Literature DB >> 35242948

Data for assessment of sediment, soil, and water quality at Ashfield flats reserve, Western Australia.

Andrew W Rate1, Gavan S McGrath2.   

Abstract

Sediment and water samples were collected using transects and grids within sampling strata, in 2019, 2020, and 2021 from a riparian reserve adjoining the Swan River estuary in Western Australia. Different sampling designs were used each year, with transects and/or grids designed to assess changes in sediment and water quality across assumed environmental gradients such as salinity or distance from possible contaminant sources. Sediments were from 0-10cm; pH and electrical conductivity were measured on suspensions, 32 elements measured by ICP-OES on HNO3/HCl digests, and microplastics counted microscopically after Fenton digestion and density separation. Surface water was from wetland ponds and stormwater drains, with pH, EC measured in-situ. Filtered acidified water subsamples used to measure nitrate + nitrite and dissolved phosphate spectrophotometrically and 26 elements using ICP-OES. Reported data include metadata and are for 231 sediment/soil samples and 172 water samples, including sampling strata categories and UTM and Longitude-Latitude coordinates. Elemental concentrations have been censored based on blank subtraction and calculated lower detection limits, with censored data presented with missing value codes.
© 2022 The Author(s).

Entities:  

Keywords:  Contamination; Nutrients; Pollution; Stormwater; Trace elements; Wetlands

Year:  2022        PMID: 35242948      PMCID: PMC8885578          DOI: 10.1016/j.dib.2022.107970

Source DB:  PubMed          Journal:  Data Brief        ISSN: 2352-3409


Specifications Table

Value of the Data

The data reported provide useful information to characterize the current state of an important nature reserve in metropolitan Perth, Western Australia, which represents (i) the largest minimally disturbed alluvial flat in the coastal part of the river catchment; (ii) the location of a threatened ecological community of temperate saltmarsh vegetation. These data can benefit managers of this and analogous sites in that they characterize the ecological suitability and inform extent and risk of contamination. The data also represent useful comparative data for researchers. The data are in suitable form to allow comparisons between sub-environments, examining potential source-sink-effects, assessment of relationships between variables, and spatial analyses.

Data Description

The location of the study site is shown in Figure S1 in the Supplementary Information, with the locations of sediment and soil samples presented in Figure S2(a). The data files accessible on Mendeley Data (see Specifications Table) are designed to be self-contained records. The two files (for sediment and soil data, and for surface water data) are Excel workbooks each with five sheets. The first sheet in each workbook contains a data table with identifying, categorical, spatial, and measured (numeric) variables in columns with observations (samples) in rows below a single header row with column names, suitable for importing into software such as R [6]. The remaining four sheets in each workbook contain the metadata: (1) a thorough description of the sampling site and procedures; (2) a description of each sheet in the workbook; (3) an explanation of the columns in the data table including a description of each variable, data type, units of measurement, and lower detection limit where relevant; (4) an explanation of the codes in each categorical variable and the missing value code. Summary statistics for sediment properties and composition based on the data hosted at Mendeley are presented in Table 1, Table 2, Table 3, and Table 4, and show high variability in some parameters across the Ashfield Flats Reserve site. Based on relative standard deviations and relative ranges of values, the greatest variability in sediment/soil properties is shown by microplastics, manganese, zinc, lead, sulfur, calcium, and phosphorus. The least variability is shown by pH, chromium, and aluminium.
Table 1

Summary of descriptive statistics for pH, EC and major elements in sediments and soils across all sampling years (2019-2021) at Ashfield Flats Reserve.

ECMajor elements (mg/kg)
StatisticpH(mS/cm)AlCaFeKMgNaPS
Mean5.979.393026936014149924943932117196345547
SD0.8819.81303046992058213052362111937209337
Minimum3.160.018884701562591066126230
Lower quartile5.502.06204561487329751432235040272991575
Median6.006.413253922453868927213814104974572981
Upper quartile6.5512.44048444404787036265407151506415159
Maximum8.36280545174846013548852652074595761702076633
N221221231231231231231231231231
Missinga101000000000

‘Missing’ for pH and EC refers to samples for which measurement was omitted or incorrect.

Table 2

Summary of descriptive statistics for potential pollutant elements in sediments and soils across all sampling years (2019-2021) at Ashfield Flats Reserve.

