{"title":"Valuasi Ekonomi Kawasan Karst Desa Jatijajar Kecamatan Ayah Kabupaten Kebumen","authors":"Rasyid Wisnuaji, Muhamad Rijal Pamungkas","doi":"10.26418/j.sea.v11i1.43542","DOIUrl":null,"url":null,"abstract":"Jatijajar Village which is included in the Gombong karst area in accordance with the Minister of Energy and Mineral Resources Decree No. 3043 K / 40 / MEM / 2014 and confirmed by the Kebumen Regency Regional Regulation No. 23 of 2012 concerning RTRW of Kebumen Regency for 2011 - 2013. Karst is a landscape of the karstification process of carbonate rock (CaCO3) which is deposited after passing through the available geological space and time. Karst has a distinctive hydrological condition due to the dissolution of carbonate rock due to the physical properties of limestone which is easily soluble and has secondary porosity so that it cannot store water for a long time. Rainwater that flushes the karst area directly falls to the bottom of the water-saturated zone and then flows through cracks and large passageways (caves) such as canals to springs exit points or is directly dumped into the sea, only a small amount flows on the surface. Until now, it has the potential value of environmental services (environmental services) and ecological services both in the karst area itself and in the non-karst area which is used as a buffer zone. The underground river system that is formed in the karst area provides benefits to the environment around the karst area and even the community as a provider of clean water needs that are perennial / flowing throughout the season. Characteristics of natural resources in the Karst Gombong area of Jatijajar Village have resource characteristics in the form of direct use, namely from the existence of a water hydrological system from the karst area which consists of the value of water resource utilization which is used to meet household needs, the value of water resources for lowland rice farming, and Water Resources from underground rivers in the karst area are 15 springs. The total economic value of the potential use of existing resources in the Gombong Karst Gombong area of Jatijajar Village is IDR 87,616,789,519 in one year. The magnitude of this value is the value of natural and environmental resources from the direct use of the availability of natural resources to the community. These values will be lost if the karst area is damaged either from mining activities or changes in environmental functions. In fact, this value will be a value that must be spent by the community in order to compensate for the loss of potential natural resources in the karst area","PeriodicalId":33119,"journal":{"name":"Jurnal Social Economic of Agriculture","volume":"22 1","pages":""},"PeriodicalIF":0.0000,"publicationDate":"2022-06-24","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"1","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"Jurnal Social Economic of Agriculture","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.26418/j.sea.v11i1.43542","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
引用次数: 1
摘要
根据能源和矿产资源部第3043 K / 40 / MEM / 2014号法令和关于2011 - 2013年克布门县RTRW的2012年第23号地区条例,Jatijajar村被列入贡峰喀斯特地区。喀斯特是碳酸盐岩(CaCO3)穿过可利用的地质空间和时间后形成的岩溶作用过程的景观。由于石灰岩的物理性质,容易溶解,具有次生孔隙,不能长期储水,因此溶蚀碳酸盐岩具有独特的水文条件。冲刷喀斯特地区的雨水直接落到饱和带底部,然后通过裂缝和运河等大通道(洞)流向泉水出口点或直接排入大海,只有少量在地表流动。迄今为止,无论是在喀斯特地区本身,还是在作为缓冲带的非喀斯特地区,都具有潜在的环境服务(环境服务)和生态服务价值。在喀斯特地区形成的地下河系统为喀斯特地区周围的环境,甚至社区提供了一年四季都需要的清洁水。Jatijajar村喀斯特贡峰地区自然资源特征具有直接利用形式的资源特征,即喀斯特地区存在由满足家庭用水需求的水资源利用价值、用于低地水稻种植的水资源价值、喀斯特地区地下河水资源15泉组成的喀斯特地区水水文系统。Jatijajar村贡峰喀斯特贡峰地区现有资源的潜在利用价值为一年87,616,789,519印尼盾。这一价值的大小是指自然资源和环境资源从直接利用到社会可利用的自然资源的价值。如果喀斯特地区因采矿活动或环境功能的变化而受到破坏,这些价值就会丧失。事实上,为了补偿喀斯特地区潜在自然资源的损失,这个价值将是社区必须花费的价值
Valuasi Ekonomi Kawasan Karst Desa Jatijajar Kecamatan Ayah Kabupaten Kebumen
Jatijajar Village which is included in the Gombong karst area in accordance with the Minister of Energy and Mineral Resources Decree No. 3043 K / 40 / MEM / 2014 and confirmed by the Kebumen Regency Regional Regulation No. 23 of 2012 concerning RTRW of Kebumen Regency for 2011 - 2013. Karst is a landscape of the karstification process of carbonate rock (CaCO3) which is deposited after passing through the available geological space and time. Karst has a distinctive hydrological condition due to the dissolution of carbonate rock due to the physical properties of limestone which is easily soluble and has secondary porosity so that it cannot store water for a long time. Rainwater that flushes the karst area directly falls to the bottom of the water-saturated zone and then flows through cracks and large passageways (caves) such as canals to springs exit points or is directly dumped into the sea, only a small amount flows on the surface. Until now, it has the potential value of environmental services (environmental services) and ecological services both in the karst area itself and in the non-karst area which is used as a buffer zone. The underground river system that is formed in the karst area provides benefits to the environment around the karst area and even the community as a provider of clean water needs that are perennial / flowing throughout the season. Characteristics of natural resources in the Karst Gombong area of Jatijajar Village have resource characteristics in the form of direct use, namely from the existence of a water hydrological system from the karst area which consists of the value of water resource utilization which is used to meet household needs, the value of water resources for lowland rice farming, and Water Resources from underground rivers in the karst area are 15 springs. The total economic value of the potential use of existing resources in the Gombong Karst Gombong area of Jatijajar Village is IDR 87,616,789,519 in one year. The magnitude of this value is the value of natural and environmental resources from the direct use of the availability of natural resources to the community. These values will be lost if the karst area is damaged either from mining activities or changes in environmental functions. In fact, this value will be a value that must be spent by the community in order to compensate for the loss of potential natural resources in the karst area