LAGO XOLOTLAN

A view from an eminence of Managua City

Photo.
Photo: A.Kurata


A. LOCATION

  • Leon and Managua, Nicaragua.

  • 12:30N, 86:45W; 37.8 m above sea level.


B. DESCRIPTION

    Lago Xolotlan, also known as Lake Managua, is situated in the Nicaraguan hydrographic depression or Nicaraguan rift valley, which is separated from the Pacific Ocean by a strip of lowlands, to the northwest of Lake Nicaragua, the largest lake in Central America. The two lakes put together cover almost 10% of the country's total area.
    The depression is probably a graben structure formed in the late Tertiary or Quaternary period, though the origin of these two lakes is often described as tectonic or volcanic. There is considerable volcanic activity along the rift valley, and part of it is employed for geo-thermal energy generation.
    Lake Managua is endorheic, or a closed lake system in which evaporation approximately equals inflow, and its water level is controlled primarily by evaporation. According to the Nicaraguan Institute of Natural Resources and Environment (IRENA), there are stratigraphic evidences that the lake water level was once higher than the present level by 10 15 m. The lake would then have formed a single great inland water body together with L. Nicaragua. A broad river had connected the two lakes until the 16th century. The remnant of this connection, the Rio Tipitapa was a free-flowing stream as late as in 1840, but ceased to function as a regular outflow by 1850 and now serves as only an occasional overflow mechanism. The total inputs of water are so closely balanced with the average evaporation (2,270 mm yr-1) that the overflow across the threshold of the Rio Tipitapa of 40.75 m has occurred only three times (1933, 1955 and 1982) in recent history.
    The lake's mean depth is 7.8 m and the deepest point (26 m) is found in a pit near the volcanic Momotombito Island. A greater part of the drainage basin is located to the north of the lake and drained by three major tributary rivers, Rio Viejo, Rio Sinecapa and Rio Pacora. The total inputs of water varies widely within the drainage basin, geographically, annually and seasonally.
    The "dirty dozen" of pesticides from agricultural and pasture lands contaminate the lake. Untreated sewage of one million population of Managua City on the southern shore is also poured into the lake. About 300 small industries discharge their effluents containing mercury, lead other heavy metals and pollutants. Inflowing sediments are mostly fine particles and rich in organic matter. Furthermore, wastes of geothermal energy plants as well as hot spring water containing rich arsenic salts, boron and other substances enter the lake (1, 2).

C. PHYSICAL DIMENSIONS

    Surface area [km2] 1,016
    Volume [km3] 7.97
    Maximum depth [m] 26
    Mean depth [m] 7.8
    Length of shoreline [km] 200
    Residence time [yr] Endorheic
    Catchment area [km2] 6,668

D. PHYSIOGRAPHIC FEATURES

D1 GEOGRAPHICAL
  • Sketch map

  • Bathymetric map

  • Number of main islands (name and area): Momotombito.

  • Number of outflowing rivers and channels: None (endorheic).

    Fig. NAM-60-1
    Sketch map of the lake (1).

    Fig. NAM-60-2
    Bathymetric map [m] with the location of 11 sampling stations (2).

D2 CLIMATIC
  • Climatic data at Managua, 1951 1960 (3)

    Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec Ann.
    Mean temp. [deg C] 26.3 27.2 28.6 29.3 29.4 27.2 26.9 27.2 26.9 26.5 26.3 26.1 27.1
    Precipitation [mm] 4 1 5 6 76 296 134 130 182 243 59 6 1,142
  • Number of hours of bright sunshine: 2,310 hr yr-1.

  • Water temperature [deg C]

    Fig. NAM-60-3
    Daily evolution of water temperature [deg C] and DO [mg l-1] profile on a calm day (rainy reason) and on a windy day (dry season)(2).

  • Freezing period: None.

  • Mixing type: Polymictic.

  • Notes on water mixing and thermocline formation
    The lake water overturns at least once a day even on calm days and mixing frequency increases when wind force grows.

