首页 | 本学科首页   官方微博 | 高级检索  
相似文献
 共查询到16条相似文献,搜索用时 171 毫秒
1.
采用外源硒加入土壤中得到硒污染土壤,6种有效硒的浸提剂NaHCO3、KH2PO4、K2SO4、EDTA、AB-DTPA和DTPA+TEA+CaCl2的最佳浸提时间和土液比进行了筛选,并通过盆栽试验对所选择的土壤有效硒浸提剂进行生物学校验,以找出石灰性土壤有效硒提取适宜的浸提剂及其浸提条件。结果表明,NaHCO3、KH2PO4、K2SO4、EDTA、AB-DTPA和DTPA+TEA+CaCl26种浸提剂有效硒浸提量都随着浸提土液比的减小而增大,且随浸提时间的增长而增大。其中NaHCO3和KH2PO4最佳土液比为1/15,振荡时间90min;K2SO4和AB-DTPA的最佳土液比为1/15,振荡时间60min;EDTA和DTPA+TEA+CaCl2的最佳土液比则为1/20,振荡时间30min。6种浸提剂在各自最佳的提取条件下提取的土壤有效硒量与白菜地上部分硒含量达极显著正相关,但土壤有效硒的提取量以DTPA+TEA+CaCl2及K2SO4最少,只占KH2PO4、AB-DTPA及EDTA提取量的14%~48%,故不适用于作为石灰性土壤有效硒的提取剂。NaHCO3适用于土壤硒含量高于5mg·kg^-1的石灰性土壤有效硒提取。KH2PO4、AB-DTPA及EDTA3种浸提剂既可提取土壤中水溶态硒,亦可提取部分的吸附态硒,提取硒数量较多,过程简单,重复性好,都可作为石灰性土壤有效硒提取的浸提剂。  相似文献   

2.
采用盆栽实验及石墨炉原子吸收光谱法测定,比较了HOAc、MgCl2、NH4OAc、EDTA和EDTA-NH4OAc等5种浸提剂在不同提取时间、不同土液比下对土壤中有效态钒的提取效果。实验表明,不同浸提剂对土壤有效态钒的提取率明显不同,提取率均随土壤钒含量的升高而升高。浸提剂对土壤有效钒的提取率顺序依次为HOAcMgCl2NH4OAcNH4OAc-EDTAEDTA,其中0.05 mol L-1 EDTA的浸提效率最高,最大提取率61.1%。最佳提取条件为:平衡时间60 min、土液比1∶10。将拟定的提取方法用于玉米盆栽土壤中有效态钒的提取,土壤中有效态钒量与玉米根、茎叶中钒含量存在极显著的相关性,相关系数达0.9742和0.9497,故EDTA提取的有效态钒能很好地用于评价土壤中钒的植物可利用性。  相似文献   

3.
土壤有效态重金属提取剂选择的研究   总被引:16,自引:0,他引:16  
李亮亮  张大庚  李天来  依艳丽  臧健  胡睿 《土壤》2008,40(5):819-823
利用5种不同的土壤重金属浸提剂,研究了土壤有效态重金属含量与玉米重金属含量的关系,并提出了一种新的土壤有效态重金属的浸提剂。结果表明:0.1mol/L HCl,0.05mol/L EDTA-2Na,0.1mol/L CaCl2,0.1mol/L HAc-NaAc,0.05mol/L DTPA提取的化学有效态重金属与玉米根、茎、叶中重金属Cu、Zn、Cd、Pb大部分呈显著或极显著相关,但各化学提取剂提取的有效态Zn、Cu与玉米籽粒Zn、Cu的相关性较差。利用柠檬酸-酒石酸为提取剂提取的重金属含量与玉米籽粒中重金属的含量有着相对较好的相关性,是一种预估玉米籽粒中重金属含量的较好办法。  相似文献   

