Study of Raw Water Needs at Cibanten Reservoir

Serang Regency, Banten Province

 

Sudarmanto, Achmad Syarifudin

Bina Darma University Palembang, Indonesia

Email: [email protected]

 

 

Keywords

Abstract

Clean Water, Embung, Discharge, Cibanten, Ciomas

The rural communities of Sukadana and Sukabares in Serang Regency, Banten Province, require clean and quality water. Current water supply of 10 liters per second serves 4,120 people in Sukadana and 500 in Sukabares. Yet, many lack access due to a required flow rate of 21 liters per second for the combined population of 9,399. Additionally, the existing water network is aging and functioning suboptimally due to damage and insufficient volume capacity. The research indicates that by 2045, the new network will cater to 15,952 individuals, with a required flow rate of 36 liters per second. This will serve domestic households at 20.30 liters per second, social activities at 1.11 liters per second, and non-domestic purposes at 3.86 liters per second, resulting in a total demand of 35.38 liters per second, considering water loss due to evapotranspiration. The available drinking water flow is abundant at 272 liters per second. With the development and improvement of the Clean Water System, this water supply will be sufficient to meet the consumption needs of the communities in Sukadana and Sukabares in the Ciomas sub-district of Serang Regency, Banten Province. Furthermore, the Cibanten Reservoir serves an additional purpose by irrigating 159 hectares of rice fields in Sukadana Village at approximately 87 liters per second, as well as supporting tourism in Serang Regency and the broader Banten Province. The challenge of the Clean Water Network System is being addressed through the construction of this system by the Ministry of Public Works and Housing, Directorate General of Water Resources, SNVT Groundwater and Raw Water, and the Cidanau-Ciujung-Cidurian River Basin Agency, Banten province.

https://jurnal.syntax-idea.co.id/public/site/images/idea/88x31.png

� 2023 by the authors. Submitted

for possible open access publication

under the terms and conditions of the Creative Commons Attribution (CC BY SA) license ( https://creativecommons.org/licenses/by-sa/4.0/ ).

 

 

1.      Introduction

Water plays a crucial role in the existence of living beings on this planet. Humans, as part of this realm, depend on water for various needsdirect, such as drinking, cooking, cleaning, and sanitation, as well as indirect, like irrigation, hydroelectric power generation, and tourism (Ikhsan, 2017). Water sources include surface and groundwater. Growing populations and rapid development across sectors have escalated water demands, while the availability of water from sources remains relatively constant due to regional climates. In the Ciomas sub-district, there's the potential of Cibanten Reservoir, serving as a raw water source for clean water in Sukadana and Sukabares communities, Serang Regency, Banten Province. Geographically located between -7� 48' 2.84'' to -7� 43' 30.9'' latitude and 105� 58' 52.89'' to 106� 4' 58.23'' longitude, its boundaries are: 1) North: Pabuaran Sub-district, 2) South: Carita Sub-district, Pandeglang Regency, 3) West: Padarincang Sub-district, and 4) East: Baros Sub-district (Post, Louis, Lippincott, & Procopio, 2013). The district's capital is situated in Panyaungan Jaya Village, approximately 26 KM away from the regency's capital. The hilly topography influences the district. Cibanten Reservoir is used by Sukadana and Sukabares for clean water, managed informally. This study aims to assess the potential water source utilized by the government to meet domestic and non-domestic water needs and provide solutions to related water supply issues (Syarifudin, 2022).

 

Peta Kota: Peta Kabupaten Serang

Figure 1 Cibanten Reservoir Research Location

 

2.      Materials and Methods

A preliminary survey was conducted to gain an overview of the Cibanten Reservoir's condition, socio-economic status, population data, as well as existing facilities and infrastructure in the communities of Sukadana and Sukabares, Ciomas sub-district, Serang Regency, Banten Province. This study utilized both primary and secondary data. Primary data encompassed the flow rate of the Cibanten Reservoir, while secondary data included population statistics, facilities, infrastructure, rainfall and climatology data, and topographic data. Rainfall data, climatology data, and topographic maps were obtained from the Cibanten Rain Gauge Station and the BBWS C3 (Cidanau Ciujung Cidurian) Office, Banten Province. Rainfall data, climatology data, and topographic maps were used to analyze the reliable flow rate, which refers to the flow rate that can be truly relied upon in a river or reservoir, during both dry and rainy seasons. The Fj. Mock method was employed for analyzing the reliable flow rate. Additionally, flow rate measurements were taken using a Curenmeter (Kironoto et al., 2012).

