Volume 2, No. 6 June
2023 - (413-423)![]()
p-ISSN 2980-4868 | e-ISSN 2980-4841
https://ajesh.ph/index.php/gp
SUITABILITY OF SEAWEED
CULTIVATION LAND POST EARTHQUAKE AND TSUNAMI IN BANAWA SELATAN DISTRICT,
DONGGALA DISTRICT
Zakira Raihani
Ya'la
Aquaculture Study Program, Indonesia
Emails: zakirahraihaniyala@gmail.com
ABSTRACT:
An earthquake measuring 7.7 on the Richter scale
(SR) shook Donggala, Central Sulawesi (Central
Sulawesi) causing disruption to the supply of electricity to the people in the
region. The incident mentioned above caused thousands of buildings to collapse
including power plants which disrupted lighting. The impact of the tsunami hit Parigi Regency and Palu City
causing the economy to be totally paralyzed, especially the people who live in
coastal areas. The specific objective of the research was to examine the
physical and chemical suitability of the waters of the waters of the grass
cultivation site after the earthquake and tsunami in Donggala
District. Based on the results overlay then the land area used for
(appropriate, less suitable and not suitable) cultivation activities is
obtained Eucheuma cottonii or
almost balanced cultivation area. In developing a cultivation business, it is
necessary to consider the area of utilization, such as the flow
of shipping traffic, the distance between ropes long line and for the
protection of other ecosystems. Based on the percentage of land suitability
covering 33.53% suitable areas, 44.26% less suitable and 19.84% not suitable.
This shows that the condition of the seaweed cultivation area is less favorable
in terms of water quality. Water quality parameters include physical, chemical
and biological aspects. These three parameters are interrelated with one
another. So that when one of the parameter elements is disturbed, it will
automatically interfere with other elements.
Keywords: Physical,
chemical, land suitability.
Article History
Received : 20 May 2023
Revised : 01 June 2023
Accepted : 14 June 2023
DOI :
10.xxxxx
INTRODUCTION
Seaweed
(sea weed) is one of the fisheries commodities that can be used to encourage
people's economic growth (Chen et al., 2020). Seaweed cultivation does not require high technology, investment
tends to be low, absorbs quite a lot of labor and generates relatively large
profits. The development of these businesses is expected to reduce the
unemployment rate (pro job), increase people's income (pro growth) and in turn
can reduce poverty (pro poor). Seaweed is one of the leading commodities that
has a prospective market. The world's demand is quite high causing the
production of products originating from nature to be insufficient, so
cultivation efforts must be made. This target is carried out by developing
15,000 hectares of cultivated land by 2009 with a production target of 0.4
million tonnes for Gracilaria
sp and 1.5 million wet tonnes
for Eucheuma sp (Yala et al., 2022).
Total expected
production of 1.9 million tons or equivalent to 186,332 dry tons, while exports
are expected to be $ 111,501,000. The reality on the ground shows that seaweed
cultivation activities have absorbed a lot of manpower, helped poverty
alleviation efforts and in turn opened up opportunities for the community's
economic growth. At least, the margin for this type of seaweed cultivation
business Eucheuma sp ranges
from IDR 20,500,000/KK/0.5 Ha/Year mean while Gracilaria
sp ranges from IDR 24,700,000/KK/Ha/Year (Eyayu et al., 2023). This margin could increase if it is accompanied by an increase in
production per unit area, area expansion, quality improvement and potential for
increasing world demand (Popp et al., 2013).
The
Province of Central Sulawesi, with a coast length of around 4,013 km covering Tomini Bay, Tolo Bay and Makassar
Strait, has a potential area for developing seaweed commodities of around
65,426 ha. The dominant species cultivated is Eucheuma
cottonii carrageenan phyte
producers, while agarophyte producers such as Gracilaria verrucosa cultivated
in ponds are being developed. In 2009 the development of seaweed cultivation in
Central Sulawesi was predicted to reach an area of 7,851.12 Ha,
in 2010 it could reach an area of 11,776.68 Ha, and in 2011 it
could reach an area of 15,702.24 Ha (Sapitri & Cokrowati, 2016).
