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1.
Abstract

A greenhouse leaching column study was conducted to compare the effects of surface‐applied langbeinite (LB), phosphogypsum (PG), Ca‐ silicate slag (SS), and calcitic lime (CL) on subsoil Al and growth of alfalfa (Medicago sativa L. ‘Florida 77') in Toula silt loam soil (Typic Fragiudult). Langbeinite was found to be more effective than PG in the reduction of subsoil exchangeable Al, apparently through SO4 2‐‐induced Al precipitation. This study demonstrated that high exchangeable Al levels are not always indicative of Al toxicity in the soil solution phase. The primary factors limiting alfalfa growth in the Toula soil were found to be surface soil pH and Mn toxicity rather than subsoil Al toxicity. The liming materials, SS and CL, effectively corrected the surface soil Mn and pH problems, but had no effect on subsoil chemical properties.  相似文献   

2.
Dilute waters (Ca = 0.3 to 0.8 mg L?1) respond by depressed pH levels throughout the year to existing atmospheric wet deposition of sulphate (20 kg ha?1yr?1).This occurs in southwest Nova Scotia particularly during the cold, wet season when runoff is high. Colored waters of similar Ca levels receiving runoff from peaty catchments exhibit pH values one unit lower (4.7 to 4.1) than those of catchments of similar Ca levels but free from peat deposits (pH > 5.3). In colored streams sulphate and organic anions show opposing cyclic patterns while the negative gran alkalinity is the near mirror image of sulphate. Sulphate anion peaks during the high spring discharge when the organic anion concentration is lowest. Sulphate suddenly drops during the summer months during periods of high evapotranspiration, low water table and runoff, when the concentration of organic anions is highest. Both Al and Fe follow cyclic patterns similar to that of the organic anions while H+ reflects that of the sulphate anion. Hydrogen ion concentration is always higher than that of sulphate in very colored waters, particularly during the summer months when organic anion concentrations are very high. Analysis of data in the tributaries in the Kejimkujik watersheds indicates that while considerable organic acidity is present in colored waters, anthropogenic sulphate further increases the free acidity of these waters, particularly at times of high discharge.  相似文献   

3.
Two adjacent soils with contrasting sulfate sorption were examined in terms of (i) water-soluble and ion-exchangeable Al, Fe, Ca, Mg, K, Mn and Zn, (ii), water- and bicarbonate-extractable sulfate, (iii) Truog-extractable P, (iv) dithionite-extractable Al, Mn and Fe and (v) treatment response to irrigation with simulated acid precipitation. The biomass of 8 year old black spruce saplings growing on the soils, and the distributions of Al, Fe, Ca, Mg, K, Mn, P and Zn within these plants, were also examined. The soils were well to moderately-well drained, with the mineral soil exposed by site preparation prior to planting. The exposed soil underneath individual saplings was treated with acid sulfate solutions (75 mm containing 2 to 50 mg L?1 H2SO4) applied during each of three consecutive growing seasons. The results indicate that Al, much like Fe, Ca, Mn and Zn, accumulated with time in the foliage, but K, Mg and P were highest in young plant tissues. Much of Al and Fe taken up remained in the fine roots. Aluminum uptake increased with the amount of dithionite-extractable Al (free Al oxide) in the soil. Growth of the black spruce saplings was not visibly affected by readily accessed Al in each soil, or by acid irrigation.Instead, growth was restricted by factors other than soil Al and acid irrigation in spite of (i) low soil pH, (ii) high levels of exchangeable Al, and (iii) high levels of Al in fine roots. Sulfate retention across and within the two soils was positively correlated with free Al oxide. The two soils responded to acid irrigation by accelerated silicate weathering and enhanced ion leaching. Sulfate sorption reduced these effects.  相似文献   

