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    CENTRAL BRISBANE LANDSCAPE STUDY REPORT

    LUKE BRINSMEAD - N6297498DLB330 - PEOPLE AND ENVIRONMENT

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    CONTENTS

    1.0 INTRODUCTION

    1.1 OVERVIEW 3

    1.2 CENTRAL BRISBANE LANDSCAPE STUDY AREA 3

    1.3 METHODS 4

    2.0 CENTRAL BRISBANE LANDSCAPE BACKGROUND

    2.1 GEOGRAPHY 5-9

    2.2 CULTURAL HERITAGE 9-13

    3.0 CENTRAL BRISBANE LANDSCAPE STRUCTURE APPRAISAL

    3.1 STRUCTURE MAP 14

    3.2 ATTRIBUTE TABLE 15-17

    3.3 NETWORK DIAGRAMS 18

    3.4 FLOWS DIAGRAMS 19

    3.5 APPRAISAL OF LANDSCAPE STRUCTURE 19-20

    4.0 FOCUS AREA LANDSCAPE STRUCTURE REDESIGN

    4.1 FOCUS AREA LANDSCAPE STRUCTURE APPRAISAL 21-22

    4.2 FOCUS AREA LANDSCAPE STRUCTURE REDESIGN 23-24

    5.0 DESIGN DISCUSSION

    5.1 USES OF LANDSCAPE ECOLOGY IN LANDSCAPE DESIGN 24

    5.2 LIMITATIONS OF LANDSCAPE ECOLOGY IN LANDSCAPE DESIGN 25

    CONCLUSION 25

    REFERENCES 26

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    1.0 INTRODUCTION

    1.1 OVERVIEW

    The Central Brisbane Landscape Study Report analyses an aerial photo graph with a scaleof 1:25,000 to outline and trace patches, corridors and networks which were used in alandscape ecology context. The report begins with methods, then moves into cultural

    history and geography; landscape appraisal and structure which includes structure a map,associated attribute tables, a network and flow diagram; following that is the focus areaappraisal and redesign, which uses the upper right quadrant of the aerial photograph; thediscussion and conclusion discusses how the method of landscape ecology is useful andsummarizes major points from the findings. This report aims to aid landscape architects,town planners and urban designers to better design/plan and redesign/plan on a spatialscale to increase ecology, human equality and well being, natural capital and ecosystemservices.

    1.2 CENTRAL BRISBANE LANDSCAPE STUDY AREAImage 1: Satellite Photo. Source: Google Earth

    Image 2: Aerial Photograph of Brisbane city and its nearby surrounding suburbs.Source: Sun Maps

    Brisbane is the third largest city in Australia with a population of around 1.6 million in thegreater metropolitan area. The city is located in the southeast corner of Queensland(27.5S, 153E) and is 960km north of Sydney and 97 km north of the Gold Coast. GreaterBrisbane comprises over 180 suburbs and localities and covers an area of 1,141 km2.Brisbane has a subtropical climate with temperatures ranging between 20-29C in summerand a very pleasant 9-20C in winter. Brisbane has an average annual rainfa ll ofapproximately 1150mm and 242 days a year of sunshine (BOM, 2009).Since the middle ofthe 20th century, much of the farmland was replaced by suburban subdivision and somemedium the high density buildings. Queen Street was developed along the line of the first

    convict buildings, they were purposely built there to be above a severe river fl ood level (deVries, 2003). Immigrants from southern Australia, the UK and Europe were attracted tothe rapidly developing town and sought opportunity to be lumberjacks, farmers andcraftsman who could then afford to purchase allotments of land, favouring hilltops whichprovided a scenic and surveillance view over the farmed landscape (de Vries, 2003).

