匈牙利洞穴监测:概述

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引用次数: 1

摘要

在这项研究中,已经发表的和新的监测数据汇编自Aggtelek喀斯特的Baradla和b洞穴,来自皮利斯山脉的Vacska洞穴以及布达山的Szemlőhegy和Pálvölgy洞穴。最近的调查(2019-2020)包括监测洞穴内外测量的气候参数(如温度、二氧化碳),以及水滴的化学、微量元素和稳定同位素组成。在巴拉德拉洞穴,研究的重点是稳定同位素组成和滴水的温度测量。Vacska洞穴属于Ajándék-Ariadne洞穴系统,为了进行化学和稳定同位素测量,我们进行了CO2测量和滴水收集。在Szemlőhegy和Pálvölgy洞穴中,测定了6个地点滴落水的化学和稳定同位素组成。这些数据集用于描述所研究的溶洞和喀斯特发生的水文过程,并追踪人为影响。气候学调查显示,CO2浓度的季节性变化与外部温度变化有关,表明洞穴内存在不同的通风机制。此外,还估算了冬季和夏季降水对滴落水的贡献,以评价主要入渗期。这些参数的掌握对控制洞内碳酸盐沉积起着至关重要的作用。因此,本研究编制的数据集可以为基于洞穴的代理解释提供依据。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Cave monitoring in Hungary: An overview
In this study, already published and new monitoring data are compiled from the Baradla and Béke caves in the Aggtelek Karst, from the Vacska Cave in the Pilis Mountains as well as from the Szemlőhegy and Pálvölgy caves in the Buda Hills. Recent investigations (2019–2020) include monitoring of climatological parameters (e.g., temperature, CO2) measured inside and outside the caves, and the chemical, trace element and stable isotopic compositions of drip waters. In the Baradla Cave, the main focus of the investigation was on the stable isotope composition and the temperature measurements of drip water. In the Vacska Cave, which belongs to the Ajándék-Ariadne cave system, CO2 measurements and drip water collection were conducted in order to perform chemical and stable isotope measurements. In the Szemlőhegy and Pálvölgy caves, the chemical and stable isotope compositions of drip waters at six sites were determined. These datasets were used to characterize the studied caves and the hydrological processes taking place in the karst, and to trace anthropogenic influences. Climatological investigation revealed seasonality in CO2 concentration related to outside temperature variation, indicating a variable ventilation regime in the caves. In addition, the contributions of the winter and summer precipitation to the drip water were also estimated, in order to evaluate the main infiltration period. The knowledge of these parameters plays a crucial role in constraining the carbonate precipitation within the cave. Thus, the dataset compiled in this study can provide a basis for the interpretation of speleothem-based proxies.
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来源期刊
Central European Geology
Central European Geology Earth and Planetary Sciences-Geology
CiteScore
1.40
自引率
0.00%
发文量
8
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