4.
比较了O lsen(0.5 mol L-1NaHCO3)和B ray-1(0.03 mol L-1NH4F-0.025 mol L-1HC l)提取剂土水比1∶4和1∶20(W/V),对我国5种类型旱耕地土壤(pHKC l3.3~7.4)无机磷(Pi)和有机磷(Po)及外加正磷酸盐态无机磷的提取效应。结果表明,以O lsen提取剂土水比1∶20对土壤Pi和Po的提取效果最佳,其测定结果是评价土壤磷素供应能力(有效磷)和活性有机磷含量较为适宜的指标。测定的土壤大多数(占60%)磷素供应能力较差(O lsen-Pi为4.2~14.0mg kg-1),应适当加强其磷素的投入。测定的土壤活性有机磷(O lsen-PO)含量为1.4~37.9 mg kg-1,占土壤全磷的0.2%~15.8%,大多数(75%)土壤占1%~6%。采用O lsen提取剂时土壤外加Pi的固定率随土水比减小而增高,当土水比1∶4提取时,酸性和强酸性(pHKC l3.3~5.5)土壤对外加Pi的固定率达40%~86%,据此推测实际田间条件下土壤对外加Pi的固定率更大。表明酸性和强酸性旱耕地土壤对外加Pi具有强烈的固定作用。  相似文献   

5.
准确评价汞(Hg)在土壤中的有效性对预测污染土壤中Hg的潜在生态风险及其环境质量标准的修订具有十分重要的意义。本研究通过稳定同位素202Hg稀释技术及同位素交换动力学方法(IEK)分析红壤和潮土中同位素可交换Hg含量(E值)及同位素可利用态Hg含量(Ea),并与4种单一提取法和1种连续提取法(改进的BCR法)获得的土壤有效态Hg含量进行比较。结果表明,外源稳定同位素202Hg加入土壤后,红壤和潮土的悬浮液中同位素交换均在24 h后达到稳定状态。同位素交换动力学方程对悬浮液中同位素比值及土壤同位素交换态含量Et值的变化有比较理想的拟合效果,红壤三个间段的E值(E1 min、E1 min-24 h和E24 h)及所占全量的比例均高于潮土。两种土壤Ea(为E1 min与E1 min-24 h之和)所占全量的比例为38%~60%,显著高于单一提取法中提取率最高的0.03%TGA-1/15 mol L-1Na2HPO4(10%~15%)及连续提取的∑BCR(20%~27%,为酸可提取态、还原态和氧化态占全量之和),这表明与化学方法相比较,用土壤同位素可利用态Hg含量(Ea)作为土壤中有效态Hg含量的表征可能偏高,原因可能与外源同位素被土壤固持及土壤悬浮液的性质有关。  相似文献   

6.
稻菜轮作制下土壤有效态汞提取剂和提取条件研究   总被引:1,自引:0,他引:1  
选择长三角地区代表性人为耕作土——青紫泥为研究对象,通过网室盆栽和室内试验,选用CaCl2,HCl,DTPA(二乙烯三胺五乙酸)和NH4OAc共4种提取剂,研究了水稻—小白菜—萝卜作物轮作系统中土壤有效态汞提取剂的选择与提取条件的优化问题。结果表明,不同提取剂提取的有效态汞含量随提取时间的延长而逐渐增加,30min可作为提取剂提取土壤有效态汞的最佳平衡时间;随土水比的减小,提取剂提取的土壤有效态汞量明显提高,1∶5为较适宜的土水比;不同提取剂的提取能力不同,对供试土壤,提取剂提取能力的大小顺序为:CaCl2>HCl>NH4OAc>DTPA。提取剂提取的土壤有效态汞量之间存在显著正相关,其中CaCl2和NH4OAc之间相关性最高;在土壤—水稻系统和土壤—萝卜系统中作物可食部位汞含量与提取剂提取的土壤有效态汞含量之间存在显著正相关关系,但在土壤—小白菜系统中相关性不强。综合分析,确定CaCl2为供试土壤汞有效态的最佳化学提取剂。  相似文献   

7.
为正确表征云南文山三七种植区土壤中植物可利用态砷,选取NaH2PO4(0.5mol·L-1)、H2O、H3PO4(0.2mol·L-1)、EDTA(0.0625mol·L-1,pH=7)、NH4C(l1.0mol·L-1)和(NH4)2SO(40.05mol·L-1)6种提取剂,比较了它们对土壤中砷的提取效果,及其所提取的砷与三七植株各部位砷含量之间的相关关系。结果表明,NaH2PO4、H3PO4和(NH4)2SO4这3种提取态砷与土壤总砷呈极显著正相关,相关系数分别为0.8359、0.8177和0.8810。NaH2PO4和H3PO4的提取效率较高,平均提取效率分别为6%和11%;而(NH4)2SO4提取效率较低,平均仅为0.084%。NaH2PO4和(NH4)2SO4提取态砷与三七主根、须根和茎部砷含量呈显著正相关,H3PO4提取态砷与三七主根和须根砷含量呈显著正相关。综合考虑认为NaH2PO(40.5mol·L-1)是最佳提取剂,H3PO(40.2mol·L-1)提取剂次之,这两种提取剂均可较好地表征土壤中砷的三七可利用性。  相似文献   

