00
PORTFOLIO
2012-2013
LARA MEHLING
01
intervention map
[ver路nal路is : marker of heat, lightness, time, the moment when winter is eclipsed by spring] As a surface puncture, a vernal pond renders visible a unique and brief moment of exchange. It marks time through the seasonally fluctuating water table; its flow programs occupation. On a regional scale, a range of perforations in the ground patterns the surface of the site into a distributed, vernal reservoir.
VERNAL OCCUPATION cape cod
warm season swimming
high water log-drive
frozen basin “wet�storage
detail plan / diagramatic model inserts
02
pond typology
bristol models
Despite its unceasing flow an aquifer is still confined. Its contours set up zones of tolerance, both in terms of disturbance and access. It “serves� the ground and its occupants directly above. A thinner surface ties the citizen closer to a vital resource. Eight pond typologies, driven by seasonal groundwater flows, explore a variety of activities demanded by and suited to the varying dimensions of vernal pools.
VERNAL OCCUPATION cape cod
type-specific experiential perspectives
03
CNC-milled model (lightbox)
The engine of not only material and metabolic exchange, but also of human activity, is an ephemeral, porous field that lies adjacent to, if not submerged directly within, the dense, compacted fabric of the upper Cape.
zone 1 zone 2
zone 3 zone 4 “TIMBER HARVEST: A moisture gradient in seasonal flux programs the harvesting techniques within a distributed, vernal reservoir. The proximity of the ground surface to the watertable determines permitted levels of disturbance. Four management zones with varying ranges radiate outward from the vernal’s fragile center.”
VERNAL OCCUPATION cape cod
installation
04
aerial (CNC model rendering) Site activities with varying degrees of access to the public eclipse one another in short succession, optimizing the specific, critical water level that signals its operation. Wet season and dry season condition its itinerant occupants.
“CIVIL LIGHTS: From an aerial perspective, night lights indicate densities of human settlement.Vernal occupation adopts the notion of nocturnal inhabitation, terrestrial-aquarian half-lives, and on/ off switch circuit boards. A seasonal round allows for coordination.�
VERNAL OCCUPATION cape cod
foam model / occupational calendar
05
decay study sample
2m
1.5"
1m
1"
1m
1"
0m
0.5"
0m
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0"
-1m
-1m
2m
1.5"
5m
3" foam model height
4m
2.5"
3m
2"
3m
2"
2m
1.5"
2m
1.5"
1m
1"
1m
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0.5" watertable
-1m
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VERNAL OCCUPATION cape cod
0" foam model depth
0"
5m
3" foam model height
4m
2.5"
3m
2"
3m
2"
2m
1.5"
2m
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1m
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1m
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0m
0.5"
0m
0.5" watertable
-1m
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-1m
0" foam model depth
resin model
Occupational activity is zoned: if porosity and moisture availability in the ground measures the rate of decay, then groundwater controls not only the speed of occupational flows, but also its regional designation as well. Unlike a typical watershed that elicits zones of exchange on the surface, an aquifer is fiercely local.
06
research folio
spotted salamander / Ambystoma maculatum
20+ masses
blue-spotted salamander / Ambystoma laterale
10+ egg masses
wood frog / Rana sylvatica
40 + egg masses
fairy shrimp / Brachinecta lynchi
in any life stage
1.5 - 3.5 cm
Vernal Occuption employs a telescopic method in order to magnify a unique and ephemeral phenomenon. From the scale of a salamander egg attached to a floating stick in a muddy forest puddle to a satellite perspective of an urban network revealing centers of activity on the upper Cape Cod, this project explores how these fine, microscopic patterns may inform a lighter urbanism at large.
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1
BREEDING GROUNDS: Just below the reflective surface of a blackwater woodland puddle, fallen twigs and leaves become the ground for amphibian reproduction. As subsurface structure for obligate species, the debris cycles nutrients back into the ecosystem.
Field Notes for Vernal Occupation Location: Camp Edwards, Cape Cod, Massachusetts, USA 41°40’17.43”N / 70°33’53.06”W
VERNAL OCCUPATION cape cod
0.3 meter vantage
spotted salamander / Ambystoma maculatum
20+ masses
blue-spotted salamander / Ambystoma laterale
10+ egg masses
wood frog / Rana sylvatica
40 + egg masses
fairy shrimp / Brachinecta lynchi
in any life stage
1
1
1.5 - 3.5 cm
BREEDING GROUNDS: Just below the reflective surface of a blackwater woodland puddle, fallen twigs and leaves become the ground for amphibian reproduction. As subsurface structure for obligate species, the debris cycles nutrients back into the ecosystem.