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    2.0 CENTRAL BRISBANE LANDSCAPE BACKGROUND

    2.1 GEOGRAPHY

    During the late Devonian and Carboniferous periods, circa (c) 370 to 300 million years ago(mya), Australia was still part of Gondwana (Willmott, 2004). The coastline was muchfurther inland and a volcanic mountain chain developed along the edge of the continent asa result of an oceanic crustal plate being subducted under the continent ,see image 1A(Willmott, 2004). As a result friction melted rocks to form magma which then rose to thesurface and was erupted as volcanic lava(Willmott, 2004). These events took place alongmuch of the east coast, from Mackay to Newcastle and is known as the New England FoldBelt (Willmott, 2004). Large amounts of sediments eroded from the volcanic mountainchain and deposited on the continental shelf were some settled and remained (Willmott,2004). At the end of the Carboniferous period, c 300 mya, there was an episode ofcompression and intense deformation of the deep water sediments, see image 1A (2)(Willmott, 2004). They became hardened and converted into rock by pressure, heat andcementing materials such as silica which as a result formed meta-sediments (Willmott,2004). The subduction process beneath the continental edge reduced by the end of the

    Carboniferous period (Willmott, 2004).

    During the preceding early Permian period, c 286 to 265 mya , the crust beneath thecontinental shelf edge relaxed, subsided and extended laterally, as a result shallow seasspread across the continental edge and deeper basins, such as the Esk Trough in theBrisbane Valley, subsided,see image 1B(Willmott, 2004). New sediments weredeposited atop of the previously deformed meta-sediments, however the crust still had ahigh heat flow which melted some magma (Willmott, 2004).Further to the east from theearly Permian to mid-Ttriassic times (280 to 235 mya), volcanic rocks and marinesediments ere being deposited, possibly along an offshore island arc above a newsubduction zone, or in shallow seas behind it, see image 1C(Willmott, 2004). From mid-Permain to mid-Triassic times (about 265 to 235 mya) the continental edg e was subjected

    to major periodic compression, known as the Hunter Bowen Orogeny , see image 1D(Willmott, 2004).The crust again relaxed and extended in the late Triassic period (235 to215 mya), with renewed heat flow and further eruption of volcanic and generation ofgranites, but no meta-sediments as a result, see image 1E(Willmott, 2004).After the

    volcanic-intrusive episode in the latest Triassic times (215 mya) the continental edgebecame much more stable.

    Small flood plains developed in valleys in the mountains of the meta-sediments and thevolcanoes. Despite some lingering volcanic activity, the older rocks were graduallycovered by shales, siltstones and sandstones deposited in and beside these rivers(Willmott, 2004). Coal seems formed in swamps on the flood plain, these deposits weremost prominent around Ipswich and Brisbane(Willmott, 2004). At the end of the Triassic

    period and extending into the Jurassic (about 215 to 180 mya), more extensive areasbegan to be covered by sediments brought down by much larger streams. Large volumesof sand and gravel with some silt were deposited in braided channels and flood plains ofhigh energy rivers to the west and south of Ipswich, and north of Brisbane, see image4(Willmott, 2004). In the latest Jurassic to early Cretaceous times (around 140 mya) theeasternmost edge of the continent was again subjected to deep crustal heating, possiblyas a result of renewed subduction process to the east of the present coastline , see image5(Willmott, 2004). In the early Tertiary period (65 to 45 mya) several small basinssubsided across the region as a result of the tension in the continental crust , see image 6.

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    This was probably a legacy of the tension related to the opening of the Tasman Sea(Willmott, 2004). During the mid and late Tertiary period (30 to 2 2mya), eastern Australia,although essentially stable, was the scene of extensive volcanic activity, which left as itslegacy remnants of large volcanoes still visible today , see image 8(Willmott, 2004). Manyof the mountain national parks near Brisbane were formed by these volcanoes.After thevolcanic episode of the mid-Tertiary, erosion continued and the landscape as we know itbegan to take shape. While the climate was still moist one or more periods of deep

    weathering and leaching created deep soil profiles, termed lateritic profiles (Willmott,2004).

    Figures 3: Geological Events, source:Willmott, 2004

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    Figure 4: Brisbane Soil Classifications, source ASRIS/Google Earth.

    The main soil type in the study area is Hydrosols, with some Ferrosols around KangarooPoint area, some Chromosols south east of Brisbane and some Rhodosols to the southwest of Brisbane.

