首页> 外文期刊>International Biodeterioration & Biodegradation >Investigating physicochemical sediment conditions at decayed wooden pile foundation sites in Amsterdam.
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Investigating physicochemical sediment conditions at decayed wooden pile foundation sites in Amsterdam.

机译:调查阿姆斯特丹腐烂的木桩基础站点的理化沉积物状况。

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摘要

For thousands of years wooden foundation piles have been widely used along coastal areas and river sites to stabilise urban settlements. Recent investigations, however, indicate that colonising bacteria can destroy the wood even below the groundwater level under low-oxygen conditions and cause severe strength loss over unexpectedly short periods. Existing knowledge of the species involved and the conditions required for growth of the bacteria is insufficient. The aim of this study was to characterise physicochemical site conditions by taking oxygen, redox potential, and chemical measurements at wooden foundation sites in Amsterdam, The Netherlands, that showed different decay intensities but had comparable sediment profiles. Oxygen (optode principle), redox potential (platinum electrodes), and groundwater table measurements were conducted biweekly over a year. Sediment solution was sampled every three months and analysed for pH, conductivity, total and dissolved carbon and nitrogen, NH< sub>4+, NO< sub>3-, SO< sub>42-, PO< sub>43-, Cl-, and major cations. Oxygen and redox measurements indicated oxygen-free conditions at both sites examined, but the water surrounding piles exhibited significantly higher total nitrogen concentrations at the site showing light decay. As other simultaneous investigations revealed a positive correlation between the nitrogen content in wooden pile samples and the decay intensities, we conclude that nitrogen might be a key factor in the decay process. We hypothesise that concentration gradients between sediment and wood matrix may control the decay intensity.
机译:几千年来,木制地基桩已广泛用于沿海地区和河流站点,以稳定城市居民点。然而,最近的研究表明,在低氧条件下,定植细菌甚至会破坏木材,甚至低于地下水位,并在意想不到的短时间内造成严重的强度损失。对涉及的物种和细菌生长所需条件的现有知识不足。这项研究的目的是通过对氧气,氧化还原电势和在荷兰阿姆斯特丹的木制地基进行化学测量来表征理化现场条件,该物理基础显示出不同的衰减强度但具有可比的沉积物剖面。在一年中每两周进行一次氧气(光电原理),氧化还原电势(铂电极)和地下水位测量。每三个月对沉积物溶液进行一次采样,分析其pH,电导率,总溶解碳和氮,NH 4 +,NO 3 -,SO 4 2-,PO 4 3-,Cl-和主要阳离子。氧气和氧化还原的测量结果表明,在所检查的两个位置处都处于无氧状态,但是桩周围的水在该位置处显示出明显更高的总氮浓度,显示出光衰减。由于其他同时进行的调查显示,木桩样品中的氮含量与衰减强度之间呈正相关,因此我们得出结论,氮可能是衰减过程中的关键因素。我们假设沉积物和木材基质之间的浓度梯度可以控制衰减强度。

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