E. LAKE WATER QUALITY (2)

E1 TRANSPARENCY [m]
    Mean for 11 stations, surface, 1988
    Rainy season (July August): 0.2.
    Dry season (April May): 0.37.
E2 pH
    Mean for 11 stations, surface, 1988
    Rainy season (July August): 9.26.
    Dry season (April May): 9.18.
E7 NITROGEN CONCENTRATION
  • NO3-N [mg l-1]
    Mean for 11 stations, surface, 1988
    Rainy season (July August): 4.64.
    Dry season (April May): 1.60.
  • NO2-N [mg l-1]
    Mean for 11 stations, surface, 1988
    Rainy season (July August): 0.21.
    Dry season (April May): 0.05.

F. BIOLOGICAL FEATURES

F1 FLORA
  • Phytoplankton
    Lyngbya contorta, Oocystis spp., Cyclotella spp., Nitzschia acicularis (4).
F2 FAUNA
  • Zooplankton

  • Rotifers (Epiphanes macrorous, Brachionus havanaensis, B. angularis, B. caudatus, B. quadridentatus f. brevispinus, B. plicatilis plicatilis, Keratella americana, Lecane bulla bulla, Filinia longiseta var. limnetica, F. pejleri, Asplanchna sieboldi, Hexarthra sp.) Cladocera (Diaphanosoma fluviatile, Moina micrura), Copepoda (Arctodiaptomus dorsalis, Thermocyclops inversus, Mesocyclops nicaraguensis, M. brasilianus).
  • Fish
    Cichlasoma rostratum, C. managuensis, C. citrinellum, Lapisosteus tropicus (1).
F3 PRIMARY PRODUCTION RATE

    Fig. NAM-60-4
    Photosynthetic activity during three different days [mg O2 m-2 day 1](6).
    : The end of the dry season, 1987.
    : The end of the rainy season, 1988.
    : The end of the dry season, 1989.

    Fig. NAM-60-5
    Profiles of photosynthetic activity at the end of

F4 BIOMASS

    Fig. NAM-60-6
    Seasonal variations of total phytoplankton biomass, dominant species and the proportions of biomass belonging to different taxonomic groups (4).

    Fig. NAM-60-7
    Temporal changes of phytoplankton abundance in the two basins in terms of a) chlorophyll a and b) fresh weight biomass (4).

    Fig. NAM-60-8

    Fig. NAM-60-9

    Fig. NAM-60-10
    Temporal changes of zooplankton mean density and monthly rainfall (5).


G. SOCIO-ECONOMIC CONDITIONS

G3 POPULATION IN THE CATCHMENT AREA (7) (1992)
    Population Population density [km 2] Major cities (population)
    Urban 600,000 Managua (600,000)
    Rural 400,000
    Total 1,000,000 150

H. LAKE UTILIZATION

H1 LAKE UTILIZATION (1)
    Source of water (irrigation and city water), fisheries, tourism and recreation.

I. DETERIORATION OF LAKE ENVIRONMENTS AND HAZARDS

I1 ENHANCED SILTATION (1)
  • Extent of damage: Serious.

I2 TOXIC CONTAMINATION: Fig. NAM-60-11.

    Fig. NAM-60-11
    Estimated (1983) and observed (1984 1986) mercury levels by the industrial discharge (1).

  • Total mercury concentration (8)