    Figure 4: Historic Palimpsest (Author photos) Figure 5: Subtropical Adaption Shade

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    Figure 6: Brisbane Metropolitan Regional Ecosystem Map, source: EPA (2009).

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    Within the study area the following regional ecosystems can be viewed in figure 6:

    12.1.2: Saltpan vegetation including grassland and herbland on marine clay plains .12.1.3: Mangrove shrubland to low closed forest on marine clay plains and estuaries .12.2.15: Casuarinaglauca open forest on margins of marine clay plains , classified asENDANGERED.12.3.5: Melaleucaquinquenervia open forest on coastal alluvium, classified as OF

    CONCERN.12.3.6: Melaleucaquinquenervia, Eucalyptus tereticornis, Lophostemonsuaveolenswoodland on coastal alluvial plains.12.3.11: Eucalyptus siderophloia, E. tereticornis, Corymbiaintermedia open forest onalluvial plains usually near coast , classified as OF CONCERN.12.3.14: Banksiaaemula woodland on alluvial plains usually near coast , classified as OFCONCERN.12.5.3: Eucalyptus tindaliae and/or E. racemosa open forest on remnant Tertiary surfaces,classified as ENDANGERED.12.9-10.4: Eucalyptus racemosa woodland on sedimentary rocks.12.9-10.17: Open forest complex often with Eucalyptus acmenoides, E. major, E.siderophloia Corymbiacitriodora on sedimentary rocks .

    12.9-10.19: Eucalyptus fibrosa subsp. fibrosa open forest on sedimentary rocks.12.11.18: Eucalyptus moluccana open forest on metamorphics interbedded volcanic.12.12.14: Shrubby woodland usually of rocky near coastal areas on Mesozoic toProterozoic igneous rocks, classified as OF CONCERN.(EPA, 2009)

    2.2 CULTURAL HERITAGE

    When commandant Henry Miller and his men first arrived into the Brisbane city regionmany of the local Aboriginal clans were displaced and felt they were being squashed out,and literally thats what happened. Surrounding the white settlements were localindigenous people with their spears defenseless against an o pponent with gun weaponry. After some quarrels with the locals Miller and his team found themselves settling in thetriangle of land, now know as the city CBD. It was chosen by commandant Miller becauseit provided a safer location from Aborigines as wel l as having less chance of Malariacompared to the original Redcliff settlement site (de Vries, 2003). The Ngundari andYagura Aboriginal clans previously roamed through this area until the settlement, whichwas known for its scenic water views (de Vries, 2003).

    The first stone buildings of the Moreton bay settlement were constructed by convicts, thefirst of which was the Military Barracks, built in 1828 (de Vries, 2003). Queen Street wasdeveloped along the line of the first convict buildings, they w ere purposely built there to be

    above a severe river flood level, see figure 7 (de Vries, 2003). Some of the stores in thenewly developing Queen Street included a butchery, tannery, fellmonger and adrapery.Stone buildings were constructed of sandstone, while some composed of a smallamount of granite on ground level. The courier building, designed by architect RichardGailey, was one of the first tall buildings in Brisbane, fives stories high.

    Apposite from the courier building was the Australian Mutu al Provident Society (AMP), itwas designed by architects Blackmann and Parks and was built of sandstone and hadreplaced a collection of tumbledown wooden shops known as Refuge Row which hadburned down several times in the past (de Vries, 2003).

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    Many of the small cottages surrounding the CBD had dirt floors, timber walls, brickchimneys, bark roofs and exterior toilets (de Vries, 2003). Surrounding these cottageswere usually fowl-runs, vegetable gardens, fruit and nut trees such as Banana, Lemon,Orange, and Paw-Paw, larger yards had Bunya Pines, Moreton Bay Fig, Camphor Laureland Mango trees (de Vries, 2003).