RESEARCH METHODS
1. Land Suitability Analysis
To determine the land
suitability of a water area in the optimal and sustainable development of
seaweed cultivation which guarantees coastal sustainability, analytical methods
are used including (Mudeng et al., 2015).
a.
Spatial Analysis
In conducting spatial analysis there are several steps that must be
carried out, namely the preparation of a spatial database and the overlay
technique (overlay).
1)
Database Compilation
The preparation of a spatial database is intended to create digital
thematic maps starting with a base map, data collection (data compilation) up
to the final stage. Overlaying. In this study the types of data collected
included ecological waters such as temperature, salinity, waves, tides,
currents, brightness, dissolved oxygen, pH, CO2, nitrate, phosphate, TSS, TDS,
protection, aquatic substrates and biological aspects. Based on these data, contours
will be made for each criterion with assistance Extension Gird Conturso that the next contour is formed conver to polygon which generates the theme itself. The
result of a polygon or coverage (layer) is used for processing overlay.
2)
Patching Process
To determine the mapping of an area that is suitable and not suitable
for the development of seaweed cultivation in the research area, an overlapping
operation is carried out (overlay) of each theme used as a criterion, using Arc
ArcView 3.2. Before the overlapping operation was carried out, each theme was
assessed for its level of influence on determining land suitability. Giving
value to each of these themes using weighting (weighting). Each theme is
divided into several classes (which are adjusted to the conditions of the
research area) given a score ranging from classes that have an effect on to
classes that have no effect. Each class will get a final score which is the
result of multiplying the class score by the weight of the theme in which the
class is located. Determination of criteria, giving weights and scores is
determined based on literature studies and competent justification in the field
of fisheries. The process of giving weights and scores as above is carried out
through an index approach overlay model to obtain the sequence of land
suitability classes. This model requires each coverage weighted and each class
in one coverage rated. The multiplication result between the weight and the
score received by each coverage is adjusted based on the level of importance to
the determination of land suitability for seaweed cultivation.
Before the overlapping operation stage is carried out, a table of land
suitability classes for seaweed cultivation is first made which contains
information on criteria, then scoring, weighting and to determine the
suitability class are carried out.
The final result of GIS analysis through index approach overlay The
model is to obtain a ranking or sequence of land suitability classes for
seaweed cultivation. Land suitability classes are distinguished at the class
level and are defined as follows:
Class S1: Not suitable,
namely land or areas that are not suitable for seaweed cultivation because they
have severe limiting factors that are permanent.
Class S2: Not suitable,
namely if the land or area has rather serious limiting factors or influences
the productivity of seaweed cultivation. In its management, additional
technological input is needed from the treatment level.
Class S3: Suitable,
namely if the land or area is very suitable for seaweed cultivation without
significant limiting factors or has minor limiting factors and will not
significantly reduce productivity.
RESULTS AND DISCUSSION
Figure 1. Brightness Map

Sunlight
is necessary for the photosynthesis process of seaweed. The amount of sunlight
that enters the water is closely related to the brightness of the sea water.
There are certain limits for the clarity of seawater. The brightness of the
water is up to a limit of 5 meters or the limit of sunlight can penetrate sea
water. Habitats Chlorophyceae generally closer to the
beach, more central again Phaeophyceaea, and even
deeper Rhodophyceae. According to Aslan (2020), optimal brightness is increased if it allows plants to receive
sunlight.
Brightness
in the waters of the research location ranges from 4 8 meters. These results
show that the brightness at each entry point shows appropriate results - not
appropriate. Points 1, 2, 6, 8, 9, 10, 11, 12, and 13 are included in the
appropriate criteria while those included in the less suitable criteria are at
points 3, 4, 5 and 7. Mubarak, et al (1990) said that for ideal seaweed
cultivation activities, the brightness level of the waters is >5 meters.