4.
Acid deposition has caused acid episodes and elevated concentrations of metals like Fe, Al and Mn in streams in mountain regions of Sweden. In streams in the area of Lofsdalen, central Sweden, an episode in 1978 during snow melt caused massive downstream migrations of fish. Acid episodes have occurred yearly since then. pH of 4–4.5 and high concentrations of total Fe, Mn and Al were measured during these spates. Liming measures have been carried out in a number of catchments in order to increase the pH and try to decrease the leaching of metals. The lime has been delivered on wetlands, seepage areas and areas covered by meltwater during the spring. Cage experiments were carried out with yearling brown trout in the springs of 1982, and 1985–86. Fe, Al and Mn were analysed in water samples and on/in the gills of dead and live brown trout. There were no significant correlations between mortality or average survival time and total concentrations of Fe, Al or Mn in the water or on/in the gills. Average survival time was positively correlated to pH (p< 0.01). Metal speciation was carried out in 15 experiments in 1985 and ?86. A canonical discriminant analysis showed that pH and the concentration of labile inorganic manganese in the water explained all the observed mortality (can. corr 0.89, p< 0.001). The rate of accumulation of manganese on/in the gills was correlated to the concentration of labile inorganic manganese in the water (p<0.01, r2=0.54, linear regression).  相似文献   

5.
The concentrations and annual fluxes of Fe, Al, Mn, Cu and Pb were measured during 1983 in bulk precipitation, throughfall, stem-flow, forest floor percolate, mineral soil solution below the root zone and streamflow in a maple-birch stand on an acid podzolic soil at the Turkey Lakes Watershed (TLW), Ontario. Inputs of metals to TLW in precipitation were small in comparison with those in the eastern United States and Europe. Considerable loss of Mn and Cu from the vegetation during both the growing and the dormant (leafless) periods was observed and presumed to be due to leaching. The enrichment in soil solution of all metals examined, in relation to throughfall, was greatest for Al (7X) and least for Cu (1.2X). Aluminum was mobilized in both the forest floor and the mineral soil, the latter possibly in association with SO4 2?. Copper was solubilized in the lower forest floor or the mineral soil. Surface soil contents of Al and Cu were reduced by Al and, to a lesser extent, Cu leaching beyond the effective rooting zone. Iron, Mn and Pb were mobilized largely in the F horizon of the forest floor, most likely by organic acids. Leaching of Fe, Mn and Pb was reduced by metal accumulation in vegetation, the lower forest floor, or mineral soil within the effective rooting zone of the vegetation. Most (80 to 99%) of the metals leached from the rooting zone were retained in the watershed and did, not appear in streamwater.  相似文献   

6.
Water chemistry data from 165 lakes in Norway are discussed in relation to contribution from long-range transported air pollutants. Concentrations of lead and antimony in terrestrial mosses are used to express the relative contribution from long range transport to each lake. The contents of Al and Zn in lake water and of ‘excess’ SO4 in low Ca lakes show high correlations with the relative heavy metal deposition values from moss analysis. The ‘excess’ SO4 in low Ca lakes correlates strongly with Al and too a lesser extent with Mn and Fe. It is suggested that the lake water levels of Al and Mn, and even to some extent Fe, are significantly affected by acidic precipitation enhancing the leaching of these metals from mineral matter in soils and sediments. In the case of Zn, airborne supply to the lakes and their catchments appears to strongly affect the water content.  相似文献   

7.
This study investigated the effect of anions on the uptake of heavy metals and aluminum by Brassica rapa L. from non-contaminated, Cd-contaminated, and sewage sludge compost (SSC)-amended sandy soil. Four types of artificial precipitation were applied: deionized water (pH 5.7) as a control, and solutions of HNO3, H2SO4, and HCl prepared to pH 4.5. Precipitation was applied daily during the last 20 d of cultivation. The pH of the Cd-treated soil after harvest was not affected by any precipitation treatment. Shoot concentrations of heavy metals and Al were unaffected by any treatments on non-contaminated soil. In contrast, all acid treatments increased the Cd concentration in shoots grown on Cd-contaminated soil, but only HNO3 precipitation increased it in SSC-amended soil. These results indicate, even without large soil pH change, there is a possibility that the Cd uptake by B. rapa L. depends on anions in precipitation and chemical form of Cd in the soil under conditions of heavy metal enrichment.  相似文献   

8.
The seasonal patterns of flow and the concentrations of color, Mg, Ca, H+, Na, Cl, organic anions, SO4, and Gran alkalinity are examined for five streams or rivers in Kejimkujik National Park (Lower Mersey River, Atkins Brook, Grafton Brook, Pebbleloggitch Brook, and Beaverskin Brook). These range in organic color and acidity from very darkwater Atkins Brook (average 191 Hazen units, pH 4.2) to clearwater Beaverskin Brook (5 Hazen units, pH 5.5). In general, most dissolved substances are present in a relatively large concentration during the high-flow period of winter-spring (most notably color, Mg, H+, Ca, Na, organic anions, and SO4). In contrast, Gran alkalinity generally occurs in its highest concentration during the lowflow period. These observations suggest that during the high-flow period, substances are “flushed” from the terrestrial watersheds of these rivers and streams.  相似文献   