Potential pollutant elements (mg/kg)
StatisticAsCdCoCrCuMnMoNiPbVZn
mean8.290.2114.6750.21241612.7420.058.564.3530
Sd8.500.2413.0420.61243662.117.990.224.41134
Minimum0.400.021.801.82.06.00.102.03.32.311
Lower quartile3.440.088.0033.931.861.91.2014.626.150.4115
Median6.200.1212.0055.585.583.02.0020.040.071.8248
Upper quartile9.000.231666.01851243.5526.058.581.0411
Maximum62.01.6011084.01008350313.050.08311187556
N219158231231224231231225231231227
Missinga1273007006004

‘Missing’ refers to concentrations below the detection limit which were removed from the data.

Table 3

Summary of descriptive statistics for trace elements in sediments and soils across all sampling years (2019-2021) at Ashfield Flats Reserve.

Trace elements (mg/kg)
StatisticBaCeGdLaLiNdSrThY
Mean59.693.36.846.227.635.759.913.521.7
Sd29.962.03.628.914.621.849.26.515.1
Minimum4.62.20.21.20.50.82.30.40.4
Lower quartile38.041.54.022.115.917.029.09.29.5
Median57.086.96.742.030.035.052.014.920.0
Upper quartile77.0136.39.066.338.149.573.018.030.5
Maximum19127118.012654.798.051226.967.0
N231231226231231231231229231
Missinga005000020

‘Missing’ refers to concentrations below the detection limit which were removed from the data.

Table 4

Summary of descriptive statistics for microplastics in sediments and soils across sampling years 2019 and 2021 (not 2020) at Ashfield Flats Reserve.

Microplastics (particle counts/kg)
StatisticFragmentsFibresOtherMicrobeadsTotal
Mean263719921114894944
Sd7727324440215468153
Minimum00000
Lower quartile0000500
Median493997002500
Upper quartile15002500005125
Maximum59113229082002850059613
N15615615665156
Missinga000910

‘Missing’ refers to blank-corrected microplastic counts ≤ 0.

Summary of descriptive statistics for pH, EC and major elements in sediments and soils across all sampling years (2019-2021) at Ashfield Flats Reserve. ‘Missing’ for pH and EC refers to samples for which measurement was omitted or incorrect. Summary of descriptive statistics for potential pollutant elements in sediments and soils across all sampling years (2019-2021) at Ashfield Flats Reserve. ‘Missing’ refers to concentrations below the detection limit which were removed from the data. Summary of descriptive statistics for trace elements in sediments and soils across all sampling years (2019-2021) at Ashfield Flats Reserve. ‘Missing’ refers to concentrations below the detection limit which were removed from the data. Summary of descriptive statistics for microplastics in sediments and soils across sampling years 2019 and 2021 (not 2020) at Ashfield Flats Reserve. ‘Missing’ refers to blank-corrected microplastic counts ≤ 0. Few sediment/soil quality variables were normally distributed. Distributions of numeric variables were most commonly positively skewed, with some variables able to be normalized by log10- or power-transformation (Table 5). The remainder of variables did not have normal distributions even when transformed using log10- or power functions. Similar distribution properties were observed when the data were analysed separately by year (Tables S2-S4, Supplementary Information).
Table 5

Distribution statistics for sediment/soil variables across the whole dataset. W is Shapiro-Wilk statistic; p(W) is probability that distribution is normal (H0; asterisked p(W) means H0 can not be rejected); ‘Power term’ is value to which variable is raised estimated using the Box-Cox method; ‘Best transformation’ is first for which H0 for the Shapiro-Wilk test cannot be rejected (shaded cells), in the order Untransformed > log10 > Power (– means neither log10 nor power transformation yields a normally distributed variable). D is Hartigan dip-test statistic; p(D) is probability that distribution is unimodal (Haltern.), so asterisked values indicate multi-modality.

