P r io r ity O f A uto mated Indus tr ies

Q ua l ity O f Sto r mwater Infra s tr ucture

A cces s To Sto r mwater Infra s tr uctures

A cces s To R enewa bl e Energ y Sys tems

Number O f Ho s pita l s A nd O ther Hea l th C are Facil ities

Number O f P r ima r y/s eco nda r y Scho o l s

R a ng e/number O f Fa cil ities ( P ubl ic/pr ivate) Avail abl e To Co mmunity Members /o rga nizatio ns

O ppo r tunities A nd Pa r ticipatio n In Civ ic O r Co mmunity Enga g ement

Va ca ncy R ates

Co mmercia l Lea s e R ates

Ca pa city Fo r P ubl ic P l a cema king

Ho us ing D ivers ity

Ho us ing Affo ra bil ity

D evel o pment Ca pa city

P ro po r tio n O f Wa s te Which Is R ecycl a bl e

A cces s To B icycl e Infra s tr ucture

Frequency O f Tra ns it Ser v ice A nd A cces s To Trans it Ser v ices

20 Min Neig hbo r ho o d Pedes tr ia n A cces s To Ser v ices Index Sco re

Net Po s itive Energ y

A nnua l Energ y D ema nd

Per C a pita R atio O f Energ y So urce

A nnua l Energ y D ema nd Per C a pita

Mea s ured Co 2 Emis s io ns

Mea s ured C02 Seques tered B y Ca no py A nd Shur bs

A cco unta bil ity O f B ird Species

A cco unta bil ity O f Inva s ive Species

R atio O f Veg etative Cover

R atio O f Imper v io us Ser v ices

Suita bil ity O f B edro ck Geo l o g y

Fer til ity O f A g r icul tura l La nd

A ccces s To A g r icul tura l La nd

Energ y O f Water Sys tem

A cces s To Gl a cia l R uno ff

A cces s To R es er vo irs

A cces To A quifers

Water D ema nd A nd Co ns umptio n


R iver

Ba rrier

R i p a r i a n B u ffe r

Wa ll

Energ y

R ain Garden

La ke

C rown

Ste p

Por t

Green R oof

Bu l kh ea d

Rip Rap

We tla n d

Es tuar y

R ail

Ro a d / H ig h way

R e n ewa b le s

Beach

Indus tr y

Serv ices

C u l t u re

Wa ste

Pa r k

A quifer

S t reet Trees

Cso

Dune

R e se r vo i r

R eef

54


Nyc

55

Bo s to n

Chicago

H o u sto n

La

Seattl e


5 B l oc ks Pe r Bo u leva rd , 1 .5 Ave n u e s Pe r 1 Block, 4 Boulevards Per Mile ( 1 . 5 Mil e s) = 1 0 0 , 0 0 0 Pe o p le

L ike T h e Mu sc le s In O u r Bo d y, Th e Fib e rs Are React ive A nd Malleable, Much Like The Block S t r uct ure Of C iti es . I n C oh es i on , Ri vers Rea c t To Th e Forc es A rou n d I t, M u c h L ike Fib e rs As We ll.

Fi s h eye

Tw i s t

I nflate

B en d

Wave

Arc

8 1 Sq Mil e s = 51 840 Ac re s 1 3 , 0 0 0 Pe op le Pe r Sq u a re M ile = 1 0 530 0 0 People

56


In dust ry And Power

C o a s ta l Protect io n

C i vi l Se r vi c e s

Net- p o si ti ve I nfra str u c tu re

57

Tra n sp o r tation

R iver Conditions


C h i c a g o , I lli n o i s 1 2, 7 5 o Pe o p le Pe r Sq u a re M i le 2.8 M i lli o n Pe o p le 234 Sq u a re M i le s

58


36 Sq M i le s = 2304 0 A cres 4 6 8 , 0 0 0 Pe opl e

59


Coastal Protec tion

Indus tr y A nd Power

Net-pos itive Infras tr ucture

River C o n d it io n s

C i vi l Se r vi c e s

Trans por tation

60


5

SELECTED WORKS


AL STIV G FE LAN I M SU

SILANG PR V

T UI FR

TA VESTING HAR

SEE DIN G

R

ES

IN

CE

PL E

G

PI FE ST IV AL

M AN G

O

LI M

E

TAH

NE

AP

AL IV A ST IV FE ST FE N YA WA KA

L

D GA RE A

PAPAYA

RO OT V

BE

HA

EM

E GE

TIN

O

S EP T

TABLES

G RIC

E

N OV E

ER CT OB

NE

ED

ES

L VA

BL

ST I

ETA

AUGUST

FE ST IVA L

MB ER

APR IL JU LY

SA PY AW

RE ST I

R MBE CE DE

AVOCA DO

JAN UA RY

MAY JU

SE

VE G

E AN F KALAYA

PLOWIN G

CORN ING ED SE

FEBRUARY

CH AR M

RI

BE

S AN

NG

RV

K

SUGAR CAN E

D IN AR M

JA C

COFFEE

TAS FES TIV AL

G ON

NATIO NAL WEEK

Selected Works,

a compilation of my work, during my time at Sasaki Associates. Unless otherwise indicated, all materials on these pages are copyrighted by the Sasaki Associates, and used for my personal use, with permission from Sasaki Associates.

62


UMASS BOSTON, 63

SASAKI ASSOCIATES


UMASS BOSTON,

SASAKI ASSOCIATES

64


BRISTOL COMMUNITY COLLEGE, 65

SASAKI ASSOCIATES


BRISTOL COMMUNITY COLLEGE,

SASAKI ASSOCIATES

66


EMERALD NETWORKS AT GALLERY 360, 67

SASAKI ASSOCIATES


EMERALD NETWORKS AT GALLERY 360,

SASAKI ASSOCIATES

68


page intentionally left blank 69


page intentionally left blank 70


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