2007
DOI: 10.1007/s10661-007-9982-x
|View full text |Cite
|
Sign up to set email alerts
|

Assessment of sampling designs to measure riverine fluxes from the Pearl River Delta, China to the South China Sea

Abstract: The Pearl River Delta (PRD), located in South China and adjacent to the South China Sea, is comprised of a complicated hydrological system; therefore, it was a great challenge to sample adequately to measure fluxes of organic and inorganic materials to the coastal ocean. In this study, several sampling designs, including five-point (the number of sampling points along the river cross-section and three samples collected at the upper, middle, and bottom parts at each vertical line), three-point (at the middle an… Show more

Help me understand this report

Search citation statements

Order By: Relevance

Paper Sections

Select...
2
1
1
1

Citation Types

0
14
0

Year Published

2008
2008
2024
2024

Publication Types

Select...
7
1

Relationship

2
6

Authors

Journals

citations
Cited by 31 publications
(14 citation statements)
references
References 17 publications
0
14
0
Order By: Relevance
“…The sampling sites and procedures have been described in detail previously [9] and are detailed in the Supporting Information (). Therefore, only a brief description is presented here.…”
Section: Methodsmentioning
confidence: 99%
“…The sampling sites and procedures have been described in detail previously [9] and are detailed in the Supporting Information (). Therefore, only a brief description is presented here.…”
Section: Methodsmentioning
confidence: 99%
“…Since the hydrophobicity nature, PBDEs have very low water solubility [2], and only a little portion of the PBDEs exist in the water phase. Due to the lower concentrations and technical difficulty in measurement, to our knowledge, few papers have been published related with sea water [31, 32]. Here, main focuses were set on the sediment and biota matrixes.…”
Section: Marine Environmental Levelsmentioning
confidence: 99%
“…Sampling was conducted on December 24, 2010, May 24, 2011, and August 28, 2011, representative of the low-, normal-, and high-flow periods, respectively, during neap tides and approximately 1 h before the intra-day low tides to avoid tidal influences (Ni et al 2008). Water was taken from 0.5 m below the air-water surface, middle of the water column, and 0.5 m above the sediment bed, with a stainless-steel submersible pump to constitute one composite sample.…”
Section: Field Samplingmentioning
confidence: 99%