8.
酸性土壤水溶性氟浸提方法的研究   总被引:2,自引:0,他引:2  
蒋倩  韩勇  孙晓丽  华建峰  倪俊 《土壤》2012,44(1):140-143
本文比较研究了振荡、超声、沸水浴和烘箱4种浸提酸性土壤水溶性氟的方法,然后采用离子色谱法对浸提液进行测定,并通过对测定数据进行统计与方差分析来确定最佳浸提方式。结果显示,水土比5:1,浸提时间20 min、温度60℃是振荡法与超声法浸提酸性土壤水溶性氟含量的最佳条件。在此条件下,振荡法与超声法浸提的土壤水溶性氟含量无显著差异,标准偏差均小于0.3%。超声法浸提的酸性土壤水溶性氟含量显著高于各自最佳处理条件下的沸水浴法与烘箱法浸提的水溶性氟含量。在离子色谱测定水溶性氟过程中,质量控制样品均在1倍标准偏差范围内。因此,采用离子色谱法测定超声法或振荡法浸提的酸性土壤水溶性氟是一种可行的、准确的试验方法,特别对于批量土壤样品的测定具有重要意义。  相似文献   

9.
为了探讨0.01mol L-1 CaCl2和0.02mol L-1 SrCl2提取土壤氮、钾能力的差异,用0.01mol L-1 CaCl2和0.02mol L-1 SrCl2提取14个土壤样品,再分别用流动分析和火焰光度法测定提取液中的硝态氮和亚硝态氮之和和钾的含量,以1mol L-1 KCl和1mol L-1中性醋酸铵提取液作为无机氮和钾的对照提取剂,同时选择部分土壤样品用盆栽试验测定提取数量与土壤氮、钾有效性的关系。结果表明,两种方法和对照方法提取氮和钾数量的相关性均达到p<0.01水平,对照提取剂、0.01mol L-1 CaCl2和0.02mol L-1 SrCl2对于14个土壤的硝态氮和亚硝态氮之和提取含量平均值分别为13.36、15.33和26.62mgkg-1,14个土样的提取钾含量的平均值分别为120.4、33.58和54.24mgkg-1。盆栽试验结果表明,对照提取剂和0.01molL-1CaCl2和0.02molL-1SrCl2提取氮的数量与植物吸氮量的相关性达到p<0.05显著水平,钾的相关性达到p<0.01显著水平。与对照提取剂的氮、钾分别提取相比,SrCl2和CaCl2提取剂均可大大降低样品提取中试剂费用。以上结果表明,0.01mol L-1 CaCl2和0.02mol L-1 SrCl2提取对土壤氮和钾的提取能力均可反映土壤硝态氮和亚硝态氮、有效钾的含量和供应能力,而提取能力以0.02mol L-1 SrCl2为高。  相似文献   

10.
不同浸提剂对海南稻田土壤有效硒浸提效果比较   总被引:4,自引:1,他引:3  
耿建梅  王文斌  罗丹  吴露露  唐树梅 《土壤》2010,42(4):624-629
在海南定安县采集硒(Se)含量水平不同的3个代表性稻田土壤,结合水稻幼苗盆栽试验与黑麦草幼苗培养试验,用H2O(pH4.5)、0.5mol/LNaHCO3(pH8.5)和0.1mol/LKH2PO4三种浸提剂进行海南稻田土壤有效Se浸提效果的比较研究。结果表明:3种浸提剂提取的有效Se与植株累积的Se都呈极显著正相关,但H2O的提取能力弱。在水稻幼苗试验中,0.1mol/LKH2PO4与0.5mol/LNaHCO3相比,浸提时间短,测定的土壤有效Se的平均变异系数较小,且与水稻植株累积Se的相关系数较大,因此海南稻田土壤有效Se测定宜选0.1mol/LKH2PO4。  相似文献   

