menu.header.image.unacom.logo
 

National Committee on Marine Sciences (NCMS)

Permanent URI for this communityhttps://repository.unesco.gov.ph/handle/123456789/6

Browse

Filters

1995 - 19982

Settings

AGROVOC Keyword: search.filters.agrovoc.sediment analysis

Search Results

Now showing 1 - 2 of 2
  • No Thumbnail Available
    Relationship between sediment conditions and mangrove Rhizophora apiculata seedling growth and nutrient status
    Duarte, C. M.; Geertz-Hansen, O.; Thampanya, U.; Terrados, J.; Fortes, M. D.; Kamp-Nielsen, L.; Borum, J.; Boromthanarath, S. (Inter-Research Science Center, 1998)
    The growth rate and nutritional status of Rhizophora apiculata seedlings were analyzed across mangrove stands with different sediment composition in The Philippines and Southern Thailand. Plant growth differed 10-fold and the production of new leaves, roots and branches varied between 50- and 100-fold across sites. Most (>60%) of the variance in mangrove growth rate across systems could be accounted for by differences in the nutrient concentration of the leaves, which was in turn related to the interstitial nutrient concentration and the silt plus clay content of the sediments. Nutrient-poor coarse sediments were characteristic of mangroves located in the mouths of rivers draining small watersheds, while sediments at the mouths of large rivers had high silt, clay, and nutrient contents, thus allowing the development of nutrient-sufficient, fast-growing R. apiculata seedlings. The growth of R. apiculata seedlings increased significantly when the plants grew adjacent to rivers draining areas >10 km2. The results provide evidence that growth of R. apiculata seedlings at the edge of the progressing mangrove forests is often nutrient limited, and that the extent of nutrient limitation depends on the delivery of silt and nutrients from the rivers. The coastal zones adjacent to small (<10 km2) drainage areas seem unsuitable to support adequate growth of R. apiculata seedlings, and afforestation programmes should, therefore, target mud flats adjacent to large rivers instead.
  • No Thumbnail Available
    Heavy metal fluxes in Bang Pakong River Estuary, Thailand: Sedimentary vs diffusive fluxes
    Cheevaporn, V.; Jacinto, G. S.; San Diego-McGlone, M. L. (Elsevier BV, 1995-04)
    Estimates of the flux of heavy metals into the sediments (sedimentary flux) of Bang Pakong River Estuary and the diffusive flux of these metals across the sediment-water interface provide quantitative approximations on the movement of heavy metals from the water column into the sediments, and vice versa. Results showed higher sedimentary flux of Cu, Pb, Zn, Cd, Cr and Ni (0.1–16.8 μg cm−2 yr−1) relative to the diffusive flux of these metals (0.01–4.8 μg cm−2 yr−1). The percentage diagenetic contribution (ratio of diffusive flux to sedimentary flux) of these metals ranged from 10–91%. This suggests that diagenetic remobilization and release of these metals from the sediments into the overlying water may contribute to the subsequent redeposition of these metals into the sediments. Metal enrichment at the surface sediments when compared with deeper sections of the sediment may not necessarily be interpreted as evidence of recent natural, anthropogenic inputs alone, but may also be a consequence of the deposition of metals previously released from the sediments through diagenesis.