Untransformed
log10-transformed
Power-transformed
Multimodality
VariableWp(W)Wp(W)Wp(W)Power termBest transf.Dp(D)
Ph0.9920.255*0.964<0.0010.9940.588*1.442none0.0150.991
EC0.283<0.0010.931<0.0010.964<0.0010.1960.0210.807
MP_fraga0.476<0.0010.9570.0060.9580.0070.0130.0650.007*
MP_fibrea0.657<0.0010.817<0.0010.950<0.0010.2310.0650.001*
MP_othera0.8690.0210.8010.0020.8990.064*0.524power0.1450.002*
microbeadsa0.7430.0020.9430.490*0.9420.489*-0.017log0.1150.114
MP_totala0.588<0.0010.9740.0110.9830.088*0.082power0.0410.106
Al0.961<0.0010.812<0.0010.965<0.0011.1270.0170.966
As0.684<0.0010.9870.0490.9880.061*0.041power0.0300.193
Ba0.960<0.0010.940<0.0010.9940.427*0.533power0.0240.521
Ca0.489<0.0010.9800.0020.9940.527*-0.208power0.0140.994
Cd0.644<0.0010.9880.186*0.9900.314*-0.071log0.0150.997
Ce0.959<0.0010.902<0.0010.9820.0050.5170.0200.817
Co0.633<0.0010.972<0.0010.972<0.001-0.0300.0230.550
Cr0.942<0.0010.766<0.0010.953<0.0011.2590.0190.836
Cu0.778<0.0010.972<0.0010.9770.0010.1210.0190.886
Fe0.868<0.0010.825<0.0010.932<0.0010.5530.0130.996
Gd0.9790.0020.914<0.0010.9910.197*0.627power0.0260.334
K0.967<0.0010.820<0.0010.963<0.0010.8510.0240.456
La0.964<0.0010.905<0.0010.9870.0320.5400.0170.944
Li0.957<0.0010.799<0.0010.952<0.0010.8990.0240.496
Mg0.896<0.0010.879<0.0010.971<0.0010.5430.0270.306
Mn0.287<0.0010.901<0.0010.924<0.001-0.1700.0120.996
Mo0.845<0.0010.965<0.0010.9890.083*0.235power0.0470.001*
Na0.771<0.0010.881<0.0010.971<0.0010.3620.0370.025*
Nd0.970<0.0010.882<0.0010.9830.0060.5970.0230.604
Ni0.9810.0040.893<0.0010.9810.0040.9500.0310.122
P0.583<0.0010.961<0.0010.963<0.0010.0490.0120.996
Pb0.394<0.0010.947<0.0010.951<0.001-0.0670.0190.862
S0.475<0.0010.9830.0060.9870.038-0.0840.0260.358
Sr0.713<0.0010.967<0.0010.9850.0130.2170.0210.745
Th0.965<0.0010.788<0.0010.966<0.0011.0130.0230.584
V0.913<0.0010.723<0.0010.943<0.0011.4710.0200.818
Y0.947<0.0010.917<0.0010.9860.0270.4600.0210.763
Zn0.402<0.0010.958<0.0010.958<0.001-0.0020.0280.253

MP_frag = microplastic fragments; MP_fibre = microplastic fibres; MP_other = microplastics other than fragments, fibres, or beads; microbeads = microplastic spheroids; MP_total = total microplastic particles.

Distribution statistics for sediment/soil variables across the whole dataset. W is Shapiro-Wilk statistic; p(W) is probability that distribution is normal (H0; asterisked p(W) means H0 can not be rejected); ‘Power term’ is value to which variable is raised estimated using the Box-Cox method; ‘Best transformation’ is first for which H0 for the Shapiro-Wilk test cannot be rejected (shaded cells), in the order Untransformed > log10 > Power (– means neither log10 nor power transformation yields a normally distributed variable). D is Hartigan dip-test statistic; p(D) is probability that distribution is unimodal (Haltern.), so asterisked values indicate multi-modality. MP_frag = microplastic fragments; MP_fibre = microplastic fibres; MP_other = microplastics other than fragments, fibres, or beads; microbeads = microplastic spheroids; MP_total = total microplastic particles. The locations of surface water samples presented in Figure S2(b). Few surface water quality variables were normally distributed. As with sediment data, distributions of numeric variables were most commonly positively skewed, with some variables able to be normalized by log10- or power-transformation (Table 9). The remainder of water quality variables did not have normal distributions even when transformed using log10- or power functions, which may be in part related to the non-unimodality of their distributions (Table 9 and Figure S3, Supp. Material). Similar distribution properties were observed when the water quality data were analysed separately by year (Tables S5-S7, Supplementary Information).
Table 9

Distribution statistics for water variables across all sampling years (2019-2021). W is Shapiro-Wilk statistic; p(W) is probability that distribution is normal (H0; asterisked p(W) means H0 can not be rejected); ‘Power term’ is value to which variable is raised estimated using the Box-Cox method; ‘Best transformation’ is first for which H0 for the Shapiro-Wilk test cannot be rejected, in the order Untransformed > log10 > Power (– means neither log10 nor power transformation yields a normally distributed variable). D is Hartigan dip-test statistic; p(D) is probability that distribution is unimodal (Haltern.), so asterisked values indicate multi-modality.

