scholarly journals Investment Analysis of Willingness to Pay as Development Effort of The Hot Spring Tourism “Cipanas” of Subang Village, Subang Sub-District, Kuningan Regency, West Java Province

2021 ◽  
Vol 4 (2) ◽  
pp. 243
Author(s):  
Willfridus Demetrius Siga ◽  
Yusuf Siswantara

The management of natural resources in terms of ecological, social and economic functions and maintaining the aesthetic value of an object and the environment by encouraging the quality of the environment and the sustainability of rural life can be a value of pride and identity of a village. “Cipanas” Hot Spring Tourism Object in Subang Village, Subang District, Kuningan Regency is managed by the local Village Business Entity (BUMDes). This tourism destination is one of the village development efforts for the common welfare (bonnum commune) both economically, socially and sustainably, it needs good governance and capital / investment support. This study aims to analyze the investment of visitors or service users of hot springs in the form of willingness to pay using the Contingent Valuation Method (CVM) to estimate the costs to be incurred by visitors, and multiple regression methods are used to analyze these factors. what factors influence the visitor's willingness to pay. This type of research uses descriptive analysis with a quantitative approach. The results showed that: 1) female consumers, middle-aged, have a Bachelor's or Diploma's latest education, have an employee status, and high income have the highest willingness to pay in a price range that is more than the WTP value, 2) Consumers are willing to pay above the price offered because it has the belief that the hot spring tourism area provides many benefits, 3) The average WTP value is greater than the average market price. This shows that there is an excess price that consumers are willing to pay. 4) The factors that significantly influence the willingness to pay for Cipanas hot water tourism are gender and monthly income. In addition, 52% of respondents are willing to pay for the development of a tourist attraction for the hot spring "Cipanas" in Subang Village.   

2019 ◽  
Vol 125 ◽  
pp. 14002
Author(s):  
Rakhmadi Sulistyanto ◽  
Udi Harmoko ◽  
Gatot Yuliyanto

Research conducted at Pesanggrahan area, Sangubanyu Village, Bawang District, Batang Regency with geographical coordinates at 7°5'00 "00 S - 7°7'30" 00 S, and 109 ° 56'00 "E-109°58'30"E, with an area of around 25 Km². Research methods used quantitative and qualitative methods with descriptive analysis, geological and geochemical analysis. Geochemical fluid samples were taken in manifestations hot springs Pesanggrahan and hot water samples in Sibanteng and Sileri Crater to determine the relationship with geothermal systems in this area. Geomorphology divided into two geomorphology units, they are steep slope and sloping hill. Stratigraphy can be divided into three lithologies, which are andesite breccia, tuff breccia, and tuff sandstone. Based on fluid geochemical characteristics of manifestations, it can be interpreted that hot spring of Pesanggrahan area is outflow zone with bicarbonate-chloride water type, Sibanteng Crater and Sileri Crater, include upflow zone with water type sulfate for Sibanteng Crater, bicarbonate-sulfide water type for Sileri Crater. Environmental source geothermal fluid Pesanggrahan from the magmatic volcanic process. Sources geothermal fluid in Pesanggrahan, Sibanteng and Sileri Crater from meteoric water. Estimated temperature Pesanggrahan in the interval 50-100°C, Sileri Craters 160-180°C, and Sibanteng Craters 140-150°C. The Conceptual model of Pesanggrahan includes a geothermal system that associated with volcanic system and high relief liquid dominated system.


2021 ◽  
Vol 13 (1) ◽  
pp. 820-834
Author(s):  
Jun Ma ◽  
Zhifang Zhou

Abstract The exploration of the origin of hot spring is the basis of its development and utilization. There are many low-medium temperature hot springs in Nanjing and its surrounding karst landform areas, such as the Tangshan, Tangquan, Lunshan, and Xiangquan hot springs. This article discusses the origin characters of the Lunshan hot spring with geological condition analysis, hydrogeochemical data, and isotope data. The results show that the hot water is SO4–Ca type in Lunshan area, and the cation content of SO4 is high, which are related to the deep hydrogeological conditions of the circulation in the limestone. Carbonate and anhydrite dissolutions occur in the groundwater circulation process, and they also dominate the water–rock interaction processes in the geothermal reservoir of Lunshan. The hot water rising channels are deeply affected by the NW and SN faults. Schematic diagrams of the conceptual model of the geothermal water circulation in Lunshan are plotted. The origin of Tangshan, Tangquan, and Xiangquan hot springs are similar to the Lunshan hot spring. In general, the geothermal water in karst landforms around Nanjing mainly runs through the carbonate rock area and is exposed near the core of the anticlinal structure of karst strata, forming SO4–Ca/SO4–Ca–Mg type hot spring with the water temperature less than 60°C. The characters of the hot springs around Nanjing are similar, which are helpful for the further research, development, and management of the geothermal water resources in this region.