    In water [micro l-1], 1988
    Sampling site Jan Apr
    1 787 506
    2 215 0.24
    3 0.19 0.21
    4 - 0.17
    5 - 0.14
    6 - 0.17
    7 - 0.14
    8 - 0.15
    9 - 0.11
    10 - 0.13
    11 - 0.19
    In sediments [micro g 1], 1988 1989
    Sampling site Depth [cm]
    5 10 15 20 25
    1 1.6 1.3 1.6 7.3 9.2
    2 1.8 1.2 1.3 4.4 4.5
    3 0.56 1.12 1.0 1.0 0.82
    4 0.58 0.87 0.1 0.53 0.1
    5 0.6 0.53 0.49 0.37 0.27
    6 0.84 0.96 0.94 0.90 0.61
    7 0.42 0.32 0.27 0.35 0.23
    8 0.42 0.39 0.27 0.26 0.22
    9 0.23 0.06 0.06 0.06 0.13
    10 0.16 0.13 0.12 0.09 0.20
    11 - 0.3 0.2 0.2 0.3
    12 0.25 0.17 0.13 0.22 0.12
    13 0.41 0.44 0.23 0.42 0.42
    14 0.22 0.42 0.15 0.63 0.35
    15 0.34 0.44 0.27 0.48 0.21
    16 0.68 0.52 0.47 0.33 0.22
    17 0.69 0.73 0.56 0.54 0.68
    18 0.84 0.76 0.56 0.27 0.19
    In muscle and liver of Cichlasoma managuense and C. citrinellum
    Area of capture No. Hg (min. max.) [micro g 1] [%] of cases above the permissible value
    Cichlasoma managuense
    - Bahia Miraflores Muscle 21 0.82 (0.42-1.45) 100
    Liver 20 2.33 (0.28-9.98) 95
    - Tipitapa Muscle 14 0.67 (0.43-1.07) 100
    Liver 21 0.24 (0.10-0.70) 9.5
    - San Francisco Libre Muscle 20 0.59 (0.40-0.87) 100
    Liver 25 0.46 (0.10-1.17) 56
    - Puerto Momotombo Muscle 25 0.48 (0.22-1.02 ) 70.8
    Liver 30 0.43 (0.05-1.17) 60
    C. cirinellum
    - Tipitapa Muscle 19 0.094 (0.008-0.45) 15.8
    Liver 20 0.35 (0.068-1.17) 35
    - San Francisco Libre Muscle 20 0.099 (0.008-0.63) 15
    Liver 20 0.88 (0.5-1.97) 100
    - Puerto Momotombo Muscle 21 0.021 (0.008-0.06) 0
    Liver - - -
I3 EUTROPHICATION
  • Nitrogen and phosphorus loadings to the lake [t yr-1](1) (1982)
    T-N: 2,190.
    T-P: 912.
I4 ACIDIFICATION
  • Extent of damage: None.


J. WASTEWATER TREATMENTS (1)

J1 GENERATION OF POLLUTANTS IN THE CATCHMENT AREA
    (f) Severe pollution with limited wastewater treatment.
J3 SANITARY FACILITIES AND SEWERAGE
  • Percentage of municipal population in the catchment area provided with
    adequate sanitary facilities or public sewerage: 75%.

K. IMPROVEMENT WORKS IN THE LAKE (1)

    None.

L. DEVELOPMENT PLANS (1)

    None.

N. SOURCES OF DATA

  1. Questionnaire filled by the editors based on the following sources.
  2. Swain, W. R. (1988) Lake-wide impacts of long-term sources of xenobiotic contaminants: Lake Managua (Nicaragua) and Lake Michigan (United States). "Toxic Contamination in Large Lakes III. Sources, Fate, and Controls of Toxic Contaminants" (ed. Schmidtke, N. W.), pp. 389 427. Lewis Publishers, Chelsea, Michigan.
  3. Montenegro-Guillen, S. (1991) Verh. Internat. Verein. Limnol., 24: 1,155 1,157.
  4. Portig, W. H. (1976) The Climate of Central America. "World Survey of Climatology Volume 12, Climates of Central and South America" (ed. Schwerdtfeger, W.), p. 460. Elsevier Scientific Publishing Co., Amsterdam-London-New York.
  5. Hooker, E. L., et al. (1991) Verh. Internat. Verein. Limnol., 24: 1,158 1,162.
  6. Cisneros, R. O. & Mangas, E. I. (1991) Ibid., 24: 1,167 1,170.
  7. Erikson, R. et al., (1991) Ibid., 24: 1,163 1,166.
  8. Martinez Martinez, F. A., personal communication.
  9. Lacayo, M., et al. (1991) Verh. Internat. Verein. Limnol., 24: 1,174 1,177