Untransformed
log10-transformed
Power-transformed
Multimodality
VariableWp(W)Wp(W)Wp(W)Power termBest transf.Dp(D)
pH0.929<0.0010.850<0.0010.965<0.0012.5360.0180.990
EC0.725<0.0010.933<0.0010.938<0.0010.0850.0240.731
NOx_N0.733<0.0010.943<0.0010.942<0.0010.0200.0370.457
PO4_P0.530<0.0010.9640.0150.9640.0150.0080.0400.382
Al0.632<0.0010.9730.0260.9860.308*-0.196power0.0410.204
As0.771<0.0010.9580.0050.9620.010-0.1510.0700.002*
B0.821<0.0010.893<0.0010.893<0.001-0.0110.0510.005*
Ba0.932<0.0010.9800.0140.9850.073*0.227power0.0320.253
Ca0.723<0.0010.898<0.0010.912<0.001-0.1980.064<0.001*
Co0.505<0.0010.739<0.0010.856<0.001-1.1120.0930.008*
Cr0.898<0.0010.856<0.0010.892<0.0010.6530.090<0.001*
Cu0.701<0.0010.8550.0130.9240.175*-0.889power0.0910.257
Fe0.275<0.0010.939<0.0010.9750.007-0.2260.0160.994
K0.779<0.0010.911<0.0010.912<0.001-0.0120.059<0.001*
Li0.500<0.0010.900<0.0010.901<0.001-0.2530.0650.001*
Mg0.752<0.0010.920<0.0010.918<0.0010.0560.061<0.001*
Mn0.557<0.0010.965<0.0010.9760.0050.1350.0350.141
Mo0.808<0.0010.9600.0030.9700.019-0.1930.0370.417
Na0.750<0.0010.914<0.0010.909<0.0010.0810.075<0.001*
Ni0.527<0.0010.8000.0090.9520.667*-0.984power0.0910.588
P0.628<0.0010.9920.520*0.9920.526*0.011log0.0210.939
S0.658<0.0010.948<0.0010.959<0.0010.1190.0470.008*
Si0.854<0.0010.947<0.0010.960<0.0010.2120.0330.222
Sr0.687<0.0010.910<0.0010.910<0.0010.0000.067<0.001*
V0.894<0.0010.949<0.0010.949<0.0010.1720.0440.034*
Zn0.293<0.0010.607<0.0010.931<0.001-0.7130.0300.466
La0.899<0.0010.922<0.0010.9310.0010.4170.0750.004*
Gd0.9560.733*0.9580.7590.9580.761-0.279none0.0970.529
The summary statistics for water composition and properties (Table 6, Table 7, and Table 8) based on the Mendeley-hosted dataset also show high variability in several parameters at Ashfield Flats Reserve. The greatest variability based on relative standard deviations and relative ranges of values is shown by Fe, Zn, S, P, and FRP; in contrast, lower variability is shown by pH, a range of trace elements, and Si.
Table 6

Summary of descriptive statistics for pH, EC, and dissolved major ions/elements in 0.45 µm-filtered water at Ashfield Flats Reserve across all sampling years (2019-2021).

StatisticpHEC (µS/cm)Concentrations on element mass basis (mg/L)
CaKMgNaNOxaPFRPbSSi
Mean7.181350715210839327310.2740.2130.1452103.79
s.d.0.671832816112750333520.3890.3220.2723082.38
Minimum3.46319.40.761.123.700.0010.0020.0010.430.32
Lower quartile6.8891245.410.617.91080.0100.0340.01113.32.32
Median7.12334053.826.787.65910.0500.0900.06457.32.67
Upper quartile7.492560028323684162820.4980.2260.1553415.59
Maximum8.7312230012476923323193441.702.051.67266115.7
N1691691691691691699416088167169
Missingc33333378128453

NOx = nitrate + nitrite as mgN/L;

FRP = filterable reactive phosphate as mgP/L

‘Missing’ for pH and EC refers to samples for which measurement was omitted or incorrect, and for other variables refers to concentrations below the detection limit which were removed from the data.

Table 7

Summary of descriptive statistics for dissolved potential pollutant elements in 0.45 µm-filtered water at Ashfield Flats Reserve across all sampling years (2019-2021).