    In the late 19th

    century double-decker horse-drawn trams were introducedto transport

    people to and from nearby suburbs within approximately five kilometres from the CBD.Horse-drawn trams would not be replaced by electricity until 1898, by 1921 some 180electrified trams were in service (de Vries, 2003). In the 1960s, the Brisbane City Councildecommissioned the trams and replaced them with buses. The streets ground surfacewas still unpaved by 1886, causing quagmire to form during heavy rain. In the early 1880s,Queen Street was in a very poor condition as state funds had b een spent on publicbuildings such as Parliament House, the Treasury Building and the Supreme Court.Consequently, little funds were left to pave Brisbane s dirt roads (de Vries, 2003).

    More immigrants from southern Australia, the UK and Europe were attr acted to the rapidlydeveloping town and sought opportunity to be lumberjacks, farmers and craftsman whocould then afford to purchase allotments of land, favouring hilltops which provided a scenic

    and surveillance view over the farmed landscape. As the trees were removed for timber,farmland was then made available on the flatter areas to grow Maize, Bananas,Pineapples, Sugarcane, Cotton. Beef and dairy cattle as well as sheep were grazed onthis newly cleared land (de Vries, 2003). Security surveillance for preventing Aboriginalattacks was also increased by default as a result of the clearing. Many of the early tracksradiating outward from the settlement were formed by either indigenous routes orlumberjack trails. Since the middle of the 20 th century, much of the farmland wasreplaced by suburban subdivision and some medium the high density buildings.

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    Figure 7(de Vries, 2003)

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    Figure 8(de Vries, 2003)

    Figure 9(de Vries, 2003)

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    Figure 10(de Vries, 2003)

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    3.0 CENTRAL BRISBANE LANDSCAPE STRUCTURE APPRAISAL

    3.1 STRUCTURE MAP

    Figure 11: Brisbane Structure Map

    The structure map, figure 11, shows Brisbanes suburban dominated landscape 68%,within the medium density residential greenfield spaces are found on more so on the flatterareas in the southern suburbs. Many of the greenfield patches are highly fragmentedfrom one another. Most of the high density buildings are located near the major bridges,which supplement the city apartment views at night. The river divides northern andsouthern suburbs with the city also being the dividing land feature. Road and railnetworks use the city as a node to allow people to travel from north to south and east towest.

    Many of the natural patchs edges are convoluted, particular the largest remnant patch,however most of the built environment patches have straight edges. There is very littleremnant vegetation near the rivers edge and on the south eastern side of the river, the

    only large amount is located to the far west of the study site. Most of the remnantvegetation patches are poorly connected and are islandised by the suburban metropolis.The patches adjoining the river or roads usually have a smooth edge on the river or roadside and a convoluted edge on the alternate side. Their boundary width appear to benarrow where patches adjoin built environment and wider adjacent to greenfield sp ace.

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    3.2 ATTRIBUTE TABLE

    Figure 12: Attribute Table 1

    The matrix (low to medium density residential) areathe vast, representing 68% of the study

    area, it permeates through the landscape without leaving few linkages for wildlife to enter,cross or exit. On the edges adjacent to the large remnant path the edge is highlyconvoluted, whereas on the edges adjacent to medium to high density buildings the edgeshave much more straightness to them. The patchsinternals are very well connected toultimately form the two very large patches, quite the opposite attribute for the smallremnant vegetation patches. Many of the remnant vegetation patches, which occupy just7.3% of the subject area,are mostly rounded, with the exception of areas sounding riversor creeks. These islands may be the result of uncleared steep areas unfavourable tofarming or even buildings. The edges which are more convoluted may indicate steepareas whereas smoother edge may indicate flatter ground.

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    Most of the medium to high density residential patches have straight edges, typicalcharacteristic of man-made patches and which is more obvious as the patch sizedecrease.

    Figure 13: Attribute Table 2

    Most of the greenfield patches have a curvilinear and partly convoluted edge, this maybeattributed to adjoining remnant vegetation patches, cul-de-sac encroachment or becausegreenfields are sometimes used by council or developers to fill the in-betweenundeveloped areas.This level of convolution and curvilinearity decreases as the patch sizedecreases. Much of the patches are situated on their lonesome with little or noconnection with remnant vegetation patches or other Greenfield patches.