Method of Fj. Mock

The parameters relevant to this study are as presented in the formulation by FJ. Mock in his paper "Land and Capability Appraisal and Water Availability Appraisal, Bogor, Indonesia, 1973." This introduced a method for simulating river flow based on rainfall, evapotranspiration, and the hydrological characteristics of the watershed. The model was derived from empirical research by incorporating monthly rainfall data and other monthly physical parameters, resulting in simulated monthly flow rates. The formula/equation of the FJ. Mock Model used in this study is: (Cuen & RH, 1982)

Rain Data Processing

Rain value monthly (P) is obtained from recording of rain data monthly (mm) and quantity day rainfall in the month concerned (h). In principle, hydrological data got with method collect secondary data, with contact related agencies� direct with problems encountered. Data bulk used rain� in studies This taken from station imminent rain� with area studies that is Rain Post Cibanten. Term trend long Rain monthly at the station used as rain data within the work area can seen in Table 1.

 

Table 1 Monthly Average Rainfall (mm) Study Area

Source: Cibanten Rain Post

Climatological Data Processing

Description of conditions climate area studies can seen from results recording station existing climatology and rainfall.� Climatological data For area studies This taken from Cibanten Rain Post (Afiatun, Notodarmojo, Effendi, & Sidarto, 2018).

Hydrometric Data Processing


Hydrometric data got from implementation survey hydrometry carried out at the Cibanten Reservoir. Survey covers measurement of river discharge and water quality (Li et al., 2023).

 

 

Figure 1 The Hydrological Cycle as the basis for the FJ water balance model. Mock and Influence Factors of Evapotranspiration

Formula of Mainstay Discharge Calculation

Evapotranspiration


Evapotranspiration limited is actual evapotranspiration with consider condition vegetation and surface land so that the similarities as following : (Ali, Lestari, & Putri, 2021)

 

Where:

E� ������� �= Difference Between Evapotranspiration Potential And Evapotranspiration Limited (mm)

ETo*��� = Evapotranspiration Potential (mm)

d �������� �= Amount Day Dry or Day without Rain In 1 Month

m ������� = Percentage Land That is not Vegetation, Estimated From Use Map Land, Taken M = 0% For Land With Heavy Forest

m�������� = 0 % at End Rain Season, and The Addition Of 10% Each Month Dry For Land With Forest Secondary

m ������� = 10 % - 40 % for eroded land ��

m ������� = 30 % - 50 % for land processed agriculture (rice field, lading, p)

Water balance at ground level

Water balance at ground level counted based on magnitude bulk Rain monthly reduced mark evapotranspiration limited monthly average so that obtained equation :

ΔS = P � ET

Where:

ΔS = change soil water content ( soil storage ).

The value positive if P > ET, water enters to in land

The value negative if P < ET, part of the groundwater go out so that happen deficit.

Ground water storage

Runoff and ground water values magnitude depends from water balance and conditions the land. Required data are :

Coefficient infiltration (I ) taken 0.2 - 0.5

Recession factor groundwater flow (k) is taken 0.4 - 0.7

Equation :

In = WS x I

Vn = k. Vn-1 + 0.5 (1 + k). in

ΔVn = Vn � Vn-1

Where:

In = infiltration, the volume of water entering to in land

Vn = volume of ground water

Vn-1 = volume of groundwater month to (n-1)

ΔVn = change in groundwater volume

I = coefficient infiltration

k = factor recession groundwater flow�

 

Flow equalization �

For even distribution incoming flow to deposition zone can used wall perforated walls.� The surface area of the pit is calculated by the equation:

The calculation of pressure loss in the hole is used equation:

Debit Measurement with Curenmeter

Location Water discharge measurement is carried out by Cibanten Dam, Sukabares Village, Ciomas District, Seranga Regency, Banten Province, at coordinates X = 615728.803, Y = 9312505.692 (Jiang et al., 2019). Water discharge measurements are carried out at 4 points, namely in the upstream of the weir, downstream of the Cibanten weir, the glory spring, and the bridal spring. An overview of the discharge measurement location can be seen in the following figure (Kuncoro, 2013).

 

Figure 2 Activity Location Map

 

River and Open Canal Discharge Measurement Method (SNI 8066:2015)

Tools:

  1. A Set of Current Meter Tools
  2. Meter

Procedure measurement of water discharge in the river (Current Meter Method)

1.      Assembly Tool Current Meter

2.      Meter stretched throughout wide river and recorded results measurement.

3.      River width shared to 3-7 areas based on wide river the.

4.      After sharing 3-7 area, depth river be measured with use meter

5.      After depth measured, parts a, b, c are measured return as point measurement current meter.

6.      After obtaining three depth river with cut each part middle, the height of the current meter is determined by multiplying depth river with 0.6d.

