Turning Volcanic Ash into Fertile Soil: Farmers’ Options in Coffee Agroforestry After the 2014 Mount Kelud Eruption

R. Ishaq, D. Saputra, R. R. Sari, D. Suprayogo, W. Widianto, C. Prayogo, K. Hairiah
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引用次数: 9

Abstract

Post eruption land reclamation consists of hoeing, mixing volcanic ash with soil, adding external organic and/or in-organic fertilizers and making infiltration-pits (‘rorak’). This study, after the 2014 eruption of Kelud volcano, aimed to evaluate: (a) soil physico-chemical fertility post eruption, (b) impact of organic inputs interacting with ash in infiltration pits on soil C and N underneath (1 st experiment), (c) biomass loss (decomposition) of local biomass ( Trema orientalis and Parasponia andersonii ) in a coffee agroforestry system (2 nd experiment). Measurements in the ash-affected (+Ash) Tulungrejo-village (Ngantang-Malang district) were contrasted with an area without recent ash deposits (-Ash) in Krisik (Gandusari-Wlingi district). The 1 st experiment (-Ash site) treatments did not lead to statistically significant influences on soil conditions just below the infiltration pits during 12 weeks of monitoring. The 2 nd experiment quantified rate of biomass loss from litterbags. In +Ash location, litter half-life time (t 50 ) was 19.5 weeks for coffee or Parasponia as single biomass source to 24 weeks for Coffee+Sengon+Durian. In -Ash location decomposition was slower, with t 50 of 24 weeks for Parasponia to 27 weeks for Coffee+Sengon+Durian biomass. Concentrations of soil NH 4 and NO 3 below the litterbags peaked between 4 to 8 weeks, with nitrification lagging behind on ammonium release.
将火山灰转化为肥沃的土壤:2014年克鲁德火山喷发后农民在咖啡农林业中的选择
火山爆发后的土地复垦包括锄地,将火山灰与土壤混合,添加外部有机和/或非有机肥料以及制造渗透坑(orak)。本研究在2014年克鲁德火山喷发后,旨在评估:(a)火山喷发后土壤理化肥力;(b)有机投入品与入渗坑灰相互作用对地下土壤C和N的影响(第1次试验);(C)咖啡农林复合系统中当地生物量(Trema orientalis和Parasponia andersonii)的损失(分解)(第2次试验)。在受火山灰影响(+火山灰)的tulungrejo -村(Ngantang-Malang地区)的测量结果与Krisik (Gandusari-Wlingi地区)最近没有火山灰沉积(-火山灰)的地区进行了对比。在12周的监测中,第1个试验(-灰点)处理对渗坑下方土壤状况没有统计学上显著的影响。第二个试验量化了垃圾袋生物量的损失率。在+灰分位置,咖啡或山梨作为单一生物质来源的凋落物半衰期(t 50)为19.5周,咖啡+仙根+榴莲为24周。在灰分位置分解较慢,在24周内,parasonia分解为50%,而咖啡+仙根+榴莲生物量分解为27周。4 ~ 8周时,垃圾袋下方土壤nh4和no3浓度达到峰值,硝化作用滞后于铵态氮的释放。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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