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    Figure 14: Attribute Table 3

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    3.3 NETWORK DIAGRAMS

    Figure 15: Network Diagram

    The rivers curvlineararity is highlighted by a thick dashed line in figure 15, showing howthe river creates pockets suburbs like New Farm, West End and St Lucia which has fewmain roads within their peninsulatype neighbourhoods. The level of curvlineararity also

    shows the different hardness of the lands surface, as the river deflects off the harder rocksand penetrates through the softer material. Many of the roads are not straight, with theexception of some roads close to the city or on flat land. All of the roads had noconvolution, which was used to help map their smooth boundaries. Many roads narrowas they meander towards the city, indicating increased buil ding density. However therailway lines increase in width nearer to the city. Wildlife networks adjacent to the riverare somewhat narrow and disconnected from each other by residential houses close to therivers edge, they are also disconnected from nearby remnant patches.

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    3.4 FLOWS DIAGRAM

    Figure 16: Flow Diagram

    Much of the surface water flows to the river, which can be seen in the flow map, thereforethe river can be seen as the natural sink. To the north west there is little housing whichcan be used as a guess that the area is quite step which gene rates more surface waterflow. Any greenfield near the city was characterized as a sink for birds, as it providesthem with food and a relatively safe temporary habitat from their natural predators. Mostof the human flow in directed towards the city, indicated by the tall buildings and lack ofvegetation or green space, this therefore represents the human sink. Standout fields,such as the Brisbane Cricket ground, can be classed as another human sink. There aremany more human sinks on this map, such as the University of Queensland, which are notclearly shown as sink on this particular map and therefore not mapped.The large granularcommercial or industrial patches are also seen as a human sink for materials andproducts.

    3.5 APPRAISAL OF LANDSCAPE STRUCTURE

    The matrix has a finer granularity than the medium to high density landscape unit,indicating a detached houses with private garden buffers surrounding each dwelling. Thelow to medium density residential of detached housing dominates the landscape, as aresult there is little greenfield space and remnant vegetation. This is probably due to theautomobile allowing mass people movement during the time of development surrou ndingBrisbane and indeed other areas of Australia and America. Analysing the structure map,the previous farming areas can be imagined where suburbanism has now replaced.

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    It is interesting to note that no farming is practiced near Brisbane, compared to many nonautomobile developed cities around the world which have many farmed fields near citiesand towns. As mentioned, the suburban low to medium density matrix area is very wellfused to form Brisbane city as it is known.

    The area of road corridors is mapped at approximately 10%, however if all the roads wereto be mapped then this figure would easily reach 20% or more. Because most of

    Brisbane is undulating and hilly in areas, most of the roads appear as meanderingnetworks. There is not defined legible ring road surrounding the city, which many otherwell planned cities have to exclude unnecessary vehicular traffic and to clearly define itsboundaries. The roads were more clearly identified as they cut through vegetation,providing contrast between the urban beige and the greenery.

    The medium to high density patches have less greenery surrounding them compared tolow to medium density patches, causing the patches to more easily stand out and appearmore granular. These patches are found orientated mostly around the river, which arereplacing valuable ecosystem space. The city centre, being the largest of these patches,dominates the study area by having a homogenous pattern which has little or no patchesin or near it. Some medium to high density patches were also mapped adjacent to main

    roads, in terms of retail it would allow for good customer exposure to advertising and allowfor ease of delivery of products and ease of customer finding.

    Remnant vegetation patches were quite easily mapped, having a strong contrast betweendark green of the canopy and beige of the building roofs. These patches are quitehomogenous, comparing to the matrix, further aiding the outlining of these patches. Tothe north west of the map, the large remnant patchs edge is being divided up by thematrix, whereas to the east and south little remnant vegetation exists. A reason for whylittle of the presumed mountain area where much of the remnant vegetation lives can befound in sun exposure, farming on south-facing slopes in the southern hemisphere is notas productive as farming on north-facing slopes due to the reduced sun exposure duringwinter.