7.      Speed current be measured with three repetitions� using a current meter with t = 60 seconds.

8.      Calculate river water discharge

 

Raw Water Needs

Clean water needs of Households ( domestic )

Clean water needs of Households is the water obtained in a manner individual from source of water made by each house ladder like well shallow, piping or hydrant general or can obtained from service System Drinking Water Supply (SPAM) PDAM. The source of raw water by PDAM consists from groundwater and surface water or combined from both. Use of water is influenced by: (Aboagye & Rowe, 2011)

-      Type of water source (connection to House or fire hydrant general)

-      Type of use (toilet, shower, etc.)

-      Equipment per house ladder

-      Use of water outside house (garden, wash car etc.)

-      Income level

Domestic water demand refers to the water used for household purposes. The water requirement per person per day is estimated at a flow rate of 144 liters/person/day (Department of Public Works, Directorate General of Human Settlements, 2006).

The total water demand is calculated based on the projected number of water users for the next 5 to 10 years, and the requirement for each user is increased by 20% to account for water losses (leakage) (Oh, Cho, & Yun, 2014). This clean water demand is determined based on service provided through Public Hydrants (PH) using the following equations (Department of Public Works, Directorate General of Human Settlements, 2006):.

Qmd = Pn xqx fmd (3.2)

Qt = Qmd x 100/80 ( factor water loss 20%) (3.3)

with :

Qmd = Need for clean water

Mr�� = Amount resident year n

q���� = Water requirement per person/ day

fmd = Day factor maximum (1.05-1.15)

Qt = total demand for clean water

Clean water needs House ladder, stated in unit liters / person / day (L/O/H), large need depends from category city based on amount residents, namely :

Table 2 Clean Water Needs Population Per Person Per Day

No

City Category

Clean Water Needs (L/O/H)

1.

Semi-Rural

60

2.

Small town

90

3.

Medium City

110

4.

Big city

130

5.

Metropolis

150

Source : Directorate General Cipta Karya Ministry Public Works

Social water needs�

Water requirement for social assumed 20% of amount residents in need need 30 liters/day. The more big and solid resident will tend more Lots own area commercial and social, so need the for water will more higher (Groot et al., 2015).

Non- Domestic Needs

Non-domestic water needs, namely water needs which include industrial needs, institutional needs, and commercial use. Institutional needs include water needs for schools, hospitals, places of worship, government buildings, and others. Commercial water needs for an area are in line with increasing population and land use changes.

Irrigation Water Needs

Water requirements for plant are shared into three needs, namely :

1)   Crop Water Requirement/CWR

2)   Farm Water Requirement / FWR

3)   Project Water Requirement/PWR

Measurement speed use method mean section is performed with share cut channel to be measured into the later sections measurement done in each section. Location and amount measurement speed on each sexy customized with depth river/channel. Channel measured irrigation is channel relatively tertiary small and shallow, therefore That channel will shared into two sections and measurement speed Genre carried out at a depth of 0.6 parts from base channel (0.6 s) (Afifah, Sabar, Wulandari, & Marselina, 2019).

 

3.      Results and Discussions

Population Growth Projection

Population analysis is conducted to understand and formulate various aspects of population needed for water demand planning, including population count and trends in growth and distribution. Over time, a region will experience population growth. To project or predict future population, several formulas such as Arithmetic, Geometric, and Exponential can be used. In this study, data for formulating clean water demand in Sukabares, Sukarena, and Sukadana villages of Ciomas sub-district are utilized to calculate maximum daily and peak-hour water requirements, based on Exponential calculations.

Population registration data processed by the Central Statistics Agency (BPS) of Serang Regency, Banten Province, shows that the populations of Sukabares and Sukadana villages in the Ciomas sub-district have been consistently growing year by year. Population growth is influenced by natural factors such as births (natality) and deaths (mortality), as well as migration. Birth and death rates contribute to natural growth, while migration contributes to non-natural growth. Population growth data for Sukabares and Sukadana villages in the Ciomas sub-district can be observed in Table 3 below.

 

 

Table 3 Growth Population Sukabares and Sukadana Subdistrict Ciomas 2016�2022

No.