2021 ◽  
Author(s):  
Francois Hategekimana ◽  
Theophile Mugerwa ◽  
Cedrick Nsengiyumva ◽  
Digne Rwabuhungu ◽  
Juliet Confiance Kabatesi

Abstract Hot spring is a hot water that is naturally occurring on the surface from the underground and typically heated by subterranean volcanic activity and local underground geothermal gradient. There are four main hot springs in Rwanda such as: Kalisimbi, Bugarama, Kinigi and Nyamyumba former name Gisenyi hot springs. This research focused on the geochemical analysis of Nyamyumba hot springs located near the fresh water of Lake Kivu. Nyamyumba hot springs are located in the western branch of the East African Rift System and they are located near Virunga volcanic complex, explaining the rising and heating of water. The concentrations of Sulfate, Iron, Ammonia, Alkalinity, Silica, Phosphate, Salinity, Alkalinity, and Conductivity using standard procedures were measured. The results showed that hot spring water has higher concentrations of chemicals compared to Lake Kivu water and the geochemistry of these hot springs maybe associated with rock dissolution by hot water. The measured parameters were compared with World Health Organization (WHO) standards for recreational waters and it has been identified that Nyamyumba hot spring are safe to use in therapeutic activities (Swimming).


2019 ◽  
Vol 23 (5 Part A) ◽  
pp. 2613-2622
Author(s):  
Bi Li ◽  
Shi Zheng

Guangxi Guilin area, China, is rich in hot spring resources. In this paper, a hot spring water temperature monitoring system is developed for longsheng hot springs. Mainly using the hot water of eye of hot springs as the heat source, designing a set of multi-point temperature monitoring system with single-chip and multi-slave as the core of the single-chip microcomputer and wireless and bi-directional transmission for the main station and multiple slave stations to realize automatic temperature monitoring. The system slave station can exchange geothermal water with high temperature extracted from the eye of hot springs and cold water, and automatically control the temperature of the hot spring pool to reach a set value range by controlling the flow rate of the cold water. At the same time, the main station can complete the tasks of monitoring system by setting control commands such as temperature.


2012 ◽  
Vol 3 ◽  
pp. 34-40
Author(s):  
Hendrik Tjiawi ◽  
Andrew C. Palmer ◽  
Grahame J. H. Oliver

 The existence of hot springs coupled with the apparent anomalous high heat flow has sparked interest in the potential for geothermal development in Singapore. This geothermal resource may be potentially significant and could be exploited through Engineered Geothermal System (EGS) technology, i.e. a method to create artificial permeability at depth in granitic or sandstone formations as found under Singapore. The apparently ever-increasing fossil fuel price has made the cost of using the EGS technology more viable than it was in the past. Thus, to assess the resource, a numerical model for the geothermal reservoir has been constructed. Mass and heat flows in the system are simulated in 2D with AUTOUGH2.2, and the graphical interface processed through MULGRAPH2.2. Natural state calibration was performed to match both the observed and the expected groundwater profile, and also to match the hot water upflow at the Sembawang hot spring, with simulated flowrate matching the hot spring natural flowrate. The simulation gives an encouraging result of 125 - 150 °C hot water at depth 1.25 – 2.75 km.


Author(s):  
Muhammad Afzal Jamali ◽  
Muhammad Hassan Agheem ◽  
Akhtar Hussain Markhand ◽  
Shahid Ali Shaikh ◽  
Asfand Yar Wali Arain ◽  
...  

Geothermal water is increasingly used around the world for its exploitation. Bulk electrical resistivity differences can bring significant information on variation of subsurface geothermal aquifer characteristics. The electrical resistivity survey was carried out in Laki range in lower Indus basin in the study area to explore the subsurface geothermal aquifers. The Schlumberger electrode configuration with range from 2 m to 220 m depth was applied. Three prominent locations of hot springs were selected including Laki Shah Saddar, Lalbagh and Kai hot spring near Sehwan city. After processing resistivity image data, two hot water geothermal aquifers were delineated at Laki Shah Sadder hot springs. The depth of first aquifer was 56 m and its thickness 38 m in the limestones. The depth of second aquifer of 190 m and with thickness of 96 m hosted in limestone. In Lalbagh hot springs two geothermal aquifers were delineated on the basis of apparent resistivity contrast, the depth of first aquifer zone in sandstone was in sandstone 15 m and thickness 12 m, while the depth of second aquifer was 61m and thickness was 35m. In Kai hot springs two hot water geothermal aquifers were delineated. The depth of first geothermal aquifer was 21m and thickness was 18 m and the depth of second aquifer was 105 m and thickness was 61m present in sandstone lithology. Present work demonstrates the capability of electrical resistivity images to study the potential of geothermal energy in shallow aquifers. These outcomes could potentially lead to a number of practical applications, such as the monitoring or the design of shallow geothermal systems.


