Disturbance to Mangroves in Tropical-Arid Western Australia: Hypersalinity and Restricted Tidal Exchange As Factors Leading to Mortality
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IJ.. DISTURBANCE TO MANGROVES IN TROPICAL-ARID WESTERN AUSTRALIA: HYPERSALINITY AND RESTRICTED TIDAL EXCHANGE AS FACTORS LEADING TO MORTALITY Environmental Protection Authority Perth, Western Australia Technical Series. No 12 June 1987 052457 DISTURBANCE TO MANGROVES IN TROPICAL -ARID WESTERN AUSTRALIA : HYPERSALINI1Y AND RESTRICTED TIDAL EXCHANGE AS FACTORS LEADING TO MORTALI1Y David M Gordon Centre for Water Research and Botany Department University of Western Australia, Nedlands, 6009, Western Australia Environmental Protection Authority Perth, Western Australia Technical Series. No 12 June 1987 i. ACKNOWLEDGEMENTS I thank C Nicholson of the Environmental Protection Authority, Western Australia, for introducing me to the environmental problems of mangroves in this region during preliminary work for this study. R Nunn and D Houghton of Woodside Offshore Petroleum Pty Ltd provided access to the King Bay supply base and low-level aerial photographs of their dredge-spoil area. N Sammy and K Gillen provided access to and information on mangroves within the salt evaporator of Dampier Salt Pty Ltd. D Button of Robe River Iron Associates provided information on mangroves at their Cape Lambert site. R Glass and I L Gordon assisted with collection of soils and I Fetwadjieff with their analysis. The project was funded by Marine Impacts Branch of the Environmental Protection Authority, Western Australia, which provided use of a field station and support, and was carried out during tenure of a research fellowship in the Centre for Water Research, University of Western Australia. i CONTENTS Page i. ACICN'OWLEDGEl\IBNTS ...... ... .. ....... ....... .. .. ....... .. ... ......... .. ......... .... ......... ... .. ii. SUMMARY V 1. INTRODUCTION 1 2. MATERIALS AND l\IBTHODS .................. ............... ..................... .. ...... .... .. .. .. 2 2.1 WCATION OF STIJDY .... ........................... ... ... .. ... .......... ... .................... ... ..... 2 2.2 AREAS OF MANGAL .............. .... ..... .. ........ .. ...... ... .. ............ .................. ........... 2 2.3 TIDAL EXCHANGE ...................... ............................................. .... ................... 3 2.4 GROUNDWAIBR SAMPLING .. .. .. ..... .. ... .. .... ..... ... .. ... ................. ....... .... .... .. ..... 3 2.5 SOIL PROPERTIES .... .......................... .. .. ........ .... .... .... ... ............................ ..... 5 3. RESULTS .................... ........... .. ....... ........... .. .......... ........ ............ .. .................. 5 3.1 EXIENTOFMANGALS ................... .. ... .......................................... ........... ... ... 5 3.2 SOURCES OF DISTURBANCE TO MANGALS ........ ........................................ 5 3 .2.1 WITIINELL BAY . .. ... .. .. .. .. .. .. .. .. .. .. .. .. .. .. .. .. .. ... ..... .. .. .. .. .. .. .. .. .. .. .. .. ... .. .. .. .. 6 3.2.2 KING BAY CAUSEWAY . .. .. .. ... .. ........ .... .. .. .. .. ... .... ... .. ... .. ... .... .... .. .. .. ... .. .. .. .... 6 3.2.3 SOU11-I-WEST KING BAY ....................................................... .. ............ ... ...... .. 7 3.2.4 KING BAY "SPOIL AREA 4" .. ...................................... ... ........ .......................... 9 3.2.5 LEVEE 24, DAMPIER SALT P1Y. LTD. 9 3.2.6 NICKOL BAY, KARRATHA TOWNSITE 9 3.2. 7 SAM'S CREEK . .. .. .. .. .. .. .. .. .. .. .. 9 3 .2 .8 POPE'S NOSE CREEK . .. .. .. .. .. .. .. 10 3.2.9 JOHN'S CREEK . .. .. .. .. .. .. .. .. .. .. .. .. .. 10 3.2.10 COSSACK CAUSEWAY ... ................ .. .................... ......................... .... ...... .. ...... 10 3.2.11 COSSACK TOWNSITE . .. .. .. .. .. .. .. .. .. .. .. .. 11 3.2.12 WICKHAM SEWAGE POND .. ............ .................... .. ..... ...................... .... ... .... ... 11 3.3 TIDAL EXCHANGE . .. .. .. .. .. .. 11 3.3.1 FREQUENCY AND MAGNITUDE OF TIDAL RECHARGE .. ........ .. ..... ...... 11 3.4 SALINfIY ... .... ... ... ........................... .. .............. ......... .............. .. ..... ... ........ .. ..... 14 3.4.1 SPATIAL VARIATION .. .. .. .. .. .. .. .. .. .. .. .. .. ... .. 14 iii CONTENTS (contd) 3 .4.2 TEMPORAL VARIATION .. .... ...... ... .. ........................ ... .......... ...... ..................... 16 3.4.3 EFFECT OF VARIABLE TIDAL RECHARGE ON SOIL PROPERTIES AND THE WATER TABLE .. .. .. .. ... .. .. .. .. .. .. .. .. ... .. .. .. .. ... .. .. .. .. .. 18 3.4.3.1 S a linity .............................. .. ............................................................. ...... .. .... 21 3.4.3.2 Chloride ...... .. ..................... ....... ......... ........... .. .... .. .... ...................... .. .. .. ......... 