Village Name

Year

2016

2017

2018

2019

2020

2021

2022

1

Sukabares

2,664

2,799

2,935

3,070

3,209

3,419

3,610

3

Sukadana

4,921

5034

5.145

5,260

5,375

5,583

5,789

Amount

6,277

6,583

6,890

7,195

8,584

9,002

9,399

�����

The projected population results for upcoming years reflect the quantity of domestic water demand, as an increase in population is equivalent to an increase in domestic water needs. Social, cultural, and economic factors within the population determine the extent of domestic water usage (Nadia, Mananoma, & Tangkudung, 2019). Three methods are employed to estimate future population: the Arithmetic Method, the Geometric Method, and the Exponential Method. These three methods, along with their mathematical formulas, are explained as follows:

Arithmetic method

Arithmetic Population Growth is population growth with an absolute number of numbed that is considered equal each year. The equation used is:

Pn = Po ( 1 + r. n )

Where :

��������� Pn = Amount resident "n" years who will come

����������� Po = Amount Resident year previously

r = average percentage increase resident

n = Amount next year� come

P2023 = Po ( 1 + r. n )

= 9,399 ( 1 + 2.3 % x 1)

= 9,615 souls.

P2024 = Po ( 1 + r. n )

= 9,399 ( 1 + 2.3 % x 2)

= 9,831 souls.

P2025 = Po ( 1 + r. n )

= 9,399 ( 1 + 2.3 % x 3)

= 10,048 souls.

Geometric Method

This method assumes that the development of the number of residents (consumers) is automatically multiplied by the equation:

Pn = Po(1 + r) n

Where :

���������������� Pn = Number of "n" years to come come

����������������������� Po = Amount Population by year previously

����������������������� r = Average percentage of population growth

����������������������� n = Amount next year� come

 

P2023 = Po(1 + r) n

= 9,399 ( 1 + 2.3 %)ˡ

= 9,615 souls.

P2024 = Po(1 + r) n

= 9,399 ( 1 + 2.3 %)�

= 9,838 souls.

P2025 = Po(1 + r) n

��������� = 9,399 ( 1 + 2.3 %)�

= 10,063 souls.

 

Exponential Method

This method follows the equation:

Pn = Po ( е ) r. n

Where :�����������

���������������� Pn = Number of "n" years to come come

����������������������� Po = Amount Population by year previously

����������������������� r = average percentage of population growth

����������������������� n = Amount next year� come

e���� = exponential

P2023 = Po ( е ) r. n

= 9.399 (2.7182818 ) 2.3 x 1

= 9,618 souls.

P2024 = Po ( е ) r. n

= 9.399 (2.7182818 ) 2.3 x 1

= 9,841 souls.

P2025 = Po ( е ) r. n

���������� = 9.399 (2.7182818 ) 2.3 x 1

= 10,070 souls.

 

 

Debit Measurement Results with Curenmeter


The cross-sectional shape of each water flow can be seen in the illustration below.

Figure 3 Cross section Genre

 

The results of measurements carried out in the field, then data processing is carried out. So that a discharge is obtained that flows from each body of water. The results of data processing can be seen in the following table.

 

Table 4 Water Debit Measurement Results

Location Point

Segment

Depth
(m)

Width
(m)

Speed
(m/s)

Average speed
(m/s)

Cross Sectional Area Wet
(m 2 )

Discharge
(m 3 /sec)

Discharge
(l/s)

Total Debit
(l/s)

Cibanten Lake

1

0.09

2,13

0.3

0.43

0.19

0.08

83.07

274.77

0.4

0.6

2

0.09

2,13

0.4

0.5

0.19

0.10

95.85

0.5

0.6

3

0.09

2,13

0.4

0.5

0.19

0.10

95.85

0.5

0.6

Location Point

Segment

Depth
(m)

Width
(m)

Speed
(m/s)

Average speed
(m/s)

Surface Area Wet
(m 2 )

Discharge
(m 3 /sec)

Discharge
(l/s)

Total Debit
(l/s)

Lower Cibanten Lake

1

0.35

0.45

0.6

0.475

0.16

0.07

74.8

242

2

0.3

0.45

0.5

0.14

0.06

64,1

3

0.28

0.45

0.5

0.13

0.06

59,9

4

0.2

0.45

0.3

0.09

0.04

42.8

 

 

Mainstay Debit Fj. Mock

Calculation of the average monthly discharge is conducted using monthly mid-rainfall data. This essential calculation of reliable flow rates can be achieved through various methods, with the commonly employed method being the F.J. Mock Method for estimating baseflow. The Directorate of Irrigation (1980) states that the estimation of available water in rivers is computed using the F.J. Mock Method. This method assumes that the rain falling within the River Irrigation Area (DPS) will partly be lost as evapotranspiration, determined based on climatological data. A portion will become direct runoff, and another portion will infiltrate into the soil as infiltrated water. When the soil moisture capacity is exceeded, water will flow downward due to gravity (percolation) into groundwater, eventually emerging in rivers as base flow (Seyhan, 1975).