    The edge of the waterways are smooth and curvilinear, and the corridors homogenousinterior contrasts greatly with the heterogeneous landscape. These attributes make theBrisbane river such a dominant feature within the study area, even though the landscapepercentage is dwarfed by the matrix. The river divides the matrix, I am of the opinion ifthere was no Brisbane River then the matrix would completely surround the city with itsislands of greenfields and remnant patches within the super matrix.

    Most of the greenfield spaces are surrounded by the matrix, with the exception of the CityBotanical Gardens and Roma Street Parklands, or some adjoin natural patches orcorridors. Most of the smaller patches showed straight edges which indicated they were

    parks or fields in relatively flat areas. Most greenfields contrast quite well with the urbanbeige and aided the accurate outline of their boundar ies.

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    4.0 FOCUS AREA LANDSCAPE STRUCTURE REDESN

    4.1 FOCUS AREA LANDSCAPE STRUCTURE APPRAISAL

    Figure 17: Focus Area Structure Map

    I chose the Brisbane city and its nearby areas to for the focus appraisal (figure 17) andredesign as I thought the heart of Brisbane can become an interesting subject to workwith. The focus area comprises all bar the remnant vegetation unit, forming juxtapositions and varying contrasts. However, most of the green fields are notconnected, such as the City Botanic Gardens and Roma Street Parklands. There is littleremnant vegetation surrounding the river near the city,however if more riparian vegetationwas in place the rivers water quality may improveand would most certainly promote safewildlife movement near the city.

    One side of the city is swiped by a main road, which covers a riparian zone near the riverand would most certainly detrimentally affect the sense of place within the city perimeter.

    Relocating the main road would possibly increase the sense of place to be more similar tonearby pocket suburbs and reduce city air pollution. As can be seen in the structure map,there is less Greenfield space in the focus area, with the Greenfield patches being

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    Figure 18: Focus Area Attribute Table

    In figure 18 it can be seen at the zoomed in scale that the matrix is broken up into smallerpatches by roads intercepting, as most of the roads at the previous scale appeared to notclearly divide the matrix. Some of the medium to high density and greenfield patcheswere trimmed a little in the zoomed process, however most retained their original shape.

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    4.2 FOCUS AREA LANDSCAPE STRUCTURE REDESIGN

    Figure 19: Focus Area Redesign

    This redesign (figure 19) represents a consolidation of ecology and human problemscaused by poor land clearing practices and poor road planning, it is a compromisebetween built environment and ecology. In summary the problems of the central Brisbanearea include:Lack of remnant vegetation, poor connectivity between each remnant orgreenfield patches, main road too close to the city, no defined city ring road to decreasevehicular traffic inside the CBD. Few large individual patches or corridors provide morehabitat and diverse mico ecosystems within them than many small patches or corridors.However, the Brisbane layout does not allow for large amounts of land to be altered,instead I chose to form the large parallel corridor adjacent to the river to maximize diversityin a perpendicular restricted site. I have proposed riparian revegetation along selectareas of the Brisbane River, the diagonal hatching represents revegetation wherepossible. For example, there are medium to high density patches adjacent to the riverwhich have gardens which could be eco-logically retrofitted with native regional ecosystemspecies, no buildings would need to be relocated for this retrofit.There are also areas

    where roads adjacent to the river could be narrowed to allow for even more room forrevegetation. The nature-inspired riparian revegetation pattern flows with the and speciesflow river, many remnant and greenfield patches outside the focus area would benefit fromreshaping to be more linear with nature rather than just an afterthought. Many of theparks near the river are partly open and would benefit from a denser canopy to decreaseto level of sun exposure to people. The retrofit would allow wildlife to use the riversconduit the safely travel up and down the river with little risk of impediment from roads.The revegeation would also improve stormwater runoff and the urban heat island effectwith improved infiltration and increased level of shading respectively.