Figure 2. Current Velocity Map

Apart
from being protected and the condition of the substrate, the fertility of a
cultivation site is determined by the presence of currents (Kotiyaet
al., 2011). Current velocity is an important ecological factor in seaweed
cultivation where through the movement of this water it can supply nutrients,
dissolve oxygen, disperse plankton and remove silt which is much needed
supplied and distributed for seaweed growth.
The
Directorate General of Cultivation (2013) says that a good current speed for seaweed cultivation is 20-40
cm/sec. Brown (2016) says that good currents will bring nutrients to plants and the plants
will be clean because dirt and adhering deposits will be washed away by the
currents so the plants will grow well. Waves and currents facilitate the
transport of nutrients and cause the water mass to become homogeneous. This
homogeneous water mass avoids large fluctuations in temperature, salinity, pH
and dissolved oxygen. Current speed desired for cultivationE.
Cottonii between 20 -40 cm/sec. Current speed is one
of the important factors affecting the growth of seaweed, indirectly preventing
an increase in pH and a significant increase in temperature and play a role in
gas exchange in the water column (Mudeng et al., 2015).
Figure 3. Water Depth

Water
depth has a close relationship with light penetration, vertical temperature
stratification, density and oxygen and nutrient content. As the depth
increases, the penetration of light will decrease. Seaweed is abundant in the
intertidal zone and is usually found at depths of 3040 meters. In clear
tropical areas it can reach a depth of 200 m (Sumich, 1980). Furthermore Bell (1992), put forward the most members Rhodophytalive
in deep and warm waters, commonly seen when stranded on the surface. For
cultivation Gracilariasp minimum required depth of 50
cm (Yala, 2022). Depth is one of the determining factors in the process of seaweed
cultivation. The depth of the cultivation location will affect water
productivity, temperature, light penetration and nutrients for seaweed growth.
Depth also plays a role in determining the method of seaweed cultivation. Depth
is a determining factor for the location of seaweed cultivation because depth
is related to the penetration of sunlight which has an important effect on growth
(Fahrizal & Ratna, 2018). Depth at the study site ranged from 4 27 meters. The highest depth
value is at points 11 and 10 while the lowest depth is at point 3.
Picture 4. Water nitrate content

The
existence of nutrients with their composition in seawater, although very small,
is very important for ecological processes. Movement of water greatly
influences many ecological and distributional processes, especially the
circulation of nutrients and oxygen. Photosynthesis of marine plants in addition
to producing oxygen, is also for the formation of proteins, enzymes, energy
reserves, transport energy, and other molecules. The concentration of N and P
in the waters is very small even though they are needed. The average nitrate
content in seawater is 0.5 ppm and the phosphate content is lower than that.
Both of these compounds can exceed the limit in the surface area of
the water (Wiyarsih et al., 2019).
Nitrate
content is one of the criteria for the suitability of waters for seaweed cultivation,
because nitrate is one of the nutrients needed by seaweed. Nitrate content in
the waters where seaweed cultivation was obtained ranged from 0.0051-0.0058
This shows that at each point the criteria are not appropriate. In line with Rohman (2018) stated that Nitrate content which is good for seaweed growth ranges
from 0.1 0.2 mg/l. Nitrate levels below 0.1 mg/l or above 45 mg/l are
limiting factors that can result in eutrophication which can stimulate the
rapid growth of phytoplankton (Atmanisa et al., 2020).
Figure 5. Water Dissolved Oxygen
Content

Oxygen
is the single most important factor in any aquatic system. Almost all plants
and animals require oxygen for respiration. The main source of oxygen comes
from the atmosphere and the photosynthesis process of green plants. The regular
entry of fresh water and sea water into the waters together with their shallowness,
stirring and mixing by the wind, means that there is sufficient oxygen in the
water column (Sadighrad et al., 2021). Life in the water column survives if dissolved oxygen is at least 4
ppm, the rest depends on the resistance of organisms, the presence of contaminants
and water temperature (Sastrawijaya, 2021).