9.
DOC concentrations in two streams of different hydrologic order are highly variable with the higher order stream exhibiting approximately a 3 mo response lag. Seasonal variation of SO4 concentration and flux are similar in both streams and do not reflect the seasonal patterns in precipitation. The basins store SO4 from May to November and lose SO4 from December to April. Consequently, SO4 concentrations and flux are maximum during January to March and reach a minimum during July to September. The highly organic lower order stream exhibits relatively stable pH controlled by two competing mechanisms. The pH is dominated by organic acids during the summer and autumn and by mineral acids during the late winter and early spring. In the higher order system, the pH tends to be inversely related to changes in SO4 concentration. These observations suggest that organic systems do respond to acidic deposition but that in some systems mineral acid influence may be restricted to the winter and spring.  相似文献   

10.
Long range transport of H2SO4 has caused many Nova Scotian rivers to decline in pH to the point where their Atlantic salmon (Salmo salar) stocks have been destroyed or much diminished. Chemical records show a declining pH trend in N.S. rivers since the early 1950's. The annual variation in hydrogen ion activity is positively correlated with sulphate and Al and negatively correlated with organic anions. It is technically feasible to restore the acidified salmon habitat by the addition of limestone, and the total cost of mounting a liming program to restore the lost habitat has been calculated. The pre-acidification Atlantic salmon production capacity was estimated from physical habitat surveys and tag return data. The estimated costs of the liming program are much greater than the anticipated economic benefits of the salmon restoration. Present plans are for a small liming program to establish a series of refuges for the preservation of nuclei of native salmon stocks.  相似文献   

11.
The liming of soils in the lower part of an upland catchment was found to have a major effect on both soil properties and the chemistry of drainage waters. Exchangeable Al was closely correlated with soil pH and showed a very steep rise from 2.6-4.8 meq 1−1 over the pH range 5.5-4.5. As streams flowed from unimproved through improved land there was an increase in pH and the concentration of all major anions and basic cations. The greatest increase was in Ca (approximately 3.5-fold). The concentrations of all dissolved Al species decreased, with inorganic monomeric Al falling to near zero. Leachates were examined from soils representative of the most acidic and the least acidic. Calcium concentrations differed by almost tenfold. Aluminium was present in leachates from the limed soil, but most was unreactive and none was inorganic monomeric. Most of the Al leached from the acid soil was monomeric.
A model of soil acidification is proposed in which soil Ca is depleted at a rate of 8% of the exchangeable Ca per annum. The model predicts that liming a soil to neutrality would be likely to influence drainage water chemistry for 30-40 years and that the most acidic soils of the catchment show no net loss of Ca to drainage.  相似文献   

12.
Longitudinal and temporal variations in water chemistry were measured in several low-order, high-elevation streams in the Great Smoky Mountains to evaluate the processes responsible for the acid-base chemistry. The streams ranged in average base flow ANC from ?30 to 28 μeq L?1 and in pH from 4.54 to 6.40. Low-ANC streams had lower base cation concentrations and higher acid anion concentrations than did the high-ANC streams. NO3 ? and SO4 2? were the dominant acid anions. NO3 ? was derived from a combination of high leaching of nitrogen from old-growth forests and from high rates of atmospheric deposition. Streamwater SO4 2? was attributed to atmospheric deposition and an internal bedrock source of sulfur (pyrite). Although dissolved Al concentrations increased with decreasing pH in the study streams, the concentrations of inorganic monomeric Al did not follow the pattern expected from equilibrium with aluminum trihydroxide or aluminum silicate phases. During storm events, pH and ANC declined by as much as 0.5 units and 15 μeq L?1, respectively, at the downstream sites. The causes of the episodic acidification were increases in SO4 2? and DOC.  相似文献   