11.
以冬小麦为试验对象,采用盆栽试验,研究了不同有机肥、不同外源汞施用量对土壤和小麦的汞污染、迁移和累积的影响。结果表明,随着汞施入量的增加,土壤全汞和有效汞含量逐渐增加,使小麦吸收汞增加。在小麦整个生育期,土壤有效汞与小麦根、茎叶、籽粒吸收的汞之间呈极显著正相关性。随着有机肥施用量的增加,土壤有效态汞含量逐渐减少,继而降低小麦对汞的吸收。相关分析表明,有机肥施用量与土壤有效汞呈显著负相关。有机肥对土壤有效汞的抑制效果以低汞高有机肥处理效果最为显著,苗期达到58.94%,收获期达到62.29%。有机肥施用量与苗期低汞处理下小麦茎叶和根部汞含量呈显著负相关,与收获期的所有汞处理下小麦茎叶、根部和籽粒汞含量呈极显著或显著负相关,在低汞处理,施用有机肥完全抑制了土壤中汞向籽粒中转移。所有处理小麦各器官汞含量的分布规律为根〉茎叶〉籽粒。  相似文献   

12.
通过对重金属污染土壤的萃取实验,比较了HCl、Na2S2O3、CaCl2 3种常用无机萃取剂对重金属Ph和cd的萃取效果,并通过改变萃取条件(萃取剂浓度、时间、固液比、萃取次数和温度),以期找到各种萃取剂达到最大萃取效率时所需的萃取条件。结果表明,萃取剂浓度对于萃取效率的影响最大,随着浓度的提高,3种萃取剂对Ph、Cd的去除作用增强;固液比和萃取次数对Ph、Cd的去除率也有较大的影响;时间对两金属的去除率也有一定的影响,但在本实验条件下,达到萃取平衡所需时间很短;温度对萃取效率的影响很小。本实验中,HCl去除Pb、Cd的能力远远大于其他两种萃取剂。对Cd进行萃取时,需增加萃取次数才能达到较好的萃取效果。  相似文献   

13.
Abstract

A study was conducted with the purpose of comparing the efficiency of Mehlich 1, Mehlich 3, and calcium acetate lactate (CAL) extractants for the deter‐ mination of available phosphorus (P) and exchangeable cations [potassium (K), calcium (Ca), magnesium (Mg), and sodium (Na)] on 22 Ethiopian and 10 German agricultural soils. The Olsen and NH4OAc extractants were used as standards against which P and exchangeable cations values were compared. Results showed that, in general, highly significant correlations were found between all of the methods for available P and exchangeable cations determination on the Ethiopian soils. The highest correlation was, however, found with the Mehlich 3 extractant. On the ten soils from Germany, the Olsen method did not give significant cor‐ relation with the CAL method for P determination. The CAL and Mehlich 3 extrac‐ tants were also not good indicators of Na availability when compared with the NH4OAc method. It can be generalized that the Mehlich 3 is a suitable extractant for P, K, Ca, Mg, and Na in Ethiopian soils, but further study is recommended to confirm these findings under field conditions.  相似文献   

14.
Abstract

Simultaneous extraction of nutrients using ammonium bicarbonate–diethylene triamine penta acetic acid (ABDTPA) extractant has been successful for highland soils, but its potential for lowland soils is still uncertain. This study evaluated the suitability of ABDTPA extractant to determine available phosphorus (P), potassium (K), sodium (Na), calcium (Ca), magnesium (Mg), iron (Fe), manganese (Mn), zinc (Zn), and copper (Cu) in lowland rice soils of Sri Lanka. Available nutrients were analyzed both by conventional and ABDTPA methods, using the original ABDTPA (1∶2 soil–extractant) method as well as a modified (1∶4 soil–extractant) method. Conventional methods tested were Olsen, Bray 1, and FeO strip for available P; neutral NH4OAc extraction for exchangeable Ca, Na, K, and Mg; and DTPA extraction for available Zn, Cu, Fe, and Mn. Nutrient content and uptake by plants were determined by a pot experiment with rice (Oryza sativa). Nutrients extracted by the conventional methods and ABDTPA methods correlated well, in general, for all nutrients. Highly significant correlations were observed between plant uptake and extractable nutrients by 1∶2 and 1∶4 ABDTPA methods for P (r=0.85***and 0.73***, respectively), K (r=0.79*** and 0.66***, respectively), Na (r=0.86*** and 0.78***, respectively), Zn (r=0.66*** and 0.60***, respectively), Mn (r=0.72*** and 0.84***, respectively), and Fe (r=0.74*** and 0.68***, respectively). Calcium and Mg extracted by ABDTPA showed a poor relationship with their respective plant uptake. The ABDTPA method was as effective as or even better than the conventional methods in evaluating fertility status of lowland rice soils with respect to most nutrients. Replacing the conventional methods by the single ABDTPA multielement extractant will reduce the time and cost of soil analysis.  相似文献   