2021 ◽  
Author(s):  
Saeed Ghoddousi ◽  
Behnaz Rezaie ◽  
Samane Ghandehariun

The scattered hot springs on the globe are natural thermal energy storages that are available for industrial and recreational advantages. A hot spring is a hydrothermal system that can be used for power generation purposes as well as deep-well geothermal plants. In the present study, a techno-enviro-economic study is conducted to determine the power generation potential of hot springs as a heat source of the Organic Rankine Cycle (ORC). The hot water temperature and discharge mass flow rate from hot springs varies from 60 to 90 ᵒC and 5 to 50 kg/s, respectively. The ORC plant is modeled by Aspen Plus V9. The impacts of the temperature and mass flow rate of discharge from hot springs on the thermodynamics and economics of the plants are investigated. The results indicate that increasing the hot spring temperature and discharge mass flow rate improves the thermal efficiency and power generation capacity of ORC plant while Payback Period (PP), Levelized Energy Cost (LEC), and Specific Investment Cost (SIC) shrink. The power generation capacity varies from 9.3 kW to 303 kW and the LEC range is from 0.03 $/kWh to 0.13 $/kWh based on the hot spring and water discharge mass flow rate.


2012 ◽  
Vol 6 (2) ◽  
pp. 33-36
Author(s):  
Helda Handayani

Suli hot springs area has a low level of acidity or neutral pH ranges (7,2–7,7). It is also supported by a high chloride concentration value, which ranges (208,87-226,27) ppm. Thisshows that the area on station 1, 2, 3, and 4 are located in areas with water flow into the upper reservoir (upflow) and belongs to hot water domination reservoir tipe (water heatedreservoir). Reservoir temperature is calculated by the formula geotermometer (SiO2)p considered whether applied in the four kinds geotermometer equation because it gives the calculation results are not much different temperature and has a value of rms-error is less than 2%. Reservoir temperature at a hot springs station Suli possible temperature (161 ± 0,9)oC. Reservoir temperature at station 2 hot spring Suli possible hot water temperature (172 ± 1,0)oC. Reservoir temperature at station 3 hot springs Suli possible temperature (171 ±0,9)oC. Reservoir temperature at station 4 hot springs Suli possible temperature (169 ± 1,0)oC.


Agro Ekonomi ◽  
2019 ◽  
Vol 30 (2) ◽  
Author(s):  
Novia Dewi Karisyawati ◽  
Any Suryantini ◽  
Arini Wahyu Utami

Banana is a fruit with the highest consumption level in Indonesia. There are many types of bananas in Indonesia, but only a few types are sold in modern markets and fruit shops, among other Cavendish banana. The Cavendish is known to consumers by their attractive appearance, superior quality and relatively higher prices. This study aims to assess the value of the consumers’ willingness to pay (WTP) for Cavendish banana and its determinant factors. There are two methods used, i.e., contingent valuation method to evaluate the consumers’ willingness to pay, and multiple regression to analyse its determinant factors. Primary data were obtained from 100 respondents by purposive sampling and interviewed in Yogyakarta Special Region between April and June 2019. The results indicate that the consumers’ willingness to pay (WTP) for Cavendish banana is IDR 24,485/kg, which is above the market price. The determinant factors of the consumers’ willingness to pay include the Cavendish banana price, quality of the Cavendish, monthly frequency of consuming banana, family size, income and marital status. The high value of the consumers’ willingness to pay indicates the good opportunity to expand the Cavendish banana market in Special Province Yogyakarta, by taking into account quality and market segmentation.


Agro Ekonomi ◽  
2021 ◽  
Vol 32 (1) ◽  
Author(s):  
Puspita Dewi Hidayaningtyas ◽  
Irham Irham ◽  
Arini Wahyu Utami

This study aims to: (1) determine the characteristics of chrysanthemum consumers in three cities in Java, namely Yogyakarta, Semarang and Surakarta, (2) compare the willingness to pay (WTP) of chrysanthemum consumers, especially Pasopati cultivar in the three cities, (3) analyze the determinant factors of the chrysanthemum consumers’ WTP. There is a total of 120 respondents who participated in this study, i.e., 40 in each city selected with accidental sampling. The consumers’ WTP was assessed using contingent valuation method, and its determinant factors was analyzed using multiple regression. The results showed that the majority of chrysanthemum consumers in the three cities were 17-25 years old, were female, held a bachelor degree, owned a job, were single and had no dependent. The value of wilingness to pay from the three cities shows higher results than the market price of IDR 30,000. The highest WTP value is in Semarang City and the lowest WTP value is in Yogyakarta City. Based on the results of the regression, the determinants that influence the value of WTP differ in each city, but income is a significant determinant in all cities. The value of willingness to pay chrysanthemum Pasopati cultivar can be used as a reference to set the selling price of chrysanthemum flowers. Chrysanthemum such as Pasopati cultivar in Indonesia, needs to be developed more by looking at the willingness of consumers to pay.


Sign in / Sign up

Export Citation Format

Share Document