Storage Capacity and Water Quality of Lake Ngardok, Babeldaob Island, Republic of Palau, 1996Ð98

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Storage Capacity and Water Quality of Lake Ngardok, Babeldaob Island, Republic of Palau, 1996Ð98 U.S. Department of the Interior Storage Capacity and Water Quality of Lake Ngardok, Babeldaob Island, Republic of Palau, 1996–98 U.S. GEOLOGICAL SURVEY Water-Resources Investigations Report 99-4118 BABELDAOB A E S E N I P P I L I Lake H P Ngardok N A E C O C I F I C A P Prepared in cooperation with the REPUBLIC OF PALAU Storage Capacity and Water Quality of Lake Ngardok, Babeldaob Island, Republic of Palau, 1996–98 By Chiu Wang Yeung and Michael F. Wong U.S. GEOLOGICAL SURVEY Water-Resources Investigations Report 99-4118 Prepared in cooperation with the REPUBLIC OF PALAU Honolulu, Hawaii 1999 ENT OF T TM H R E A IN P T E E D R . I U.S. DEPARTMENT OF THE INTERIOR S O . R U BRUCE BABBITT, Secretary M A 49 RCH 3, 18 U.S. GEOLOGICAL SURVEY Charles G. Groat, Director The use of firm, trade, and brand names in this report is for identification purposes only and does not constitute endorsement by the U.S. Geological Survey. For additional information write to: Copies of this report can be purchased from: District Chief U.S. Geological Survey U.S. Geological Survey Branch of Information Services 677 Ala Moana Blvd., Suite 415 Box 25286 Honolulu, HI 96813 Denver, CO 80225-0286 CONTENTS Abstract . 1 Introduction . 1 Purpose and Scope . 1 Previous Studies . 2 Acknowledgments . 2 Description of Study Area. 2 Data-Collection Methods . 5 Storage Capacity . 7 Water Quality. 13 Summary . 19 References Cited . 19 FIGURES 1–4. Maps showing: 1. The island of Babeldaob, Palau Islands, Western Pacific Ocean. 3 2. Cross sections and water-quality sampling sites, Lake Ngardok, Palau, 1996. 4 3. Bathymetry of Lake Ngardok, Palau, 1996 . 6 4. Bed elevation at cross sections, Lake Ngardok, Palau, 1996. 20 5. Elevation/surface-area and elevation/capacity curves for Lake Ngardok, Palau, 1996 . 8 6. Rainfall and lake elevation at Lake Ngardok, Palau, from July 1996 to July 1997 . 12 TABLES 1. Daily mean lake elevation at Lake Ngardok near Melekeok, Palau . 8 2. Elevation/surface-area and elevation/storage-capacity for Lake Ngardok near Melekeok, Palau, 1996 . 9 3. Daily total rainfall, in inches, from Ngardok rain gage near Melekeok, Palau. 10 4. Temperature, dissolved oxygen, and specific conductance at selected cross sections, Lake Ngardok, Palau, 1996. 14 5. Water-quality results at outflow station on April 3, 1996 and November 10, 1997, Lake Ngardok, Palau. 15 6. Pesticides, herbicides, and other volatile organic constituents found to be less than detection limits in water samples from outflow station on April 3, 1996 and November 10, 1997, Lake Ngardok, Palau. 17 7. Data from AECOS Inc. station 20, 1.4 miles downstream of Lake Ngardok outflow, Palau . 18 Contents iii CONVERSION FACTORS Multiply By To obtain acre 4,047 square meter acre-foot (acre-ft) 1,233 cubic meter foot (ft) 0.3048 meter inch (in.) 2.54 centimeter square mile (mi2) 2.590 square kilometer Water temperature is given in degree Celsius (°C), which can be converted to degrees Fahrenheit (°F) by the following equation: Temp.°F = (1.8 temp. × °C) + 32. Air temperature is given by degrees Fahrenheit (°F), which can be converted to degrees Celsius (°C) by the following equation: Temp.°C = (temp. °F – 32) / 1.8. Chemical concentrations are given only in metric units. These are milligrams per liter (mg/L), micrograms per liter (µg/L), or picograms per liter (pg/L). Milligrams per liter is a unit expressing the solute mass per unit volume (liter) of water. One thousand micrograms per liter is equivalent to 1 milligram per liter. One million picograms per liter is equivalent to 1 microgram per liter. Specific conductance is given in microsiemens per centimeter (µS/cm) at 25°C. Turbidity is given in NTU, nephelometric turbidity units. iv Storage Capacity and Water Quality of Lake Ngardok, Babeldaob Island, Republic of Palau, 1996–98 Storage Capacity and Water Quality of Lake Ngardok, Babeldaob Island, Republic of Palau, 1996–98 By Chiu Wang Yeung and Michael F. Wong Abstract As a result, complete mixing of the lake is probably rare. Near anaerobic conditions exist at the lake A bathymetric survey conducted during March bottom. Low dissolved oxygen (3.2 milligrams per and April, 1996, determined the total storage liter) measured at the outflow indicated that water capacity Lake Ngardok to be between 90 and 168 flowing past the outflow was from the deep oxy- acre-feet. Elevation-surface area and elevation- gen-depleted depths of the lake. capacity curves summarizing the current relations among elevation, surface area, and storage capacity INTRODUCTION were created from the bathymetric map. Rainfall and lake-elevation data collected from April 1996 To alleviate overcrowding in Koror, the current to