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首页> 外文期刊>Journal of caves and karst studies: the National Speleological Society bulletin >ENVIRONMENTAL PARAMETERS CONTROLLING STALAGMITE GROWTH IN TROPICAL AREAS: NEW INSIGHTS FROM CAVE MONITORING AT PETRUK CAVE, CENTRAL JAVA, INDONESIA
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ENVIRONMENTAL PARAMETERS CONTROLLING STALAGMITE GROWTH IN TROPICAL AREAS: NEW INSIGHTS FROM CAVE MONITORING AT PETRUK CAVE, CENTRAL JAVA, INDONESIA

机译:控制热带地区石笋增长的环境参数:佩特鲁克洞穴,中爪哇省,印度尼西亚洞穴监测的新见解

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摘要

To elucidate environmental parameters controlling stalagmite growth in tropical areas, we conducted cave monitoring throughout a year in Petruk Cave, central Java, Indonesia. We compared stalagmite growth rate with the cave's environmental parameters, air temperature, drip rate, calcium concentration of the drip waters, and pCO(2)-air. We found a relationship where stalagmite growth rate is fast (slow) when pCO(2)-air is low (high) during dry (rainy) season, suggesting that pCO(2)-air controls stalagmite growth. Note that this is a first study that reports that dramatic pCO(2)-air reduction occurring during dry season in a tropical cave controls stalagmite growth. Additionally, we discuss the mechanism of pCO(2)-air fluctuation. Monitoring results show that pCO(2)-air fluctuation is divided into two phenomena: seasonal fluctuations and daily fluctuations. Dramatic pCO(2)-air reduction during the dry season is likely to result from a decline of plant activity due to little rainfall. On the daily scale, pCO(2)-air reached to the minimum around 6 a.m. and maximum around 2-4 p.m., although it is not obvious whether this is due to plant activity or cave ventilation. Also, dynamic pCO(2) pCO(2)-air reduction was observed following cave ventilation driven by the sudden drop of outside air temperature due to a downburst during severe rain. This suggests that heavy rainfall in short duration is also one factor that controls cave ventilation and pCO(2)-air.
机译:为了阐明控制热带地区石笋生长的环境参数,我们在印度尼西亚中部爪哇省佩特鲁克洞穴的一年内进行了洞穴监测。我们将石笋生长速率与洞穴的环境参数,空气温度,滴度,滴水水钙浓度进行比较,以及PCO(2)--Air。我们发现了一种关系,当干燥(雨水)季节PCO(2) - 空气(高)时注意,这是第一研究,报告在热带洞穴中的干燥季节期间发生戏剧性的PCO(2) - 在热带洞穴控制中进行戏剧性的增长。此外,我们讨论了PCO(2) - 空气波动的机制。监测结果表明,PCO(2) - 公废波动分为两种现象:季节性波动和日常波动。在干燥季节期间,在干燥季节期间减少戏剧性PCO(2)减少可能因降雨而导致植物活动的下降。在日常规模上,PCO(2) - 达到最低约6周,最大左右2-4左右。虽然这是由于植物活动或洞穴通风是不明显的。此外,在严重雨中由于突然暴风雨引起的突然间空气温度驱动的洞穴通风后观察到动态PCO(2)-AIR减少。这表明短暂的降雨量也是控制洞穴通风和PCO(2)的一个因素。

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