PROOF Correction on Atom Indonesia Journal
Article Title : Sedimentation Rate in Sayung Coast, Demak, Central Java Using Unsupported
210Pb Isotope
Line
Number Original Text Correction Note / Change
8 W.A. Gemilang1*, U.J. Wisha1, T.
Solihuddin2, and A. Arman3
W.A. Gemilang1*, U.J. Wisha1, T.
Solihuddin2, A. Arman3, K.
Ondara1
Actually, the author consists of five persons, I apologize not to add the last author in the article metadata. I hope that this change can be accepted by AIJ editor
10 Gedung Mina Bahari I Lt 5, Jl. Medan Merdeka Timur No. 16, Jakarta Pusat, DKI Jakarta 20220, Indonesia
Jl. Raya Padang-Painan KM. 16, Bungus Teluk Kabung, Kota Padang, Sumatera Barat 25245, Indonesia
The mailing address is not correct
12 Gedung Mina Bahari I Lt 5, Jl. Medan Merdeka Timur No. 16, Jakarta Pusat, DKI Jakarta 20220, Indonesia
Komplek Bina Samudera, Jl. Pasir Putih II Lt 4, Ancol Timur, Jakarta Utara, DKI Jakarta 14430,
Indonesia
The mailing address is not correct
18 efforts to reduce abrasion were temporarily succeeded
efforts to reduce abrasion temporarily succeeded
The last line of abstract should be slightly improved 26 which shifts the hydrodynamic
patterns
which shift the hydrodynamic patterns
28 Three Sub-Districts are experiencing coastal erosion
Three sub-districts are undergoing coastal erosion
46 the tide flooding or inundation (rob) the tidal flooding or inundation (rob)
49 Demak experienced rapid coastal erosion
Demak run into rapid coastal erosion
81-82 increase of land that was previously eroded by erosion
increase of land that was previously eroded
115-117 The study area is positioned in the lowland coast unit, where broadly utilized as fish ponds and mangrove areas
The study area is positioned in the lowland coast unit, whereby it is broadly utilized as fish ponds and mangrove areas
118 The Demak area is tectonically controlled by
Demak region is tectonically controlled by
153-154 accumulation rates in Sayung, Demak. The tidal and currents were
accumulation rates in Sayung coast. In addition, tidal and sea
recorded using the Acoustic Doppler Current Profiler (ADCP).
current data were recorded using the Acoustic Doppler Current Profiler (ADCP).
208-209 The ADCP was deployed on March 4th, 2016 15:00 pm until March 22th, 2016 12:00 am (18 days)
The ADCP was deployed at March 4th, 2016 15:00 pm until March 22th, 2016 12:00 am (18 days) 211 Current and tidal data Sea current and tidal data 233-235 flexible mesh (fm) was employed to
figure out the tidal current pattern in the form of two-dimensional model
flexible mesh (fm) was developed to figure the tidal current pattern out in the form of two-dimensional model
236 sourced from PUSHIDROSAL retrieved from PUSHIDROSAL 241-243 Besides, the tidal forecast data were
resulted from ERGtide software simulation in the form of time series data
Moreover, the tidal forecast data were extracted from ERGtide software simulation in the form of time series data
272 While, the tidal range was 0.6 m Furthermore, the tidal range was 0.6 m
277-279 Moreover, station ISTD-02 was not covered by water during the neap tidal condition, so that the simulation was impossible to be performed.
In fact, station ISTD-02 was not covered by water during ebb tides so that the simulation was impossible to be performed.
295 Whilst, at the spring low tidal condition
In contrast, at the spring low tidal condition
308 Whilst, the sediment will be relatively deposited
On the other hand, the sediment will be relatively deposited 357 6-10 cm, the accumulation ages could
not be detected
6-10 cm. In addition, the accumulation ages could not be detected
360-361 The sediment accumulation rates show that on the top layer of sediment
On the top layer of sediment
363 The highest accumulation rate The highest sedimentation rate 388-389 resulting in the massive sedimentation
sourced from land.
resulting in massive sedimentation sourced from land.
405 the rates were dramatically elevated the rates dramatically elevated 424 Based on the results above In regard to the results above
increase since year 2000 which correlated with the changes of mangrove area during 2004 - 2013
increase since year 2000 in accordance with the changes of mangrove area during 2004 - 2013 476 surf wave with the height more than 4 surf wave with the inundation
meters more than 4 meters (overtopping)
486 wave-driven currents. wave-driven currents [1]. missing one citation 488 identified in 2016. At ISTD-01 station identified in 2016 specifically at
ISTD-01 station 490 ISTD-02 station, the sediment
accumulation rate
ISTD-02 station, the sedimentation rate
494-495 where the current pattern is dominant influencing the area.
where the current pattern has a dominant role in the transport mechanism.
500-502 The development of either breakwater or the other coastal structures has a significant role in inducing sediment transport along the coast [1].
The construction of either breakwater or the other coastal structures has a significant role in altering sediment behavior along the coast [1].
507-517 Based on 210Pb isotope analysis, the average of sedimentary rate reached 0.06 cm/year in Surodadi (SRD-01 and SRD-02) and 0.14-0.15 cm/year in Timbulsloko (ISTD-01 and ISTD- 02). The enhancement of mangrove forest area in 2013 up to 2016 resulted in the higher sediment accumulation rate (ranging from 0.20 – 0.43 cm/year). The implementation of HE since 2013 succeeded to raise the mangrove cultivation areas that related to the increase of sediment accumulation rate in the Sayung Coast.
Based on 210Pb isotope analysis, the average of sedimentation rate is higher in Timbusloko compared to Surodadi coast. The increase of mangrove forest area in 2013 up to 2016 had a significant role in increasing sedimentation rate. The implementation of HE since 2013 had been succeeded to raise the mangrove cultivation areas, as a result, the sedimentation rate in the Sayung Coast increased instead.
I opine that in the conclusion, it does not need to mention any results (in number) that have been mentioned in the section before.
525-526 The difference in the average of sediment accumulation rate
The difference in the average of sedimentation rate
528 The increase of sedimentary rate The increase of sedimentation rate
Please return to Atom Indonesia Editorial Office via supplementary file in OJS application.
Date: 11 April 2020