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    The two major gardens in the CBD are currently divided between each oth er by the citysmetropolis, I am proposing a main eco-axis down Albert Street to allow people and wildlifeto traverse through the CBD to gain relatively good access to either patch. To promote theCBD to regain its original peninsular sense of place, I have proposed the main roadadjacent to the CBD to be relocated and completely placed underneath SouthBrisbane/Bank to retain their own sense of place.The relocation of this road would alsoimprove the air quality and ecology surrounding the city botanical garden to help recover

    its more historically natural placeness. It is also hoped from this redesign that estuaryecology will improve along the intertidal areas due to improved habitat and increased foodsupply. To help encapsulate the citys sense of place, I have proposed a small ring roadto circulate vehicular traffic on the perimeter of the CBD to decrease the dominance of theautomobile on the CBD culture and allow for better human circulation within the CBD.Complementing this ring road would be vehicular traffic control measures such closings ofmany carparks in the centre of the CBD and where appropriate roads closures inside thering road.

    5.0 DESIGN DISCUSSION

    5.1 USES OF LANDSCAPE ECOLOGY IN LANDSCAPE DESIGN

    Knowing the location of patches and corridors and the connectivity between them canassist a landscape architect in better understanding is spatially organized how thelandscape interacts between each element. The attributes of natural patches such astheir convolution can be used as an ideal ecological template for designing parks andbuffering zones in new suburban areas. Knowing how fauna move through patches andcorridors complements knowledge of landscape mosaicsand helps assist landscapearchitects to promote ecology to move through a dominant built environment.

    By knowing the percentage of landscape units ,it can provide statistical information to

    improve the equality of unbalanced elements within a lands cape or to prevent furthermonopoly of certain elements such as suburban sprawl or unnecessary roads.Features ofpatches such as boundary width can provide buffering areas for patches and a morediverse ecosystem within a natural patch. In the context of land planning management,Forman quotes think globally, plan regionally, and then act locally (p435, Forman (1995),instead of think globally, act locally. Adding to this Forman also quotes The perennialchallenges in planning, design and management of an area are not only to take a broadspatial view and a long temporal view, but also address all major environmental andhuman issues present (p436, Forman (1995).Together with this he states that on toomany occasions large areas of land are planned with only one primary object, suburbanresidential living is the primary object in many suburbs of Australia since industrialization.Forman finishes this argument by quoting By focusing on the preceding principles in

    landscape and regional ecology the appr oach is broader, incorporating cultural,socioeconomic, aesthetic, and other human dimensions that are explicit, i.e., used inphysical planning, are schematically integrated.

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    5.2 LIMITATIONS OF LANDSCAPE ECOLOGY IN LANDSCAPE DESIGN

    In reference to this particular report, the main concepts of landscape ecology can be usedon various different scales, however if government or council do not use these principles intheir town planning guidelines then developers will continue to develop landscapes th esame way which has resulted in the problems points highlighted in this report in 3.1 and4.1. Excluding politics from the limits of landscape ecology, the theory is limited to

    guessing from map reading. For example, there are many roads and natural/human sinkswhich on many resolution-restricted, non hybrid (without suburbs, roads and major nodes)maps cannot be generated. However, if a hybrid map was used then this could beoverlaid over an aerial map to map these landscape features to map the sinks. In generalhowever, there are few limitations to landscape ecology in terms of contradictions and orimpracticality. It though could prove to be a timely exercise though for some landscapepractices and therefore may not be done to reasonable level during a siteappraisal/analysis.

    6.0 CONCLUSION

    From the historical and geological history information to the landscape appraisals thisreport has documented how previous events have ultimately formed Brisbane as it isknown presently. The information generated from structure maps, network and flowdiagrams has developed a mosaic representation of the central Brisbane area as well asdeveloping a discussion about its spatial characteristics. By focusing on a particularquadrant of the central Brisbane map the same principles were applied to formulate astructure map, a network diagram and a proposed redesign. In summary, the redesignwithin the focus area represents an opportunity, not an unrealistic challenge, for futuredecision makers (mostly politicians) as well as landscape architects to better improveBrisbanes CBD to partly restore its ecology by integrating nature with the builtenvironment.

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    7.0 REFERENCES

    Bureau of Meteorology (2009).Climate statistics for Australian locations. Accessed25.5.09. http://www.bom.gov.au/climate/averages/tables/cw_040214.shtml

    deVries, S and J (2003). History Brisbane: Convict Settlement To River City. Brisbane:Pandanus Press.

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