The rainwater flow, modified by the DPS system in question, eventually reaches the rivers within the corresponding DPS. River flow is composed of the sum of surface runoff and base flow.

 

Table 4 Total Rain and Daily Amount of Rain

 

The results of mainstay discharge analysis with the F.J Mock method in the Study area can be seen in Table 4 Calculation of Cibanten Embung Discharge with FJ Method. Mock with the calculation results of Debit experienced a surplus every month with the highest surplus in February of 63.79 liters / second and the lowest in August of 22.37 liters / second. Then the Cibanten Embung Water Balance Balance can be seen in Figure 5.10. Cibanten Embung Water Balance which shows that the discharge of water use is smaller than the availability of water, water use is 35.38 liters / second to 118.61 while water availability ranges from 254.07 liters / second to 292.83 liters / second. There is a water balance surplus between 133.91 liters / second to 189.42 liters / second (Soewarno, 1991).

Results of Raw Water Needs

Household, urban and industrial water needs are calculated using population statistics. The results of the calculation of clean water needs are as follows::

 

Clean water needs of Households ( domestic )

Household clean water needs are water obtained individually from water sources made by each household such as shallow wells, piping or public water supply or can be obtained from the Drinking Water Supply System (SPAM) service (Badaruddin, Kadir, & Nisa, 2021).

Raw water sources consist of groundwater, surface water or a combination of the two. The use of water used is influenced by:

-      Type of water source (connection to a house or public hydrant)

-      Type of use (toilet, shower, etc.)

-      Equipment per household

-      Water use outside the home (park, car wash etc.)

For Sukabares and Sukadana villages, Ciomas sub-district, Serang Regency, Banten Province, the category of cities is medium so that the need for clean water per liter per person per day is 110 liters / person / day (see table). Formula calculates Clean Water Needs of Domestic Population = Number of Population x 110 x 1/(24x60x60) liter/second = 9,618 x 110 x 1/(24x60x60) liter/second = 12.24 liter/second.

Social water needs�

Water needs for social are assumed to be 20% of the total population that requires the need of 30 liters / day. The larger and denser the population will tend to have more commercial and social areas, so the water needs will be higher. Social Water Needs Formula = 20% x Total Population x 30 x 0.00001157 liters/second = 20% x 9,618 x 30 x 1/(24x60x60) liters/second = 0.67 liters/second.

Non- Domestic Needs

Non-domestic water needs, namely water needs which include industrial needs, institutional needs, and commercial use. Institutional needs include water needs for schools, hospitals, places of worship, government buildings, and others. Commercial water needs for an area are in line with increasing population and changes in land use. The following are some of the water needs for non-domestic in 2023.

1). Water needs of school pupils

According to the Directorate General of Copyright, Department of Public Works, the need for clean water for school students is 5 liters / student / day. School Student Water Needs Formula = Number of Students x 5 liters/day = 1,820 x 5 liters/day = 9,100 liters/day.

2). Water needs of Puskesmas

According to the Directorate General of Copyright, Department of Public Works, water needs for hospitals are calculated based on the number of beds, which is 500 lt/bed/day and for puskesmas of 1200 liters/unit/day. Puskesmas Water Requirement Formula = Number of Puskesmas x 1,200 liters/day = 0 x 1,200 liters/day = 0 liters/day.

3). Water Needs for Places of Worship

According to the Directorate General of Copyrights of the Department of Public Works, the water requirement for mosques is 3000 liters / unit / day while churches / temples are 1000 liters / unit / day. Mosque/Mushola Water Requirement Formula = Number of Mosques/Mushola x 3000 liters/day = 44 x 3000 liters/day = 132,000 liters/day. Church/Temple Water Requirement Formula = Number of Churches/Temples x 1000 liters/day = 0 x 1000 liters/day = 0 liters/day.

4). Water needs for the Market

According to the Directorate General of Copyrights of the Department of Public Works, the water requirement for mosques is 12,000 liters / unit / day. Water Requirement Formula Number of Markets = Number of Markets x 1,200 liters/day = 1 x 1,200 liters/day = 1,200 liters/day.