13.
Four sand pit lakes, at the Rio de Janeiro Sand Mining District, were monitored from November 2003 to November 2005, in order to characterize their hydrogeochemistry aiming to provide information to their possible use as fishponds at the end of mining activities. The results show diluted waters (low electrical conductivity) with low pH (<4) and relatively high sulfate and aluminum concentrations. The major water components (in particular Fe, Mn, SiO2, Al and SO4) are related to water acidity, since it controls solubility of aluminum silicate minerals and Mn and Fe oxides. Fe, Mn and Al availability in these waters are probably associated to organic colloids formation. On the other hand, the SiO2 content, as well as the decrease of sand mining in rainy season, may partially control Al availability by the formation of hydroxi-aluminum silicates. These geochemical processes together with the interruption of sand mining in the rainy season and the dilution of sand pit lakes water by rainwater can support the use of these pit lakes as fishpond for aquaculture.  相似文献   

14.
In the absence of SO infin4 sup= and NO inf3 su? in precipitation, the pH of precipitation is primarily a function of CO2?20 equilibria. Soil CO2 and organic acids, acquired during descent through soil profiles, augment the dissolving capacity of the solutions which initially may have a pH of 4 or lower. The recent man-related increase of H2SO4 and HNO3 in rainfall results in a significant lowering of pH in incident precipitation and an increase in corrosiveness of soil solutions. H2SO4 and HNO3 may contribute some Eh buffering capacity. Particularly susceptible to these changes are clay minerals and redox sensitive elements such as Fe, Mn, Ni, and Co. The overall chemical weathering trends associated with increased acidity of rainfall will be de-stabilization and eventual solution of clay minerals (and the loss of their cation exchange capacity), increased rates of chemical denudation, and solution of illuvial Fe and Al oxides and hydroxides. The latter results in the loss of the adsorbed and coprecipitated metal trace elements associated with these highly reactive phases. The general result in soils developed on non-carbonate substrates is a tendency toward extensive podsolization, with associated decrease in clay minerals, loss of cation exchange capacity, and decrease in fertility.  相似文献   

15.
Metals in water have been monitored for up to 18 years in acidified regions of Sweden. The concentrations of metals (Al, Cd, Cu, Fe, Mn, Mo, Pb, Zn) were determined by AAS and ICP-MS, the dissolved fractions after separation by in-situ dialysis. Elements showing negative pH-correlation were primarily Al, Zn, Cd, Mn, and Pb, while Mo was positively correlated to pH, indicating a predominance of negatively charged ionic forms. Zn, Cd, and Mn occurred primarily in the dissolved fractions, especially at the lower pH levels. Fe, Al, Pb and Mn were further enriched in humic waters. During the study period, some of the sites were subject to lime treatment, which had a marked influence on most elements, causing the mean levels and the seasonal fluctuations to decrease. Treatment on the lake surface was less effective than wetland liming to reduce seasonal fluctuations, especially for metals mainly originating from the catchments, as Fe and Al.  相似文献   

16.
Exchangeable and soluble soil aluminum (Al) is limiting plant growth in many soils worldwide. This study evaluated the effects of increasing rates of dolomite and magnesium carbonate (MgCO3) on Al3+, pH, dissolved organic carbon, cations, anions, and Al speciation on oil palm Deli dura × AVROS pisifera root growth. Dolomite and MgCO3 additions significantly raised linearly soil solution pH, magnesium (Mg2+), nitrate (NO3 ?) and chlorine (Cl?) concentrations; exponentially decreased the activity of phytotoxic Al species [aluminum (Al3+), aluminum sulfate (Al2SO4), and aluminum fluoride (AlF3)]; and reduced manganese (Mn) concentration and activity. High activity of those species exponentially reduced root dry weight. Optimum oil palm growth was achieved at: <50 μM monomeric Al, < 30 μM Mn, and <0.20 unit of the ratio Al+Mn to calcium (Ca)+Mg. High activity of Al species and Mn in acidic soil solution cause significant reduction of the root growth. Soil acidity alleviation either with dolomite or MgCO3 mitigates the toxic effect of Al and Mn.  相似文献   