Dissolved
oxygen is the amount of oxygen dissolved in water. Dissolved oxygen is an
important factor in supporting the growth of organisms as well as other
factors. The results of measuring the dissolved oxygen content at each point
indicate that dissolved oxygen is included in the appropriate criteria for
seaweed cultivation where at each point it ranges from 6.7 and 7.0. This is
supported by the Zuldin (2016) who said that the dissolved oxygen content to support seaweed
cultivation is 3.0 8.0 mg/l. Furthermore Nurdin (2012)said that seaweed can grow and develop optimally in the range of
dissolved oxygen > 6.5 mg/l.
Figure 6. Water pH content
According
to Aslan (1998), the degree of acidity of water (pH) is suitable for growth Eucheuma generally ranges from 69, while the optimal is 6.5.
Meanwhile, according to Poncomulyo et al., (2006), pH is good for growth Eucheuma ranged from
7.3-8.2. According to Tuli (2020), the optimal pH for growth Gracilaria sp ranges from 6-9. Based on the results of measuring the
pH parameters of the waters at each point, the range is between 6 7. This
shows that the pH value supports the growth of seaweed. Appropriate criteria
are at points 5, 6, 7, 9, 10, 11, 13 and those that fall into unsuitable
criteria are at points 1, 2, 3, 4, 8, and 12. This is supported by Hilson (2017) who said that a good pH for seaweed cultivation ranges from 6.5
8.5.
Figure 7. Water Salinity

Salinity
of waters suitable for cultivation Eucheuma cottonii generally ranges from 28 -35. Salinity below 28
makes seaweed susceptible to disease. Eucheuma sp is an algae that is only able to tolerate changes in a
narrow range of salinity, so that salinity below 30 can result in poor growth.
Gracilaria Sp originating
from the Atlantic and East Pacific maximum growth during cultivation ranged
from 15-28, with optimal levels of 25 (Aslan, 1998). Based on the results of
salinity measurements at each point it ranges from 29 - 30 ppt
where these results indicate that the salinity content at each point is within
the appropriate criteria for seaweed cultivation. This is supported by Adipu et al (2013) that the salinity for a very suitable
location for seaweed cultivation is between 28 34 ppt.
Figure 8. Water Temperature

Even
though the water temperature does not have a lethal effect, it can inhibit the
growth of seaweed. Too large a difference in water temperature between day and
night can affect growth. This often occurs in waters that are too shallow.
Seaweed can usually grow well in areas with temperatures between 26 - 30ΊC (Afrianto & Liviawaty, 2019). Meanwhile, according to Gusrina (2013), water temperature is good for growth Eucheuma
cottonii ranges from 2633ΊC. In seaweed cultivation
(Eucheuma spinosum), the condition of reef exposure
with a sand bottom that is not mixed with silt, water clarity, high salinity,
temperature and strong currents are the necessary requirements (Neudeck et al., 2002). According to Aslan (1998), the optimal temperature for cultivation Gracilaria
sp range 20 -25 0C. Based on the results of
temperature measurements at each water point in Lalombi
Village, the range is between 28 30oC (can be seen in table 4.5). These
results indicate that the temperature at each point is at the appropriate
criteria for seaweed cultivation. This is supported by Andriano
(2016) that the good water temperature range for seaweed is 27 30oC, Asni (2015) also said that seaweed grows and develops well in waters that have a
temperature range of 26 33oC.
Figure 9. Waterland
suitability
Based
on the results overlay then the land area used for (appropriate, less suitable
and not suitable) cultivation activities is obtained Eucheuma
cottonii or almost balanced cultivation area. In
developing a cultivation business, it is necessary to consider the area of
utilization, such as the flow of shipping traffic, the distance
between rope long line and for the protection of other ecosystems.