0.3 meter vantage
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12 sequential elements
07
concept section
VERNAL OCCUPATION cape cod
faunal ranges
The profile of a shallow ephemeral pond reveals how minute changes in topography and moisture elicit particular vegetation types. Graminoids, forbs, shrubs, and trees emanate outward from a New England pond. Animals are drawn to vernal pools, altering their migration patterns to come upon these stepping stones in an arid landscape, particularly in years of drought when still-standing water is scarce. Animals eat seeds and move on; they become agents for propagating water, literally carrying the potential for future vernal ecosystems.
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fog phenomenon - a visibility calendar white rainbow
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2
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+ peak sea fog occurrence
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cold patch formation
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cold patch maturity
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3
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1
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full spectrum saturation
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12
1
2
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3
4
cold patch decay
5
6
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7
cold patch formation
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10
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cold patch maturity
10
-
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12
cold patch decay
cold patch maturity
cold patch maturity
ambient sound personal sound 69 24
57
22
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vertical mixing / tidal cooling
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20
14 13 7
7
5
surface air temperature (SAT) (Fahrenheit) sea surface temperature (SST)
22
26
vertical mixing / tidal cooling
66 24
22 20
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35
14 13 7
7
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0
surface air temperature (SAT) (Fahrenheit) sea surface temperature (SST)
0
0.09 0.24
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17
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ambient sound personal sound 69
66
1.13
tidal flux (m)
0.09 0.24
1.28
vortex
1.13
1.28
vortex
TERRITORIAL TURBULENCE jamaica bay, ny
tidal flux (m)
fog frequency diagram
fog frequency
SST
atmospheric stability
+ ++
+ +
SAT SST
downdraft
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+ + - -
vertical mixing atmospheric stability surface inversion
amplified bathymetry
colliding currents
- -
atmospheric stability
opposing wind and current directionality
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vertical mixing
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SST
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SAT
surface wind
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wind speed
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- -
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obstacle 2: depression
wind speed
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downdraft
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+ ++
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+ upslope fog
surface wind
downdraft amplified bathymetry (split channel)
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+ +
- -
vertical mixing
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split channel
+ +
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+ +
-
advection fog (SEA FOG)
radiation fog
SAT
obstacle 1: mound
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++ surface wind
wind speed
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+
-
downdraft
split channel
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surface inversion
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atmospheric stability
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vertical mixing
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SST
cold patch
downdraft
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-
-
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--
strait
SAT
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topographic contraction
+
+ ++ surface wind
wind speed
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downdraft
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steam fog
cloud development: vertical mixing + surface wind + thermal contrast
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- -
cold patch parameters: bathymetry + tidal flux
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atmospheric phenomenon: fog types
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infrastructure catalog elevaational program infrastructure catalog
8m 8
learning
research
production
distribution
wetland cultivation
recreation
multi-level classroom facility
multi-level laboratory
storage and maintenance center
commercial program areas
stilted residences
event spaces
ferry ports
observation decks
aquaponic docks
distribution roadways / parking
elevated dike roadway
pedestrian pathway / bicycle access
“floating� classrooms
desalination network
hydroponic greenhouses
salt storage piles
intertidal retention ponds
beach swimming areas
public underwater viewing areas
split-level observation areas
aquaculture pools p l (open ((op + enclosed)
underground salt filtering facility
intertidal pools
thermal pools (fueled by greenhouse air purge)
1 unit (3 apartments: 48 sq.m. each)
single housing unit
corner module (3 units)
building module (4 units)
superstructure
assembled courtyard
assembled unit (8 units)
vehicular traffic mainland road
dike road
pedestrian
dock / connecting boardwalk
circulation
