International Archives of the Photogrammetry, Remote Sensing and Spatial Information Sciences, Vol XXXV, Part B7. Istanbul 2004
Up to determined limits urban condensation is of interest for
city administration, due to bigger social profitability of public
equipments and installed substructure basic services, avoiding
expenditure of money in peripheral areas where populating
increase occur (CONTADOR, 1997). Countries under
economical crisis have difficulty to implant adequate plans; as
consequence, the utilized urban condensation parameters differ
much from the idealized ones, which results in a complete
chaos of the urban management (CARVALHO, 2000). The
paper must be compiled in one column for the Title and
Abstract and in two columns for all subsequent text. All text
should be single-spaced unless otherwise stated herein. Left and
right justified typing is preferred.
The main function of a water supply system is to furnish fresh
water to the community directly in the houses and in quantities
compatible with the real necessities. It is highly desirable the
establishment of a predictive plan in confrontation with the
urban concentration, in order to attain up to date and future
results, through integrative actions of public bodies (LLAMAS
et GARRIDO, 1997). In companies in charge of water
distribution one may depict disarray between project and
operation, which results in expansion of the net without
observance of technical premises. As consequence water lacks
in the faucets due to insufficient pressure and minimum
outflow.
When urban expansion runs independently or ahead urban
planning generally the law is broken especially because many
clandestine water tubing of lower quality are constructed out of
control of the distributing company. The constant ruptures of
such tubing function as important occult draining points of the
water net. These conflicts are source of important social,
ecologic, sanitary and economical damages, protagonists of an
authentic urban catastrophe.
The catastrophe theory represents a universal method to explain
transitions through leaps, discontinuities and unexpected
changes in quality (figure 1) (ARNOLD, 1989).
| STABLE BALANCED STATE |
Y Y
MILD CONTINUOUS SUBITANEOUS
QUALITATIVE CHANGE QUALITATIVE CHANGE
Y Y
| SYSTEM FRAGILITY | | SYSTEM COLAPSE |
Y y
| OSCILLATIONS | | NO OSCILLATIONS |
Y Y
NORMALIZATION CATHASTROPHE
Example: city water rationing Example: abolishing city water
from 0:00 to 6:00 am supply
Figure 1 - Diagram of the catastrophe theory.
Source: Adaptation from R. Thom in Arnold, 1989.
518
2. MATERIALS AND METHODS
2.1 Area of Study
The city of Florianopolis, SC. has an area of 436.5 Km”, being
localized between the latitudes 27°25’ and 27°50” south and
longitudes 48°25’ and 48°35 west. Its geographic limits
comprehend an insular area of 424.4 Km” and a continental area
of 12.1 Km? (figure 2).
FLORIANÓPOLIS 5
Figure 2 - Outline of the city of Florianópolis.
Source: Guia Digital Florianopolis — ed.2002.
To reduce the area of study it was elected the District of Santo
Antonio de Lisboa situated in the mid-west of the island,
because the following criteria of study were fulfilled in a way to
grant representative ness of the global system: daily macro-
measurements in confrontation with relative consumer-micro-
measurements; daily water necessities relative to home-unities;
weather data, particularly envisaged to weekly, monthly and
yearly variations.
Otherwise the area (Condominium Mareney, Ostras' street and
Brito alley) was elected because of its characteristic supply
system of reservoirs along the net and because some areas of
the District present variable intensities of urban development.
The population of the District is 5.338 inhabitants (IBGE,
2000).
2.2 Cartography
In accordance to a aero-photogrammetric survey (scale 1:2000)
performed in February 2000 by Aeroconsult Aerolevantamentos
e Consultoria S/A a reconstitution of the area of study was
obtained and the topographic map of the research was
digitalized, as base to all other thematic maps. The aero-survey
presented the following characteristics:
Universal Transverse Mercator Projection — UTM;
Origin of the distance in kilometres UTM Equator and Central
Meridian, the constants 10,000 Km and 500 Km respectively
accreted;
Central Meridian = 51? WGR;
Coefficient of linear deformation in the middle of the sheet (K)
= 1.0003315; 3
Vertical datum = Imbituba — SC;
Horizontal datum = SAD-69;
Aero-photogrammetric covering — 1:8000 (Jan 2002);