Based
on the percentage of land suitability covering the appropriate area of
33.53%, it is not suitable 44.26% and 19.84% that do not fit.
This shows that the condition of the seaweed cultivation area is less favorable
in terms of water quality. Water quality parameters include physical, chemical
and biological aspects. These three parameters are interrelated with one
another. So that when one of the parameter elements is disturbed, it will
automatically interfere with other elements. For example, when the temperature
of the water rises, it will affect the decrease in dissolved oxygen levels in
the water. This is due, when the temperature rises will causes the respiration
process of aquatic organisms to increase resulting in a decrease in oxygen
levels in the waters.
CONCLUSION
Based
on the overlay results, the area of land used for (appropriate, less
appropriate and inappropriate) Eucheuma cottoni cultivation activities or cultivation areas is
almost balanced. In the development of aquaculture business, it is necessary to
consider the utilization area such as shipping traffic flow, distance between
long line ropes and for the protection of other ecosystems.
Adipu,
Y., Lumenta, C., & Sinjal, H. J. (2013). Kesesuaian lahan budidaya laut di
perairan Kabupaten Bolaang Mongondow Selatan, Sulawesi Utara. Jurnal
Perikanan Dan Kelautan Tropis, 9(1), 1926.
Afrianto, E., & Liviawaty, E. (2019). Potensi Mikroba Probiotik dari
Ikan Nila Mati Masal di Waduk Cirata. Jurnal Perikanan Kelautan, 10(2).
Andriano, N., Bonaccorso, P., Iachelli, V., La Rosa, M., Cannata, E.,
& Lo Nigro, L. (2016). Genetic aberrations in the DNA repair pathway among
children with Philadelphia chromosome positive leukemias. Cancer Research,
76(14_Supplement), 2428.
Aslan, A., & Autin, W. J. (1998). Holocene flood-plain soil formation
in the southern lower Mississippi Valley: implications for interpreting
alluvial paleosols. Geological Society of America Bulletin, 110(4),
433449.
Asni, A. (2015). Analisis Poduksi Rumput Laut (Kappaphycus alvarezii)
Berdasarkan Musim dan Jarak Lokasi Budidaya di Perairan Kabupaten Bantaeng. Jurnal
Akuatika Vol. VI No, 140(153), 253262.
Atmanisa, A. (2020). Analisis Kualitas Air pada Kawasan Budidaya Rumput
Laut Eucheuma Cottoni di Kabupaten Jeneponto. UNIVERSITAS NEGERI MAKASSAR.
Atmanisa, A., Mustarin, A., & Taufieq, N. A. (2020). Water Quality
Analysis In The Eucheuma Cottoni Seaweed Cultivation Area In Jeneponto
District. Jurnal Pendidikan Teknologi Pertanian, 6, 1122.
Bell, N. J. V, Burget, D., Howden, C., Wilkinson, J., & Hunt, R. H.
(1992). Appropriate acid suppression for the management of gastro-oesophageal
reflux disease. Digestion, 51(Suppl. 1), 5967.
Brown, S. L., Chaney, R. L., & Hettiarachchi, G. M. (2016). Lead in
urban soils: a real or perceived concern for urban agriculture? Journal of
Environmental Quality, 45(1), 2636.
Chen, J.-L., Hsu, K., & Chuang, C.-T. (2020). How do fishery resources
enhance the development of coastal fishing communities: Lessons learned from a
community-based sea farming project in Taiwan. Ocean & Coastal
Management, 184, 105015.
Eyayu, A., Getahun, A., & Keyombe, J. L. (2023). A review of the
production status, constraints, and opportunities in East African freshwater
capture and culture fisheries. Aquaculture International, 122.