5). Water needs for industry

According to the Directorate General of Cipta Karya DPU in 1996, the need for water for industry is 10 liters / unit / day. Water Requirement Formula for Industry = Number of Industries x 10 liters / day = 0 x 10 liters / day = 0 liters / day.

6). Water needs for stall employees

According to the Directorate General of Cipta Karya DPU in 1996, water needs for stall employees are liters / units / day. Water Requirement Formula for stall employees = Number of stall employees x 10 liters / day = 120 x 10 liters / day = 1,200 liters / day

Total non- domestic water demand = (1+2+3+4+5+6) x 0.00001157 liter/ second = 9,100 + 0 + 132,000 + 1,200 + 0 + 1,200 = 143,500 liter/ day x 1/(24x60x60) liter / second = 1.66 liters / second.

Total Water Needs in 2023 = Domestic Water Needs + Social Water Needs + Non- Domestic Water Needs = 12.24 +0.67 + 1.66 = 14.57 liters/ second.

Loss of Water

loss = 10% x Total Water Needs (liters/ second ) = 10% x 14.57 liters/ second = 1.46 liters/ second.

Maximum Daily Needs

Maximum Daily Needs = 1.15 x Total Water Needs (liters/ second ). = 1.15 x 14.57 liters/ second = 16.75 liters/ second.

Needs at Peak Hours

Demand for discharge at peak hours = 1.5 x total water demand (liters/ second ) = 1.5 x 14.57 liters/ second = 21.85 liters/ second.

Total Water Needs = Debit Needs at Peak Hours � Water Losses (liters/ second ) = 21.85 � 1.46 = 20.40 liters/ second.

Prediction of raw water needs in Sukabares and Sukadana Villages, Ciomas District, Serang Regency, Banten Province, in 2023 Domestic Water Needs of 12.24 liters/second, Social of 0.67 liters/second and Non-Domestic of 1.66 liters/second, water needs at peak hours of 21.85 liters/second, maximum daily needs of 16.75 liters/second, predictions of water loss of 1.46 liters/second, then the total water demand in 2023 is 20.40 liters/second. Then after that, in 2024, the total water demand is 20.96 liters / second and increases every year.

If reviewed until 2045, Domestic Water Demand is 20.30 liters/second, Social 1.11 liters/second, Non-Domestic is 3.86 liters/second, water needs at peak hours are 37.91 liters/second, maximum daily needs are 29.06 liters/second, predicted water loss is 2.53 liters/second, then Total Water Demand in 2045 is 35.38 liters/second (Table 4).

 


Table 5 Non- Domestic Water Needs in Sukadana and Sukabares Villages Subdistrict Ciomas Year 2023

�������������������������������

Water Balance

The results of mainstay discharge analysis with the F.J Mock method in the Study area can be seen in Table 5 Calculation of Cibanten Embung Discharge with FJ Method. Mock with the calculation results of Discharge experienced a surplus in each month with the highest surplus in February of 63.79 liters / second and the lowest in August of 22.37 liters / second. Then the Cibanten Embung Water Balance Balance can be seen in Figure 5.10. Cibanten Embung Water Balance which shows that the discharge of water use is smaller than the availability of water, water use is 35.38 liters / second to 118.61 while water availability ranges from 254.07 liters / second to 292.83 liters / second. There is a water balance surplus between 133.91 liters / second to 189.42 liters / second.

 

 

 

 

 

 

 

Table 6 Cibanten Reservoir Water Balance Balance

Figure 4 Cibanten Reservoir Water Balance

 

Water Quality Analysis (Laboratory Test)

In terms of health considerations, the quality of raw water must account for the possibility of pollution from potential sources of contamination in the river. In terms of its intended use, raw water should be capable of removing turbidity, color, iron, and manganese through a conventional filtration system without requiring special treatment. Regarding operational and maintenance aspects, the system should function and be maintained normally to produce potable water that meets health standards.

Sampling of this water is conducted at the planned intake site. These samples are collected for laboratory testing. Through these laboratory tests, the water quality intended for raw water purposes (Quality standard B) will be determined.

To assess water quality in the field, a "Water Quality Checker" measuring instrument is utilized.

For laboratory testing purposes, water samples are collected at the planned intake site. These samples are gathered for laboratory testing. Through these laboratory tests, the quality of the water intended for raw water purposes (Quality standard B) will be ascertained.

 

 

Line Callout 3: Lokasi Pengambilan Sampel Air

Figure �5 Water Sampling Locations

 

The water quality parameters studied refer to the standard parameters for drinking water quality according to Government Regulation No. 82 of 2001 as presented in Table 5.10 below

 

Table 7 �Quality Standards for Raw Water Quality

No.