15.
Abstract

Acid extractants were found to be a problem when determining phosphorus in some soils especially in soils with a higher content of carbonates. Carbonate content, soil pH or extractable calcium cannot exactly predict the behavior of a particular soil. On the other hand, measurement of pH after extraction reflects the ability of soil to change the properties of an extractant. The objective of this study was to find the relationships between pH changes during the extraction and the extraction of phosphorus for Mehlich 3, Mehlich 2, CAL, and Egner extractants. Twelve soil samples from various regions of the Czech Republic were taken for investigation. The pH/KCl of the samples was in the range 4.9–7.3. Calcium carbonate was added into the extracting bottles to the soil samples before extraction. The CaCO3/soil ratio was from 0 to 0.5. The content of phosphorus and pH were measured in filtrates after extraction. The ratio P1 =Pmeas /PO was calculated for all measurements, all additions of calcium carbonate and all soils. Pmeas is the measured value of phosphorus after extraction with the addition of calcium carbonate and Po is the value of phosphorus determined after the extraction without addition of calcium carbonate. The ratio Pr reflects the changes in the extractability of phosphorus and it is independent of the absolute content of phosphorus in soil. The relationships between Pr and pH after extraction for CAL, Mehlich 2, and Mehlich 3 extractants were found. No such relationship was found for Egner extractant. Correction equations (x=pH after extraction, y=Pr):  相似文献   

16.
Deficiency of sulfur (S) is becoming widespread in the rainfed systems of India, and there is increasing need for diagnosing the deficiency. Calcium chloride and Ca phosphate are commonly used for extracting available S in soils. Because of cost and the ease of availability locally, we prefer using Ca chloride as an extractant over Ca phosphate, for extracting available S. However, there is paucity of data on the comparative evaluation of the two extractants to extract available S, especially in soils having a wide range in natural pH (from acidic to alkaline range). It is recognized that soil pH plays a dominant role in the adsorption–desorption and extractability of sulfate‐S in soils. We compared the extraction of S by Ca chloride and Ca phosphate in 86 Indian soils having a wide range in pH (4.5 to 10.6). Sulfur in the extracts was determined by ICP‐AES. Considering all the 86 soil samples tested, there was an excellent agreement between the values of extractable S determined by using the two extractants (r = 0.96, p < 0.001). However, the correlation coefficient (r) between the values of extractable S by the two reagents, although highly significant, varied among the groups of soil samples according to the range in soil pH. The highest correlation coefficient (r = 0.99, p < 0.0001, n = 17) was found for soils with pH in the alkaline range (8.5–10.6), and the lowest correlation coefficient (r = 0.71, p < 0.0001, n = 58) was obtained with a set of soil samples with pH in the acidic range (4.5–6.5). For soil samples having pH in the near‐neutral range (6.7–7.3), an excellent agreement was observed (r = 0.93, p < 0.0001, n =11) between the extractable‐S values obtained by the two extractants. While Ca phosphate extracted higher amount of S compared to Ca chloride in soil samples with pH in the acidic range, the two extractants were equally effective for soil samples with pH in the neutral or alkaline range. Our results suggest that for most of the soils in the semiarid tropical regions, which have pH in the neutral to alkaline range, Ca chloride can replace Ca phosphate as an extractant for removing available S in such soils.  相似文献   

设为首页 | 免责声明 | 关于勤云 | 加入收藏

Copyright©北京勤云科技发展有限公司  京ICP备09084417号