deck / connected surface connecting bridge
capped/solid platform
double wall/courtyard
subsurface infrastructure
surface condition
double wall/capped
double wall/open
single wall/open
TERRITORIAL TURBULENCE jamaica bay, ny
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cold patch formation
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cold patch maturity
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cold patch decay
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cold patch formation
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cold patch decay
cold patch maturity
cold patch maturity ambient sound personal sound 69 26
24
57
22
vertical cooling vertical mixing / tidal t
69
66 24
20
17
35
24
57
22
14 13 7
7
5
surface air temperature (SAT) (Fahrenheit) sea surface temperature (SST)
66
26
24
vvertical ertical mixing / tidal t coolingg
22 2
22 20
17
35
14 13 7
5
0
0
tidal flux (m)
0.09 0.24
1.13
0.09 0.24
1.28
1.13
1.28
vortex vortex programming tidal zones main research campus
shellfish aquaculture
residential
shellfish aquaculture pond
intertidal pools
seawater farm
waterpark
shellfish aquaculture pond
seawater greenhouse
tidal retention pond
floating fish pen
desalination plant
natural intertidal pool
swimming basin
freshwater swimming pool
shellfish aquaculture pond
thermal bath shellfish aquaculture pond
recreational waterfront
P
halophyte fields
PP
0
-10 -1
sugar kelp crop LP -12m
PP
P -55
dike
HP +3m
high tide low tide
P 0
material exchange worrki kiing ng w waterfront ter (port)
axonometric vignettes:
recre ecre creatioonal waaterfront ont (harbor))
researcch + recreeation
ferryy route vehhicular la road secction n cutl tlin line
production + wetland wetlland ccultiva ultivation
1. fish feces fertilize greenhouse plants 2. greenhouse pool heating 3. feed production for aquaculture 4. laboratory for aquarium species 5. nitrogen extracted by seaweed 6. nutrient-rich water from shrimp farm fertilizes halophyte fields PLAN
Dead Horse Bay
scale 1:2000 05
25
50
100m
Fog is a phenomenal experience. Its occurrence relies on a delicate balance of thermal contrast, humdity, and wind. In Territorial Turbulence, surface sea and air temperatures are manipulated to affect localized advection fog within Dead Horse Bay through tidal flushing. Through an engineered system of subsurface vortices (whirlpools) and microclimatic, heat-generating superstructures, invisible processes and cycles such as tidal flux and seasonally rotating wind patterns are rendered visible, albeit ironically through fog. Fog provides private spaces within the public realm. By playing with depth of field, expansive and vast, yet unenclosed experiences are granted to the inhabitants, visitors, and employees at a new environmental research facility and education center that seeks to integrate production and play.
zonal program map
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isometric views: walking woods, pedestrian roadway, open seating
FRANKLIN PARK ENTRANCE boston
Crossing the Midline: An Amendment to Olmsted’s Plan contemporizes Frederick Law Olmsted’s vision for Franklin Park, the final component of Boston’s Emerald Necklace. Through the careful preservation and manipulation of his primary design principles, namely the setting up of changing views and the curation of movement through an interplay of topography, circulation, and tree spacing, the intentional barrier between the city and park is dissolved and a series of connected urban plazas is introduced to activate the edge.
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intervention plan / circulation isometric
FRANKLIN PARK boston
sections of generational plantings
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axonometric: program excerpts
FRANKLIN PARK boston
spring perspective: the boardwalk
Preserving Olmsted’s vision for Franklin Park requires one basic, counterintuitive move: giving a portion of its perimeter up to the city. Dissolving the intentional barrier between the “country” park’s eastern edge and the city of Boston through a network of pathways which allow for cross-lateral movement becomes the agenda in rejuvenating a declining park.
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autumn perspective: platform hill
As Olmsted drew his designs out of the topography at hand, manipulating landform consciously and conservatively, this project reconfigures the ground immediately adjacent to the street. Contours are pulled back along the edge and gathered up near corners and major entrances to open up spaces for public gathering.
FRANKLIN PARK boston
section perspective: corner square As keyholes into the park’s interior, these smaller plazas hint at a more permeable environment. The cuts where the contours have been pulled back and the soil removed become the grounds for revegetation.
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plan
EDGE EFFECT cambridge
detail plan
Edge Effect seeks to revitalize a small urban delta at the heart of Cambridge, Massachusetts as the site for a shared gathering place between the city of Cambridge and Harvard University. This small urban plaza is divided into two main spheres, a roughly public one for large-scale, organized events and a more private one that invites more intimate and spontaneous encounters.
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site section elevation
To soften the transition, porous rows of resilient roadside vegetation are introduced in imitation of diorama panels, which create a gradient of visibility and privacy for occupational diversity within a small urban plaza. As ones moves through the site to its point, a gradual change in size relationships occurs. The desired effect is one in which the visitor appears to shrink in size and despite ascending the tiers, begins to lose visibility, encouraging a slower and more cautious pace.