Parameter

Unit

Quality standards

A

B

1

Nitrate

Mg/L

10

10

2

Nitrite

Mg/L

0.05

1

3

Substance organic

Mg/L

-

400

4

Fe

Mg/L

0.3

-

5

M N

Mg/L

0.1

-

6

Na

Mg/L

-

200

7

Hg

Mg/L

0.001

0.002

8

F

Mg/L

0.5

1.5

9

TDS

Mg/L

1000

1000

10

Sulfate (SO 4 )

Mg/L

400

-

11

Cl -

Mg/L

0.03

0.03

12

hardness

Mg/L

-

500

Source : Regulation Government No. 82 of 2001

 

The water samples were collected from Cibanten Reservoir. Each sample was collected in an amount of 2 liters. Based on the laboratory test results conducted at the Serang City laboratory, the tested samples are still suitable for use as raw water, as they still possess good physical and chemical properties for household/drinking water purposes. However, it should be noted that water quality during the rainy season, when the water at the location becomes turbid for a period, needs to be considered.

Water quality analysis is performed, taking into account the content of iron, magnesium, potassium, boron, chloride, sulfate, and nitrogen oxide that meet drinking water standards. Raw water to meet the needs of the community should contain as few toxins, heavy metals, and substances affecting health as possible, such as mercury, fluoride, and nitrate. The water content from the Cibanten Reservoir is suitable for consumption by the community after boiling. The results of the water quality analysis are presented in Table 5.11.

 

Cibanten Reservoir Capacity/Capacity

Reservoir volume Cibanten at the time This with Still there is aquatic plants and sedimentation is of 6,511.51 m3. Sediments and water plants Apu-apu of 1,416.87 m3. pond volume after done cleaning/normalization is 6,511.51 + 1,416.87 = 7,928.38 m3. Calculation of Reservoir Volume Cibanten can seen in table 5.13.

Table 8 Cibanten Reservoir Capacity/Capacity

Source : Analysis Researcher

Calculation Capacity / Capacity Reservoir Cibanten and Graphics Inundation Area Relationship and Volumes Reservoir can be seen in tables and figures below.

Table 9 Inundation Area Relationship with Reservoir Volume

Source : Analysis Researcher

 

Figure 6 Relationship of Inundation Area and Reservoir Volume


On 40% of the surface of Cibanten Reservoir, there is a water plant known as "Apu-apu" (Pistia stratiotes). Despite reducing the reservoir's capacity and storage, this plant has numerous benefits. Also known as "kapu-kapu," this aquatic plant serves as an ornamental plant. The plant's size ranges from 2 to 10 cm in length and 2 to 6 cm in width, with leaves featuring notched edges and thick hair on the water's surface. Apu-apu produces spike-like flowers that emerge from the leaf axils. These white flowers are approximately 1 cm in size. Its fruit is round and red, measuring 5 to 8 cm, containing black, round seeds about 2 mm in size. With its broad leaves growing in clusters, Apu-apu serves well as shade for fish. Furthermore, Apu-apu functions as a cleaner of harmful radioactive pollutants in water. It effectively reduces iron (Fe) levels in water by more than 90% and enhances water quality over time. The plant also naturally removes excess algae and nutrients from the water. Additionally, Apu-apu can be used as feed material due to its dry weight composition of 37% BETN, 19.5% crude protein, 25.6% ash content, 1.3% crude fat, and 11.7% crude fiber (Yudhistira 2013). The volume of Apu-apu water plants in Cibanten Reservoir is calculated as 25% x 4,091.50 m� x 0.1 m = 102.29 m�. Recognizing the importance of Apu-apu, it is advisable not to completely remove this plant during the Cibanten Reservoir Rehabilitation activity. Instead, around 5-10% of the reservoir's surface area should be dedicated to preserving this plant.