Element concentrations (mg/L)
StatisticAlAsCoCrCuMnMoNiVZn
Mean0.0710.0140.0260.00480.00670.2930.00210.00910.01530.248
SD0.0900.0130.0360.00330.00920.3790.00130.01050.00950.848
Minimum0.0090.00220.00710.00040.00190.00640.00080.00340.00370.005
Lower quartile0.0210.00450.00810.00140.00250.0900.00120.00500.00690.008
Median0.0400.0100.00930.00530.00350.1930.00160.00570.0110.010
Upper quartile0.0700.0180.0490.00720.00610.3850.00240.00820.0210.013
Maximum0.6160.0580.1900.0100.0502.990.00520.0400.0414.09
N1078831107521699211138139
Missinga6584141651203801613433

‘Missing’ refers to concentrations below the detection limit which were removed from the data.

Table 8

Summary of descriptive statistics for dissolved trace and rare-earth elements in 0.45 µm-filtered water at Ashfield Flats Reserve across all sampling years (2019-2021).

Element concentrations (mg/L)
StatisticBBaFeGdLaLiNdRbSr
Mean1.030.0582.730.00220.00270.05230.00640.1092.12
s.d.1.040.0328.600.00040.00160.05860.00240.1302.65
Minimum0.0310.00860.050.00160.00030.01300.00210.00080.026
Lower quartile0.190.0330.210.00190.00120.01840.00470.01580.226
Median0.340.0480.470.00220.00230.04540.00590.03250.55
Upper quartile1.940.0801.910.00250.00440.06740.00810.2214.31
Maximum5.280.17297.90.00290.00550.5600.01260.94022.1
N164168153176811069169167
Missinga84191551046210335

‘Missing’ refers to concentrations below the detection limit which were removed from the data.

Summary of descriptive statistics for pH, EC, and dissolved major ions/elements in 0.45 µm-filtered water at Ashfield Flats Reserve across all sampling years (2019-2021). NOx = nitrate + nitrite as mgN/L; FRP = filterable reactive phosphate as mgP/L ‘Missing’ for pH and EC refers to samples for which measurement was omitted or incorrect, and for other variables refers to concentrations below the detection limit which were removed from the data. Summary of descriptive statistics for dissolved potential pollutant elements in 0.45 µm-filtered water at Ashfield Flats Reserve across all sampling years (2019-2021). ‘Missing’ refers to concentrations below the detection limit which were removed from the data. Summary of descriptive statistics for dissolved trace and rare-earth elements in 0.45 µm-filtered water at Ashfield Flats Reserve across all sampling years (2019-2021). ‘Missing’ refers to concentrations below the detection limit which were removed from the data. Distribution statistics for water variables across all sampling years (2019-2021). W is Shapiro-Wilk statistic; p(W) is probability that distribution is normal (H0; asterisked p(W) means H0 can not be rejected); ‘Power term’ is value to which variable is raised estimated using the Box-Cox method; ‘Best transformation’ is first for which H0 for the Shapiro-Wilk test cannot be rejected, in the order Untransformed > log10 > Power (– means neither log10 nor power transformation yields a normally distributed variable). D is Hartigan dip-test statistic; p(D) is probability that distribution is unimodal (Haltern.), so asterisked values indicate multi-modality.