EDGE EFFECT cambridge
sequential section elevations
PRODUCED BY AN AUTODESK EDUCATIONAL PRODUCT
PRODUCED BY AN AUTODESK EDUCATIONAL PRODUCT
PRODUCED BY AN AUTODESK EDUCATIONAL PRODUCT PRODUCED BY AN AUTODESK EDUCATIONAL PRODUCT PRODUCED BY AN AUTODESK EDUCATIONAL PRODUCT
PRODUCED BY AN AUTODESK EDUCATIONAL PRODUCT
PRODUCED BY AN AUTODESK EDUCATIONAL PRODUCT PRODUCED BY AN AUTODESK EDUCATIONAL PRODUCT PRODUCED BY AN AUTODESK EDUCATIONAL PRODUCT PRODUCED BY AN AUTODESK EDUCATIONAL PRODUCT
PRODUCED BY AN AUTODESK EDUCATIONAL PRODUCT
PRODUCED BY AN AUTODESK EDUCATIONAL PRODUCT PRODUCED BY AN AUTODESK EDUCATIONAL PRODUCT
PRODUCED BY AN AUTODESK EDUCATIONAL PRODUCT
PRODUCED BY AN AUTODESK EDUCATIONAL PRODUCT PRODUCED BY AN AUTODESK EDUCATIONAL PRODUCT
PRODUCED BY AN AUTODESK EDUCATIONAL PRODUCT
PRODUCED BY AN AUTODESK EDUCATIONAL PRODUCT
PRODUCED BY AN AUTODESK EDUCATIONAL PRODUCT PRODUCED BY AN AUTODESK EDUCATIONAL PRODUCT PRODUCED BY AN AUTODESK EDUCATIONAL PRODUCT PRODUCED BY AN AUTODESK EDUCATIONAL PRODUCT
Black Birch, Betula nigra Common Witchhazel, Hamamelis virginiana Staghorn Sumac, Rhus typhina Red Chokecherry, Aronia arbutifolia Kentucky Bluegrass, Poa pratensis
PRODUCED BY AN AUTODESK EDUCATIONAL PRODUCT
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perspective 1
As traditional Japanese gardens achieved deep space by tricking the eye in creating a sense of depth within a very small, contained space, the illusion set up in Edge Effect is one of distance. A small site, through elevational change and increasing vegetation heights miniaturizes a larger landscape. Somewhat counterintuitively, creates the illusion of deep space through a clear separation of foreground, middleground, and background.
EDGE EFFECT cambridge
perspective 2
The plaza sets up two opposing views, one from either extreme: the first reveals, the second conceals. In comparison to the relatively open panoramic view from the Quincy Street side, the view from the tunnel and overpass through the delta’s point is obscured by the layered vegetation screens, reducing the site’s transparency. One’s sight is veiled by the sub-canopy foliage and repetitive stem structure.
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diorama perspectives [section model]
EDGE EFFECT cambridge
isometric / detail
Vegetation heights and distinct occupational uses correspond to the spatial arrangement of the three tiers. Like a paper pop-up, reminiscent of a stage set or a diorama, the planting rows act as screens to separate between passive and active occupation. EXPLODED ISOMETRIC SCALE 1:225 01
5
10
20
25 M
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study perspectives
EDGE EFFECT cambridge
plant selection studies
CYPERUS PAPYRUS papyrus sedge
COLOCASIA ESCULENTA var. ANTIQUORUM 'black beauty' elephant ear
LYSIMACHIA NUMMULARIA creeping jenny 'auria'
COURTYARD WETLAND
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runoff / percolation studies
ANGLE OF REPOSE (DRY SAND)
FUNNEL FLOW
CONICAL SURFACE RUNOFF
CONIC GARDEN tucson
SURFACE ANALYSIS
axonometric (vegetative proliferation) The berms and the conic depressions shaping the landform of this garden determine water flow. The berms’ high points create ridges which points runoff into multiple watersheds while the cones act as micro-basins. Water catchment is concentrated along the perimeter of the garden where traffic is also hindered by steeper grade. The largest cone diameter is thus located along the highest percent slopes to maximize collection and mitigate flashfloodig in the washes.