Figure 7 Apu-apu Aquatic Plants on the surface of the Embung water Cibanten

 

4.      Conclusion

 

From the results of the study can be concluded and suggested as follows: 1. The projected result of the discharge (liter / second) of clean water needs of Sukadana Village and Sukabares Ciomas District until 2045 is 35.38 liters / second. 2. The availability of mainstay discharge (liter/second) of Embung Cibanten is 254.07 liters/second (minimum discharge in July) to 292.83 liters/second (maximum discharge in January), so that the people of Sukadana and Sukabares villages can enjoy the abundance of Cibanten Embung Water. 3. The result of the Cibanten Embung Water Balance Simulation is greater Availability than Usage (Surplus). Availability is 254.07 liters / second to 292.83 liters / second while Usage is 35.38 liters / second to 122.36 liters / second. Use in addition to raw water is also for agricultural irrigation. 4. After going through laboratory tests, the content of Cibanten Embung Water is included in the Class B category, so that it meets the standards for the procurement of raw water that is suitable for consumption by the community as clean water by first boiling it before being used as drinking water. 5.The volume of water in Cibanten Reservoir before cleaning/normalization of sediments and aquatic plants was 6,511.51 m3 and after cleaning/normalization of reservoirs from sediments and aquatic plants was 7,928.38 m3.

 

5.      References

Aboagye, G., & Rowe, M. T. (2011). Occurrence of Mycobacterium avium subsp. paratuberculosis in raw water and water treatment operations for the production of potable water. water research, 45(11), 3271�3278.

Afiatun, Evi, Notodarmojo, Suprihanto, Effendi, A. J., & Sidarto, K. A. (2018). Cost minimization of raw water source by integrated water supply systems (a case study for Bandung, Indonesia). GEOMATE Journal, 14(46), 32�39.

Afifah, Eva, Sabar, Arwin, Wulandari, Suci, & Marselina, Mariana. (2019). The Reliability Study of Raw Water Sources in the Development of Potable Water Supply Systems in Indonesia. GEOMATE Journal, 16(54), 209�216.

Ali, F., Lestari, D. L., & Putri, M. D. (2021). Peat water treatment as an alternative for raw water in peatlands area. IOP Conference Series: Materials Science and Engineering, 1144(1), 12052. IOP Publishing.

Badaruddin, Badaruddin, Kadir, Syarifuddin, & Nisa, Khairun. (2021). Hidrologi Hutan. CV. Batang.

Cuen, Mc R. H., & RH, A. (1982). A guide to Hydrologic Analysis using SCS Methode. Prentice Hall Inc. Englewood. Cliffs, NJ.

Groot, C. K., Van Den Broek, W. B. P., Loewenberg, J., Koeman-Stein, N., Heidekamp, M., & De Schepper, W. (2015). Mild desalination of various raw water streams. Water Science and Technology, 72(3), 371�376.

Ikhsan, Cahyono. (2017). The effect of variations in flow rate on the bottom of an open channel with uniform flow. Civ. Eng. Media.

Jiang, Zhiqiang, Wang, Chao, Liu, Yi, Feng, Zhongkai, Ji, Changming, & Zhang, Hairong. (2019). Study on the raw water allocation and optimization in Shenzhen city, China. Water, 11(7), 1426.

Kironoto, Bambang Agus, Yulistiyanto, Bambang, Istiarto, Istiarto, Sumiadi, Sumiadi, Nugroho, Bayu, & Ariyanto, Anton. (2012). The Validity of Clauser�s Method for Determining Shear Velocity, u*, in a Curved Channel.

Kuncoro, Mudrajad. (2013). Metode Riset Untuk Bisnis & Ekonomi: Bagaimana Meneliti & Menulis Tesis?

Li, Lingjie, Wang, Leizhi, Gao, Xuan, Su, Xin, Wang, Yintang, & Gao, Rui. (2023). Joint Optimal Dispatch of Complex Urban Raw Water Supply: A Case Study of Lanxi City, Zhejiang Province, China. Water, 15(17), 3136.

Nadia, Kivani, Mananoma, Tiny, & Tangkudung, Hanny. (2019). Analisis debit banjir dan tinggi muka air Sungai Tembran di Kabupaten Minahasa Utara. Jurnal Sipil Statik, 7(6).

Oh, Sunhee, Cho, Yong, & Yun, Rin. (2014). Raw-water source heat pump for a vertical water treatment building. Energy and buildings, 68, 321�328.

Post, Gloria B., Louis, Judith B., Lippincott, R. Lee, & Procopio, Nicholas A. (2013). Occurrence of perfluorinated compounds in raw water from New Jersey public drinking water systems. Environmental science & technology, 47(23), 13266�13275.

Seyhan, Ersin. (1975). Fundamentals of hydrology. Geografisch Instituut der Rijksuniversiteit te Utrecht.

Soewarno, S. (1991). Hidrologi Pengukuran dan Pengolahan Data Aliran Sungai (Hidrometri). Nova, Bandung, hal. xx, 825.

Syarifudin, Achmad. (2022). Uji kemiripan--Prediction of The Depth Erosion in Rivers with Scale Models.