21 3.4.3.3 Soil Moisture and the Water Table . .. .. .. .. .. .. ...... .. .. .. 22 3 .5 EFFECT OF DISTURBANCE TO TIDAL EXCHANGE ... .. 22 3.5.1 WATER RE1ENTION . .. .. .. .. .. .. .. .. .. .. .. .. .. .. .. .. .. .. .. .. .. .. ... .. .. .. .. 22 3 .5.2 ALTERED SOIL PROPERTIES .. .... ...... .. ....... .... .. .. .. ..... ........ ..... ... .... .. ... .. .. ..... 25 4. DISCUSSION . 28 4 .1 TIDAL RECHARGE AND SALINI'IY..... .... .. .. .. .. 28 4.2 SOIL PROPERTIES. .. ..................... ......... ..... .................. ........... .................. ...... 30 4.3 DISTIJRBANCE AND STRESS.. .. .. .... .. ... ........ ................ ........ ........................... 30 4.3.1 EFFECTS OF ROAD CONSTRUCTION ON TIDAL EXCHANGE......... ........ ...... 31 5. CONCLUSIONS . .. .. .. ......... .. .. ... .. ... .. .. .. .. .. .. ....... .. .. .. .. .. .. ... .. .. ... ..... .. .... ... 33 6. REFERENCES . .. .. .. .. ... .. .. .. .. .. .. .. 34 iv ii. SUMMARY 1. Sources and extent of disturbances to mangroves are described for the arid Dampier Cossack region of the Pilbara,Westem Australia. 2 2. Over 16% of the 70km ofmangals occurring from Cape Preston to Cape Lambert are now dead. Avicennia marina makes up 87% of living mangroves in the region. 3. Greatest mortality of mangroves has occurred from permanent ponding of seawater during construction of brine ponds for a salt evaporator close to Dampier. 4. Other sites with mangroves suffering widespread mortality are landward-located, in hypersaline soils and with disturbance to natural tidal exchange. 5. Disturbances to mangroves are related to urban and industrial development and include examples of altered tidal exchange, removal of mangroves, dumping of dredge spoil and bunding. 6. Comparisons of tidal exchange and soil properties on each side of a road truncating a mangal implicate two factors in decline and death of the mangroves landward of the road, and these have their greatest impact at dilTerent times of the year. • Reduced frequency and duration of seawater recharge, around the time of the winter solstice, which increases salinity. • Retention of seawater, around the time of the equinoxes, which extends the duration of inundation and submergence of breathing roots from hours to days. 7. Living mangroves in this region are typically associated with groundwater salinities below 90 0 /00 . 8. Changes in soil properties measured over a tide cycle reveal that during the absence of seawater recharge soil salinity increases to very high values at the surface but rapidly re-establishes lower values with the return of tidal wetting. Further down the soil profile salinity and moisture remain relatively stable irrespective of tidal wetting or drying. Changes in chloride mirror those of salinity over the tide cycle and constitute about 70% of IDS. 9. The water table is shallow, being at the surface during inundation and within 10 cm of the surface between inundations during the wetting phase of the tide. In the absence 1 of recharge this falls an average 7 cm d- . 10. Groundwater salinity is diluted for short intervals (hours) during tidal inundation in shallow bioturbated soils but rapidly re-establishes higher salt concentrations following inundation. 11. Salinity of groundwater under salt flats landward of the main vegetation zone is hypersaline, spatially-variable and temporally-stable; changes in salinity between successive tidal wettings are small and are apparently not strongly influenced by inundating seawater. 12. There were differences in soil properties on each side of a road restricting tidal exchange. Over the same tide cycle salinity was elevated by an average 26 O/00, up to a maximum 41 0 /00, at the depths of the cable roots under the remaining living trees in the tidally-restricted mangal, compared with healthy trees in the adjacent unrestricted site. Soils in the tidally-restricted mangal also displayed a lower silt and higher clay fraction. V 13. Soil properties were measured at the extreme seaward and landward margins of the dead zone of mangroves in the tidally-restricted mangal and compared with those separated by the road in the adjacent, healthy tidally-unrestricted mangal. This suggests that soil salinity has been increased by about 20 0 /00 under the remaining living trees close to the road and by about 50 O/00 at the extreme landward limit of the original, but now-dead, mangroves. 14. Differences in soil properties on each side of the road at Cossack over a tide cycle suggests that tidal restriction introduced by this disturbance has had most impact on the trees through its role in increasing the salt content of the water supply rather than reducing the amount of water available externally to the roots. 15. Priority should be given to minimising changes to the natural exchange of seawater