March 1998 indicated that lake levels correlated capital of the Republic of Palau, the Palau government to rainfall values with lake elevation rising rapidly passed a resolution to relocate its capital to Melekeok in response to heavy rainfall and then returning to on Babeldaob Island, the largest of the Palau Islands. normal levels within a few days. Mean lake eleva- Melekeok is on the east coast of Babeldaob and a tion for the 22 month period of data was 59.5 feet nearby freshwater body, Lake Ngardok, was proposed which gives a mean storage capacity of 107 acre- as the major source of domestic water supply for the feet and a mean surface area of 24.1 acre. A float- new capital and nearby villages. To evaluate the storage ing mat of reeds, which covered 58 percent of the capacity and water quality of Lake Ngardok, and to learn more about freshwater lakes in tropical environ- lake surface area at the time of the bathymetric sur- ments, the Republic of Palau entered into a cooperative vey, makes true storage capacity difficult to esti- agreement with the U.S. Geological Survey (USGS). mate. Water-quality sampling during April 1996 and Purpose and Scope November 1997 indicated that no U.S. Environ- mental Protection Agency primary drinking-water This report describes storage capacity and water standards were violated for analyzed organic and quality of Lake Ngardok. A bathymetric survey of Lake inorganic compounds and radionuclides. With suit- Ngardok was done to estimate storage capacity in rela- able biological treatment, the lake water could be tion to lake water-surface elevation. Samples were col- used for drinking-water purposes. Temperature and lected in late March and early April 1996, and dissolved oxygen measurements indicated that November 1997, from the lake outflow for water-qual- Lake Ngardok is stratified. Given that air tempera- ity analyses. At selected lake cross sections, samples ture on Palau exhibits little seasonal variation, it is were collected at depth for analysis of water-quality likely that this pattern of stratification is persistent. properties and constituents. Introduction 1 Previous Studies Climate.--The Palau Islands have a uniform tropi- cal warm and moist climate throughout the year. Sea- No previous studies on the storage capacity and sonal changes are minimal. At the long-term weather water quality of Lake Ngardok exist, although various station on Koror Island, the mean temperature is 81.7°F estimates have been made. The U.S. Army Chief of (National Oceanic and Atmospheric Administration, Engineers (1956) estimated Lake Ngardok to be 2,400 1995). Mean temperature for the coolest months (Janu- ft long, 600 ft wide at the widest part, as much as 9 ft in ary and February) is 81.0°F and for the warmest months depth, and with a capacity of 46 acre-ft. Van der Brug (April, May, and November) is 82.2°F (National Oce- (1984) used these estimates in his water-resource inves- anic and Atmospheric Administration, 1995). Average tigation of the Palau Island. AECOS Inc. (1997) esti- annual rainfall is 148 in. (National Oceanic and Atmo- mated the lake area to be 16 acres and the capacity to be spheric Administration, 1995). Rainfall is variable from 46 acre-ft also. The AECOS Inc. (1997) study also month to month and is usually heaviest in June and July included water-quality data for a sampling point 1.4 mi (National Oceanic and Atmospheric Administration, downstream from the Lake Ngardok outlet. 1995). Rainfall data for Babeldaob are available for short Acknowledgments periods from scattered locations. Van der Brug (1984) Special acknowledgment is made to Patrick Colin determined that climatic descriptions for Koror are rep- of the Coral Reef Research Foundation for providing resentative of conditions at Babeldaob. Comparison of the aerial photographs of Lake Ngardok. the available rainfall records for Babeldaob with those for Koror showed no significant difference in rainfall totals. Nance (1986) estimated that rainfall across DESCRIPTION OF STUDY AREA Babeldaob was between 90 and 110 percent of the rain- fall at Koror and that rainfall in the region of Lake Ngar- The Republic of Palau consists of a chain of dok is 90 percent that of Koror. islands in the western Pacific Ocean, east of the Philip- pine Sea, between latitude 6°53′ and 8°12′ north and Geology.--Babeldaob is a volcanic island formed longitude 134°07′ and 134°39′ east (fig. 1). Babeldaob primarily by the accumulation of volcanic breccia and Island is near the northern end of the island chain and, interbedded tuff which form three geologic formations: 2 with an area of 153 mi , is the largest of the Palau the Babelthuap Formation, the Aimeliik Formation, and Islands. Koror, the current administrative, commercial, the Ngeremlengui Formation (U.S. Army Chief of and population center of Palau, lies directly south of Engineers, 1956).
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