Effects of oil palm bunches and coal fly ash on the cation exchange capacity of reclaimed mining soil
			
	
 
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				1
				Program Study of Soil Science, Faculty of Agriculture, Lambung Mangkurat University, Jalan Jenderal Achmad Yani KM 36 Banjarbaru, South Kalimantan 70714, Indonesia
				 
			 
						
				2
				Doctoral Program of Agricultural Science, Faculty of Agriculture, Lambung Mangkurat University, Jalan Jenderal Achmad Yani KM 36 Banjarbaru, South Kalimantan 70714, Indonesia
				 
			 
						
				3
				Center for Post-mining Land Studies, Lambung Mangkurat University, Jalan Jenderal Achmad Yani KM 36 Banjarbaru 70714, South Kalimantan, Indonesia
				 
			 
										
				
				
		
		 
			
			
		
		
		
		
		
		
	
							
					    		
    			 
    			
    				    					Corresponding author
    					    				    				
    					Akhmad Rizalli Saidy   
    					Program Study of Soil Science, Faculty of Agriculture, Lambung Mangkurat University, Jalan Jenderal Achmad Yani KM 36 Banjarbaru, South Kalimantan 70714, Indonesia
    				
 
    			
				 
    			 
    		 		
			
																																					 
		
	 
		
 
 
J. Ecol. Eng. 2025; 26(6):241-250
		
 
 
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ABSTRACT
Cation exchangeable capacity (CEC) is a significant soil chemical property influencing the availability and exchange of cation nutrients in soils. This study aims to quantify the alterations in CEC of reclaimed mining soil (RMS) treated with oil palm bunches (OPB) and coal fly ash (CFA). The experiment was carried out by adding 3 levels of OPB (0, 20, and 40 Mg ha−1) and CFA (0, 50, and 100 Mg ha−1) were counted to RMS. After 15 days of incubation, CEC with other soil chemical characteristics were measured. The results indicated that the application of 40 Mg ha−1 of OPB increased soil CEC from 20.4 cmol kg−1 to 35.6 cmol kg−1, and 100 Mg ha−1 of CFA caused a 25% decrease. These changes in CEC were associated to the fluctuation in number of functional groups due to the addition of OPB and CFA. The results suggested that adding organic matter could initiate a decrease in CEC due to the presence of multivalent cations from ash, thereby increasing net soil CEC.