浅谈人工挖孔桩

分析了人工挖孔桩施工中遇到的问题(如水、溶洞、淤泥层、流砂),并提出了相应的处理措施。     

岩溶洞穴长度空间形态的分形研究

为使洞穴的研究从定性走向定量,应用分形理论给出洞穴长度定义,进一步明确洞穴长度的物理意义,通过对洛塔洞穴系统２２个洞穴长度分形维数的计算,分析了洞穴长度维数与岩性的关系。     

磁法勘探解析延拓算法在探测地下洞穴中的应用

通过对某地下防空洞探测的磁异常数据的研究,以解析延拓的方法作了向上与向下的延拓．结果表明：解析延拓算法的研究,对确定地下异常体与更精确圈定其几何形态是非常有效的．     

溶洞上方条形基础地基极限承载力有限元分析

针对岩溶地区典型围岩条件,采用有限元方法对岩溶地区条形基础下溶洞顶板稳定性进行分析计算,得出溶洞顶板跨度、顶板厚度不同时地基的极限承载力;分析了极限承载力与各影响因素之间的关系,给出了溶洞顶板安全厚度的有限元分析结果.研究结果表明:溶洞顶板厚度在一定范围内,当顶板跨度从B增加到4B时,地基极限承载力降低1/3;当跨度一定时,地基极限承载力随溶洞顶板厚度增加而增加;当顶板厚度达到安全厚度时,溶洞对地基极限承载力影响可以不计.     

Holocene lake deposits of Bosten Lake, southern Xinjiang, China

A 9.25-m-long sediment core from Bosten Lake,Xinjiang, provides detailed information about changes in the water budget and biological acticity over the last 8400 cal-endar years. The chronology is constructed from six AMS radiocarbon dates on the terrestrial plant remains. Based onanalyses of TOC, CO3, detrital compounds and biogenic SiO2,lake level fluctuations and periods of remarkably-negative water budget appeared at 8.4-8.2 cal ka, 7.38-7.25 cal ka,5.7-5.5 cal ka, 3.7-3.4 cal ka and 3.3-2.9 cal ka, respec-tively. As they are in-phase with low lake levels at Sumxl Co and Bangong Co in western Tibet Plateau and with paleo-lakes in Inner Mongolia, a climate-induced change to some-what drier and warmer conditions is inferred. A further drop in lake level after 1320 AD of about 200 yr duration may heattributed to a negative water balance prior to the main phase of the Little Ice Age. Deep and stable lake phases of 1500 yr and 1800 yr duration at 7.2-5.7 cal ka and 5.5-3.7cal ka coincide with maximum moisture during the Holocene Megathermai in China. The long term trend towards aridity since about 4.3 cal ka can dearly be recognised. The reduced water budget of Bosten Lake from 640-1200 AD may be attributed to local effects.     

广西洞穴金线鲃一新种--九圩金线鲃

描记广西河池市九圩镇一地下河中的金线鲃属一新种，以标本采集地命名为九圩金线鲃，新种．Sinocyclcheilus jiuxuensis Li et Lan,sp．nov.新种与分布区相邻的半盲金线鲃S.Halfibindus Li et Lan和高肩金线鲃S．altishouldeus Li et Lan相近，但新种背鳍分枝鳍条为7，鳃耙7～9和甲须纤弱等特征可与半盲金线鲃区别．新种头后平缓上升而不是急剧隆起；侧线鳞47～49，头长为眼间距的3．93～4．43(4．20)倍，可与高肩金线鲃区别。     

剑川石窟档案文献资源的开发利用

以大理剑川石窟档案文献为例,论述了如何在网络环境下,充分有效地开发和利用剑川石窟档案文献资源,努力为民族地方文献资源的建设和发展增添新的亮点.     

浅析岩溶洞穴旅游的可持续性发展--以重庆武隆芙蓉洞为例

文章借鉴旅游可持续发展的研究成果,初步探讨了岩溶洞穴旅游可持续发展的概念内涵,提出了发展的目标;分析了岩溶洞穴旅游可持续发展的方法,包括负面影响分析、环境容量的计算、指标体系的建立和评价方法等。     

Characteristics of strontium isotopes and their implications in the Qixing Cave of Guizhou,China

The strontium isotopic compositions (87Sr/86Sr) of samples including soils, bedrock, soil waters, drip waters and their corresponding speleothems in the Qixing Cave (QXC), Guizhou Province, China, were systemically measured and analyzed. The results indicate that there are significant Sr isotopic differences among samples. The mean 87Sr/86Sr ratios in drip water for the samples 1#, 4# and 9# were 0.709568, 0.709139 and 0.708761, respectively, which possibly result from different flow paths, residence times, and other hydrogeological processes in the unsaturated zone overlying QXC. Meanwhile, levels of 40.8%, 57.6% and 72.4% of Sr in drip waters for 1#, 4# and 9#, respectively, were derived from bedrock dissolution, which was calculated by the mixture model of the two end-members (soil and bedrock). There is, however, no positive correlation between the relative proportion from bedrock dissolution (δ13C value is 1.8‰) and drip water δ13CDIC values. The mean drip water δ13CDIC value in 1# is the heaviest (–4.5‰) with the lowest contribution rate of bedrock dissolution, whereas the value in 9# is the lightest (–9.3‰) with the highest contribution rate of bedrock dissolution. The proportion from host rock dissolution in 4# is higher than that in 1# and lower than that in 9#, while its mean drip water δ13CDIC value (–8.6‰) is higher than that of 9# and lower than that for 1#. This suggests that the prior calcite precipitation (PCP) processes in the unsaturated zone overlying the cave are responsible for the δ13CDIC value differences between different drip waters, and not bedrock dissolution. Furthermore, this study also demonstrates that the 87Sr/86Sr ratios of speleothems in the 1# and 4# mainly reflect the variation in the relative proportions from the soil system (soil water) and bedrock dissolution overlying the cave. It is, therefore, feasible to use the strontium isotopic signals of speleothems as an indicator for soil chemical weathering intensity, and consequently as a monsoon proxy in the study area.     

微生物对沉积物汞释放影响的实验研究

受污染沉积物汞的释放已成为湖泊水体汞的重要污染源之一.通过沉积物原状柱的室内培育实验,对微生物、氧化还原电位对沉积物汞释放的影响进行了研究.实验表明氧化还原条件和微生物都是沉积物汞释放的重要因素,厌氧条件初期以及微生物的活动都能促进汞的释放.