Experimental Design, Materials and Methods

Ashfield Flats Reserve (approx. 40 ha; Figure S1 in the Supplementary Information) is listed as a Western Australian Bush Forever Site (No. 214) [7] and fringes the Swan-Canning Estuary. It is also listed in the Directory of Important Wetlands in Australia [8]. It is the largest remaining salt marsh in the Swan-Canning Estuary, but is impacted by altered hydrology, several stormwater drains, and poor water quality from historical groundwater contamination. Two main drains that flow through Ashfield Flats Reserve are Chapman Street drain which has a 129 hectare catchment, and Kitchener Street drain has a 9 hectare catchment. Both drains flow directly into, and affect the water quality of, the Swan River. While groundwater comprises 45% of their annual discharge, they have little interaction directly with the wetland's groundwater [9]. A third drain, the Woolcock Court drain, with a catchment area of 17 ha, discharges perennially and delivers an estimated 56 ML/y of water into the western area of the wetland. The reserve therefore conducts and potentially receives a large proportion of the Ashfield and Bassendean storm water from urban residential, transport, and industrial land uses, including a large containment cell for landfill storage of pyritic waste from historical fertiliser production [10]. The hydrology and quality of groundwater of the area has likely been altered due to groundwater use and contamination up-hydraulic gradient in the catchment. The site has a history of agriculture, with sheep and cattle farming across much of the area in the early 1800s, and a dairy farm occupying some of the area up to the 1950s [11]. Potential acid sulfate soils are known to occur naturally in the estuarine soil deposits present across Ashfield Flats Reserve [9]. Sampling was conducted on three occasions approximately 1 year apart, on 15 March 2019, 13 March 2020, and 5 March 2021. Sampling design was systematic within pre-identified strata, achieved with transects across anticipated contamination gradients, or regular or irregular grids within strata, depending on sampling year (Figure S2, Supplementary Information). Soils and wetland sediments were sampled in cylindrical cores from 0-5 cm depth using a trowel. Triplicate cores at each location were bulked to achieve a sample mass of ca. 500 g, and stored at ca. 4°C in zip-lock plastic bags prior to transport back to the laboratory. All bulk soil and sediment samples were air dried at 40°C in a convection dryer prior to chemical analyses. Water sampling protocols followed Clesceri et al [3]. Acid-washed plastic bottles were used to sample water from wetland ponds and drains at approximately mid-depth (and mid-stream for the drain samples). A portion (ca. 50 mL) of the water sampled was immediately removed, filtered through a 0.45 µm membrane into a separate clean plastic bottle, and acidified with 1∕100 volume of 5 mol/L HNO3. The acidified samples were stored in insulated containers prior to transporting to the laboratory within 4 hours and were subsequently stored at 4°C until analysis. Powder-free nitrile gloves were worn at all times while handling samples.

Ethics Statements

No ethical guidelines or consents were relevant for the research reported on in this article.

CRediT authorship contribution statement

Andrew W. Rate: Conceptualization, Data curation, Formal analysis, Investigation, Methodology, Project administration, Supervision, Writing – original draft, Writing – review & editing. Gavan S. McGrath: Conceptualization, Funding acquisition, Investigation, Methodology, Writing – review & editing.

Declaration of Competing Interest

The authors declare that they have no known competing financial interests or personal relationships that could have appeared to influence the work reported in this paper.
SubjectEnvironmental science
Specific subject areaEnvironmental geochemistry of urban environments
Type of dataTableMap
How the data were acquiredSamples were surface sediments (0-10cm, composites of 3 cores), soils (profile sampling to ≤100cm), and surface water grab samples. pH and EC of water and sediment suspensions by potentiometry [1]. Elemental content of filtered then acidified water, and conc. HNO3/HCl digests of sediments [2], used ICP-OES (Perkin-Elmer Optima 7300DV). Dissolved phosphate [3] and nitrate + nitrite in water [4] by spectrophotometry (BMG FluoStar Optima). Microplastics in sediment by Fenton digestion [5], density separation in 40% KI solution, and counting using optical microscopy. Data analysis in R [6] and packages.
Data formatRaw
Description of data collectionSediments (manual cores) and surface water (grab samples) were collected from wetland ponds and stormwater drains on 15/03/2019, 13/03/2020, 05/03/2021. Sediments were air dried at 40°C before analysis; water samples were acidified and filtered (0.45 µm membrane) for analyses other than pH and EC. Analyses were excluded if concentration was less than method blank or lower limit of detection (Table S1, Supplementary Information).
Data source locationInstitution: The University of Western Australia:City/Town/Region: Crawley, Western Australia 6009Country: AustraliaLatitude and longitude (and GPS coordinates, if possible) for collected samples/data:min maxLongitude (°E) 115.94128 115.94937 (WGS84)Latitude (°S) -31.92018 -31.91476 (WGS84)UTM Zone 50J (EPSG 32750) GPS coordinates (m) min maxEasting 399908 400668 (WGS84)Northing 6467925 6468531 (WGS84)
Data accessibilitySediment data Repository: Mendeley Datadoi:10.17632/d7m3746byk.1Link: https://data.mendeley.com/datasets/d7m3746byk/1Water data: Repository: Mendeley Datadoi: 10.17632/vphzgjshgm.1Link: https://data.mendeley.com/datasets/vphzgjshgm/1Supplement Repository: Mendeley Datadoi: 10.17632/sz7rwg5p4n.1Link: https://data.mendeley.com/datasets/sz7rwg5p4n/1
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