Lake Todos los Santos is located in the Andean pre-mountain range in the Araucanian lake district of southern Chile within the latitudinal range of 39-42S. Lakes in the district have many biotic and abiotic characteristics in common, but differ in the extent of their oligotrophy.
L. Todos los Santos has a surface area of 178.5 km2 and a large volume owing to its great depth reaching a maximum of 337 m. The catchment area of the lake is fairly wide, being 17 times as wide as the lake surface. Its origin is both glacial and volcanic. During in the Ice Age, two glacier arms, one flowing down southward through the present Negro River valley and the other in the opposite direction through the Blanco River valley, converged in the central valley and advanced westward excavating the tertiary valley to form the depression now occupied by Lakes Todos los Santos and Llanquihue. After the disappearance of the ice, the action of Osorno and Calbuco Volcanoes divided the two lake basins with volcanic matters. Matters from Tronador Volcano also reached the lake via Blanco River glacier.
The lake is warm monomictic and oligotrophic. The concentration of major nutrients are low. The highest carbon assimilation rate per unit amount of chlorophyll occurs in winter, but the primary production reaches its highest level at the beginning of summer, though the productivity itself is low (1, 2).
C. PHYSICAL DIMENSIONS
Surface area [km2]
178.5
Volume [km3]
34.4
Maximum depth [m]
337
Mean depth [m]
191
Length of shoreline [km]
125
Residence time [yr]
4
Catchment area [km2]
3,036
D. PHYSIOGRAPHIC FEATURES
D1 GEOGRAPHICAL
Bathymetric map: Fig. SAM-11-1.
Number of main islands (name and area): Cabras.
Number of outflowing rivers and channels (name): 1 (Petrohue R.).
D2 CLIMATIC
Climatic data at Puerto Montt*, 1911 1959 (3)
Jan
Feb
Mar
Apr
May
Jun
Jul
Aug
Sep
Oct
Nov
Dec
Ann.
Mean temp. [deg C]
15.2
14.8
13.2
11.2
9.3
8.0
7.6
7.8
8.8
10.6
12.2
13.9
11.1
Precipitation [mm]
90
139
139
181
236
257
209
197
158
119
131
125
1,981
* Altitude 10 m.
Fig. SAM-11-1 Bathymetric map [m](1).
Water temperature [deg C]
Fig. SAM-11-2
Time-depth diagram of water temperature (1).
Freezing period: None.
Mixing type: Monomictic.
Notes on water mixing and thermocline formation
The winter circulation results in a homeothermy between 8.1 8.8deg C with a small difference between surface and bottom. Surface layers begin to warm up in the beginning of spring, the heat penetrating to a depth of 62 m.
Fig. SAM-11-3
Thermal and oxygen variations at different depths (1).
E. LAKE WATER QUALITY (1)
E1 TRANSPARENCY [m]
Center of the main basin (Fig. SAM-11-1), 1982 1983.
Winter (June) 4; spring (December) 13; mean 10.2.
E2 pHCenter of the main basin, 1982 1983
Depth Jan
Feb
Mar
Apr
May
Jun
Jul
Aug
Sep
Oct
Nov
Dec
Mean* 7.0
6.6
6.5
7.5
7.4
6.9
7.0
6.7
7.1
7.1
7.0
7.6
* Mean of observations at 0.1, 15, 40, 60 and 100 m depth.
E4 DO [mg l-1]
1982 1983
Depth Jan
Feb
Mar
Apr
May
Jun
Jul
Aug
Sep
Oct
Nov
Dec
Mean
10.2
9.9
10.3
9.8
9.6
10.2
10.8
7.7
10.6
10.6
10.9
10.9
E6 CHLOROPHYLL CONCENTRATION
Fig. SAM-11-4
Seasonal variation of chlorophyll concentration [mg m-2] and primary productivity [mg C m-2 hr 1](1).
E7 NITROGEN CONCENTRATION
Fig. SAM-11-5
Vertical distribution of primary productivity and biotic components (1).
Fig. SAM-11-6: Relative abundance (A) and biomass (B) of algal groups (1).
Fig. SAM-11-7 Biomass of two phytoplankton species (cumulative values for 0.1 45 m layer) (1).
Fig. SAM-11-8: Monthly variation of zooplankton abundance and biomass (1).
G. SOCIO-ECONOMIC CONDITIONS
G2 INDUSTRIES IN THE CATCHMENT AREA AND THE LAKE
Secondary and tertiary industries: None.
Numbers of domestic animals in the catchment area: Negligible.
H. LAKE UTILIZATION
H1 LAKE UTILIZATIONSource of water, fisheries, tourism, recreation (sport-fishing) and navigation.
I. DETERIORATION OF LAKE ENVIRONMENTS AND HAZARDS
None (1, 2).
J. WASTEWATER TREATMENTS
J1 GENERATION OF POLLUTANTS IN THE CATCHMENT AREA (1, 2)
a) Pristine lake environments.
K. IMPROVEMENT WORKS IN THE LAKE (1, 2)
None.
L. DEVELOPMENT PLANS (1, 2)
None.
M. LEGISLATIVE AND INSTITUTIONAL MEASURES FOR UPGRADING LAKE ENVIRONMENTS
M3 RESEARCH INSTITUTES ENGAGED IN THE LAKE ENVIRONMENT STUDIES
Instituto de Zoologia, Universidad Austral de Chile, Valdivia
Departmento Botanica, Universidad de Concepcion, Concepcion
Instituto de Biologia, Unitersidad Catolica de Valparaiso, Valparaiso
N. SOURCES OF DATA
Questionnaire filled by the editors with the support of Dr. H. C. Campos, Instituto de Zoologia, Universidad Austral de Chile, Valdivia, Chile, based on the following sources.
Campos, H., Steffen, W., Aguero, G., Parra, O. and Zuniga, Z. (1990) Arch. Hydrobiol., 117: 453 484.
The editor's observation.
Miller, A. (1976) The climate of Chile. "World Survey of Climatology, Volume 12, Climates of Central and South America" (ed. Schwerdtfeger, W.), pp. 113 145. Elsevier Publishing Company, Amsterdam-London-New York.