17.
凉水国家级自然保护区溪流水化学特征分析   总被引：1，自引：0，他引：1       下载免费PDF全文
 采用集水区对比分析方法,探讨凉水国家级自然保护区不同森林类型对溪流水化学特征的影响。结果表明:保护区内各集水区溪流水均呈弱酸性至中性;主要离子中阳离子均以Ca2+的质量浓度最高,Na+次之,阴离子均以HCO3-的质量浓度最高,SO2-4次之;不同集水区溪流水中TP月平均质量浓度为0.031～0.077mg/L,TN为0.682～0.942 mg/L,NO-3-N的质量浓度高于NH+4-N;Fe的月平均质量浓度为0.030～0.037mg/L,Mn为0.010～0.012 mg/L。溪流水化学季节变化规律表现为:除HCO-3、SO2-4、Ca2+、Fe和Mn外,其他元素在融雪（4、5月）含量均较高;大多数元素在雨季的质量浓度比9月份低,而TN、TP、Fe、Mn表现为9月份的质量浓度低于雨季。保护区内原始阔叶红松林集水区溪流水质为最优,其他研究集水区溪流中的溶解物质含量增高,但除TP和SO2-4（p<0.05）外,差异性均不显著。说明凉水国家级自然保护区内虽进行过森林采伐和人工造林等人为干扰,但对于溪流水质并没有显著影响。  相似文献   

18.
There is a declining gradient of wet SO4 deposition from south to north in Nova Scotia with the highest values being in the south, along with a localized increase around the Halifax metropolitan area, due to local SO4 emission. Edaphic conditions such as drainage from soils containing gypsum or drainage on disturbed rocks containing pyrite, provide additional SO4 to surface waters.Acidity is usually absent in the former (pH > 7.0) and very high in the latter (as low as pH 3.6). By contrast peaty, organic drainages release water low in SO4 during the growing season but they release high amounts of organic anions (A?), consequently, these waters maintain decreased pH values, usually < 4.5. A study of over 80 wetlands and lakes during the ice free period in Nova Scotia showed that sea salt corrected SO4 concentrations range from 45 ueq L?1 in the south end of the province, ～30 ueq L?1 in the Kejimkujik area and < 17 ueq L?1 in the northern areas with values > 85 ueq L?1 in the Halifax area, reflecting the atmospheric deposition pattern of SO4 The SO4 concentrations may be > 2000 ueq L?1 in drainages containing gypsum, > 700 ueq L?1 in drainages over pyrite bearing socks but < 20 ueq/L?1 in streams draining bogs. The SO4 concentrations change considerably during the non-growing season when the ground is saturated with water or frozen, and the runoff is high (snow and rain often alternate in winter). Under such conditions SO4 concentration drops in the two former cases and increases in bog drainages, accompanied with a considerable drop in (A?) concentrations. Care should be taken when interpreting SO4 concentrations in surface waters in Nova Scotia with respect to atmospheric SO4 deposition.  相似文献   

19.
The study was performed in mountain streams in Central Sweden where a dramatic decrease in fish populations has been observed during the latest years. The spring runoff caused acid surges of pH 4.4 to 5.5 and high concentrations of Fe, Mn and Al occured in the stream waters. Water samples were collected during fish cage experiments performed during spring flood of 1985. The metal fractions were separated with filtration, in-situ dialysis and ion-exchange technique and determined using atomic absorption spectroscopy. The elements analyzed included Fe, Mn, Al, Zn, Cu, Pb and Cd. During spring flood, when a 100 % fish mortality was observed, particulate forms of Fe, Al and Mn dominated and were probably responsible for the toxic action. The high leaching of Fe, Mn and Al at spring flood during the recent years is a new phenomenon and seems to be caused by the increased acid deposition to the area.  相似文献   

20.
Loading of chemical elements in precipitation at the Solling For the period 1969–1976 (NH4, NO3: 1971–1976) monthly values of concentrations and flows of the ions NH4, H, Na, K, Ca, Mg, Fe, Mn, Al, Cl, NO3, SO4, P and organic bound N in precipitation are passed on. From the correlations between elements the following main ion sources are concluded: sea water (Na, Cl), combustion processes (SO4, NO3, NH4), lime dust after dissolution by H2SO4 and HNO3 (Ca, Mg), soil dust after dissolution by H2SO4 and HNO3 (Al, Fe), leaching from plants (K, NO3, SO4, Mg, Ca), biogenic contaminations (P, organic N, K, NH4, NO3). Seasonal variations in the concentrations are most evident for Na and Cl, less for NH4, SO4 and NO3. During the measuring period the flux of NH4 is significantly increased; for H and SO4, less for NH4, Mg, Ca and Fe, the increasing trend was interrupted in winter 1973/74 (oil crisis). Consequences for sampling are discussed.  相似文献   

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