Effects of different pretreatment methods on grain-size measurement of the north red weathering crust
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摘要: 选取中国北方岩溶区红色风化壳为研究对象,首先用浓度为30%的H2O2去除样品中的有机质,然后用4种不同的前处理方法分别进行处理,其中方法A未用盐酸溶液处理,方法B、C、D均用盐酸溶液分解可能存在的残余碳酸盐和次生游离氧化物,以消除其对机械颗粒可能存在的胶结作用,此外方法C的HCl在煮沸的条件下反应,方法 B的HCl在常温条件下进行,方法D则更改了超声波振荡的时间。本文样品采用Beckman公司生产的LS13320 型激光衍射粒度测试仪进行测量。结果表明,样品前处理方法对中国北方红色风化壳粒度分析结果有影响,不同的前处理方法使样品的粒度值最大产生5%左右的变化;从实验的稳定性上考虑,4种方法的平行试验标准偏差最大达到6.78%。在现有的认识条件下,粒度测量结果的可重复性是最基本的要求。本文认为方法C的测量效果要好于其他方法。Abstract: Liaodong peninsula is located in the north of Sino-Korean paraplatform of which tectonics is relatively mature, an important part of Asian paraplatform. Due to the Yanshan movement, there developed lots of structures, such as folds and faults. The strata such as Cambrian is well exposed. Its main lithologies are limestone, quartzite, slate and sandstone. The Liaodong peninsula is located in the southern end of northeast China, surrounded by seas on three sides, and between the Yalu river and Liaohe river, mainly hilly and mountainous terrain. It belongs to the temperate continental monsoon climate, mean annual temperature is around 10 ℃, and mean annual rainfall is 550-950 mm. Rainfall is mainly concentrated in July and August.In this paper, the design of pretreatment methods is as follows. First of all, the samples are digested with 30% H2O2 to remove organic matter, and then four methods are used for preprocessing. Of them, the method A is not disposed by hydrochloric acid, methods B, C and D are all decomposed by hydrochloric acid solution to remove the residual carbonate and secondary free oxides in order to eliminate the cementation of debris and mineral particles. HCl of method C is in the boiling conditions of the reaction. HCl of method B is under normal temperature conditions, and method D changes the ultrasonic vibration time.There are different pretreatment methods for the samples to test, the purpose of which is to analyze the influence of various methods on particle size measurement. Combined with the laser diffraction particle size analyzer, it can explore the analysis results of particle size and the reason for the difference to recommend the most optimal pretreatment method, which can facilitate further studying on weathering crust in the region of grain-size analysis. The experimental results show that the pretreatment methods have a certain effect on the particle size measurement results of red weathering crust in northern China, and the different pretreatment methods make the grain size of the samples have about 5% rotates. Considering the stability of the experiment, the error of the parallel tests of the 4 methods reaches up to 6.78%. Under the existing recognized conditions, reproducibility of particle size measurement results is the most basic demand to experiments. In this paper method C is better than others (A, B and D).The results in different pretreatment methods reflect the basic characteristics of the weathering crust in particle size distribution. The method mentioned in the paper is suitable for the weathering crust of north China, the other types and regions should be combined with the actual situations in order to obtain a more ideal test result.