Fahrizal, A., & Ratna, R. (2018). Analisa Proksimat Pellet Berbahan
Limbah Ikan PPI Klaligi Kota Sorong. Median: Jurnal Ilmu Ilmu Eksakta, 10(3),
3138.
Gusrina, G., & Amri, Z. (2013). Englishspeak. Com As Media For
Teaching Pronunciation Of Junior High School Students. Journal of English
Language Teaching, 2(1), 94102.
Hilson, G., & Laing, T. (2017). Gold mining, indigenous land claims
and conflict in Guyanas hinterland. Journal of Rural Studies, 50,
172187.
Mudeng, J. D., Ngangi, E. L. A., & Rompas, R. J. (2015). Identifikasi
Parameter KualitasAir untuk Kepentingan Marikultur di Kabupaten Kepulauan
Sangihe Provinsi Sulawesi Utara. E-Journal Budidaya Perairan, 3(1).
Neudeck, P. G., Okojie, R. S., & Chen, L.-Y. (2002). High-temperature
electronics-a role for wide bandgap semiconductors? Proceedings of the IEEE,
90(6), 10651076.
Nurdin, I. N. (2012). Evaluation of the Quality and Post Harvest
Handling Seaweed Eucheuma cottonii Buto n in Southeast Sulawesi Province.
Thesis Graduate Program Faculty of Agricultural Technology Universitas
.
Poncomulyo, T., Maryani, H., & Kristiani, L. (2006). Budidaya dan
pengolahan rumput laut. PT. Agromedia Pustaka. Surabaya, 89.
Popp, J., Pető, K., & Nagy, J. (2013). Pesticide productivity and
food security. A review. Agronomy for Sustainable Development, 33,
243255.
Rohman, M., & Hairudin, H. (2018). Konsep tujuan pendidikan islam
perspektif nilai-nilai sosial-kultural. Al-Tadzkiyyah: Jurnal Pendidikan
Islam, 9(1), 2135.
Sadighrad, E., Fach, B. A., Arkin, S. S., Salihoğlu, B., & Hόsrevoğlu,
Y. S. (2021). Mesoscale eddies in the Black Sea: Characteristics and kinematic
properties in a high-resolution ocean model. Journal of Marine Systems, 223,
103613.
Sapitri, A. R., & Cokrowati, N. (2016). Pertumbuhan rumput laut
Kappaphycus alvarezii hasil kultur jaringan pada jarak tanam yang berbeda. Depik,
5(1).
Sastrawijaya, M. D. (2021). The Character and Moral Values in to Kill a
Mockingbird by Harper Lee. INFERENCE: Journal of English Language Teaching,
3(1), 8187.
Sumich, J. L. (1980). Biology of marine life. NC Brown Company Publ.
Iowa.
Tuli, M. (2020). Analysis of Shortfin Scad (Decapterus macrosoma)
fisheries in Pohuwato, Gorontalo Province. PROSIDING, 10(3453).
Wiyarsih, B., Endrawati, H., & Sedjati, S. (2019). Komposisi dan
kelimpahan fitoplankton di laguna Segara Anakan, Cilacap. Buletin
Oseanografi Marina, 8(1), 18.
Yala, Z. R., Sulistiawati, D., & Tobigo, D. (2022). Multiple Biota
Cultivation (Gracilaria sp and Chanos-chanos) Development Model as a Pillar of
Milk Fish-Agar Agroindustry and its Applications. IOP Conference Series:
Earth and Environmental Science, 1075(1), 12008.
Yala, Z. R. (2022). Physical and chemical conditions of waters for seaweed
cultivation in Morowali, Central Sulawesi, Indonesia. Natural Science:
Journal of Science and Technology, 11(01), 2029.
Zuldin, W. H., Yassir, S., & Shapawi, R. (2016). Growth and
biochemical composition of Kappaphycus (Rhodophyta) in customized tank culture
system. Journal of Applied Phycology, 28, 24532458.