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[1] 胡宗杰,颜佳新,韩鸿印.湖泊沉积物粒度分析前处理过程中絮凝现象的消除方法研究[J].湖泊科学,2013,25(2):243-249. [2] 孙有斌,周杰,鹿化煜,等.风化成壤对原始粉尘粒度组成的改造证据[J].中国沙漠,2002,22 (1):16-20. [3] Ducloux J, Guero Y, Sardini P, et al. Xerolysis:a hypothetical process of clay particles weathering under Sahelian climate [J].Geoderma,2002,105(1-2):93-110. [4] White A F, Bium A E, Schulz M S, et al. Chemical weathering rates of a soil chronosequence on granitic alluvium:Ⅰ.Quantification of mineralogical and surface area changes an calculation of primary silicate reaction rates[J]. Geochimica et Cosmochimica Acta,1996,60(14):2533-2550. [5] 冯志刚,王世杰,罗维均,等. 不同前处理方法对红色风化壳粒度测试结果的影响[J].矿物学报,2006,26(1):1-7. [6] 冯志刚,王世杰,刘秀明,等.碳酸盐岩风化壳母岩的不均一性:来自粒度分析的证据[J].成都理工大学学报(自然科学版),2003,30(6):635-643. [7] 王果,林景亮,庄卫民.福建红壤和砖红壤性红壤的发生和分类的探讨[J].土壤学报,1987,24(4):352-360. [8] 王明珠,何园球.我国富铝化土的分类探讨[J].土壤学报,1990,27(2):219-227. [9] 李德文,崔之久,刘耕年.湘桂黔滇藏红色岩溶风化壳的发育模式[J].地理学报,2002,57(3):293-300. [10] 黄英,符必昌,付君蕖,等.昆明玄武岩红土物质组成的剖面特征[J].昆明理工大学学报(理工版), 2000, 25(4):88-92. [11] 梁福源,宋林华,唐涛.石林地区土壤性质与喀斯特洼地发育[J].地理研究,2004,23(3):321-328. [12] 黄振国,张伟强,陈俊鸿,等.中国南方红色风化壳[M].北京:海洋出版社,1996:56-57. [13] 徐树建,杜忠花.激光粒度仪测量风成堆积物粒度的实验研究[J].水土保持研究, 2007,14(2):209-212. [14] 张红艳,鹿化煜,赵军,等.超声波振荡对细颗粒黄土样品粒度测量影响的实验分析[J].沉积学报, 2008,26(3):494-500. [15] 王德杰,范代读,李从先.不同预处理对沉积物粒度分析结果的影响[J].同济大学学报(自然科学版),2003,31(3):314-318. [16] 刘冬雁,李巍然,彭莎莎,等.粒度分析在中国第四纪黄土古气候研究中的应用现状[J].中国海洋大学学报(自然科学版),2010,40(2):79-84. [17] 鹿化煜,安芷生.前处理方法对黄土古土壤粒度测量的影响[J].科学通报,1997,42(23):2535-2538. [18] 鹿化煜.洛川黄土粒度组成的古气候意义[J].科学通报,1997,42(1):66-69. [19] 鹿化煜,苗晓东,孙有斌.前处理步骤与方法对风成红粘土粒度测量的影响[J].海洋地质与第四纪地质, 2002,22(3):129-135. [20] 蒲晓强,钟少军.不同的前处理方法对南黄海沉积物粒度测试的影响[J].海洋地质动态,2009,25(5):15-18. [21] 孙有斌,高抒,鹿化煜.前处理方法对北黄海沉积物粒度的影响[J].海洋与湖沼,2001,32(6): 665-671. [22] 王君波,朱立平.不同前处理对湖泊沉积物粒度测量结果的影响[J].湖泊科学,2005,17(1):17-23. [23] 谢昕,郑洪波,陈国成,等.古环境研究中深海沉积物粒度测试的预处理方法[J].沉积学报,2007,25(5):684-692. [24] 李华勇,潘安定,明庆忠.不同预处理方法对尕海沉积物粒度测试的影响[J].干旱区地理,2011,34(4):621-628. [25] 刘海丽,韩志勇,李徐生,等.不同前处理方法对南方红土粒度测量的影响:以安徽宣城第四纪红土剖面为例[J].海洋地质与第四纪地质,2012,32(2):161-167. [26] 梁永平,王维泰,赵春红,等.中国北方岩溶水变化特征及其环境问题[J].中国岩溶,2013,32(1):34-42. [27] 庞奖励,乔晶,黄春长,等.前处理过程对汉江上游谷地“古土壤”粒度测试结果的影响研究[J].地理科学,2013,33(6):748-754. [28] 熊平生,袁道先,谢世友.我国南方岩溶山区石漠化基本问题进展[J].中国岩溶,2010,29(4):355-362. [29] 李景阳,朱立军.论碳酸盐岩现代风化壳和古风化壳[J].中国岩溶,2010,29(4):349-354.
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