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1.
    
The influence of bedrock on aluminium toxicity and aluminium speciation in the soil solution was studied in four Pinus pinaster plots. Growth and biomass parameters in the acidic soils were also evaluated in relation to different Al toxicity indices. The plots were developed over slate, biotitic schist, mica schist and granite. Samples of rhizospheric and non‐rhizospheric soil, 1‐year‐old needles and roots were collected in each study plot. Total Al, reactive Al, acid‐soluble Al, non‐labile and labile Al and Al species (Al3+, Al‐OH, Al‐F and Al‐SO4) were determined in soil solution. Reactive Al dominated over the acid‐soluble Al, and the non‐labile Al predominated over the labile Al in all soils, but particularly over mica schist. In the biotitic schist soil, the Al forms and total Al were lower, whereas concentrations were always higher over mica schist. The Al forms considered most toxic were Al3+ and Al‐OH, and Al concentrations were highest over slate and mica schist. Al toxicity indices in soil, needle and roots showed a risk of toxicity in mica schist, slate and granite. The stand site indices over slate and mica schist were lower, consistent with the high labile Al and Al3+ + Al‐OH in soil solution. Despite the high stand site index over granite, the growth efficiency was low, in accordance with very low ratios of Ca/Al in needles or fine roots. This confirmed the adaptation of maritime pine to granitic substrates. Copyright © 2016 John Wiley & Sons, Ltd.  相似文献   

2.
    
Common bean (Phaseolus vulgaris L.) proved to be very sensitive of low pH (4.3), with large genotypic differences in proton sensitivity. Therefore, proton toxicity did not allow the screening of common bean genotypes for aluminium (Al) resistance using the established protocol for maize (0.5 mM CaCl2, 8 μM H3BO3, pH 4.3). Increasing the pH to 4.5, the Ca2+ concentration to 5 mM, and addition of 0.5 mM KCl fully prevented proton toxicity in 28 tested genotypes and allowed to identify differences in Al resistance using the inhibition of root elongation by 20 μM Al supply for 36 h as parameter of Al injury. As in maize, Al treatment induced callose formation in root apices of common bean. Aluminium‐induced callose formation well reflected the effect of Ca supply on Al sensitivity as revealed by root‐growth inhibition. Aluminum‐induced callose formation in root apices of 28 bean genotypes differing in Al resistance after 36 h Al treatment was positively correlated to Al‐induced inhibition of root elongation and Al contents in the root apices. However, the relationship was less close than previously reported for maize. Also, after 12 h Al treatment, callose formation and Al contents in root apices did not reflect differences in Al resistance between two contrasting genotypes, indicating a different mode of the expression of Al toxicity and regulation of Al resistance in common bean than in maize.  相似文献   

3.
Surface waters in northern forest ecosystems receive a substantial amount of drainage water from superficial soil horizons enriched in organic matter (SOM). Chemical reactions in the interface between the soil solution andf organic colloides will therefore affect the surface water chemistry. The mobilization of total organic carbon (TOC) and pH was studied as a function of amounts of organically adsorbed Na, Ca and Al in two O and one A horizon, which differed in the likelihood of contributing to the chemistry in runoff, in a forested watershed in northern Sweden. The samples were hydrogen ion saturated, washed and titrated with NaOH, Ca(OH)2 and Al(OH)3 in a constant ionic medium of 0.01 M NaCl in order to give rise to a population of manipulated samples differing in the composition of adsorbed cations. The highly humified SOM accumulated in the Oh and Ah horizons of a Gleysol close to the draining stream was stabilized by flocculating Al (95% of adsorbed metal cations), which resulted in a low release of TOC. These horizons showed a high potential of organic carbon solubility when Al was changed for di- or monovalent cations. Calculations suggested that the release of TOC would increase more than ten times if Al was exchanged for Ca upon liming to pH 6.0. The pH values of all horizons were shown to be determined mainly by the composition of adsorbed mono-,di- and trivalent cations.  相似文献   

4.
由于磷和铝在溶液中的相互作用,研究磷对植物铝毒害作用的关键是选择合适的磷铝处理方法,本研究采用两种磷铝处理方法就磷对植物铝毒害的作用进行了比较。结果表明,采用计算铝活度的方法,磷能缓解铝对小麦的毒害,而采用磷铝交替处理的方法,磷则加重铝对小麦的毒害。尽管在计算铝活度的方法中不同磷浓度处理液中铝的活度相同(用GEOCHEM软件计算),但磷浓度越高的处理液,其毒性铝的浓度越低,在该方法中,磷可能是通过降低溶液中毒性铝的浓度而缓解铝毒的,不能很好地避免溶液中磷铝相互作用。磷铝交替处理彻底避免了磷铝在溶液中的相互影响,保证相同的磷和铝处理浓度,而且长期交替处理在一定程度上也降低了磷铝不能同时处理对试验结果准确性的影响,因而,该方法是一种研究植物磷铝关系比较可行的方法。在磷铝交替处理条件下,磷加重小麦的铝毒害,可能与磷促进铝在根尖的累积有关。  相似文献   

5.
Abstract

The relationships between the ratio of plant-available phosphorus (P-AL) to total P and soil properties were examined in 52 samples of mineral soils collected from different parts of Norway. The ratio P-AL/total P in the soils was used as a measurement of a soil's capacity to bind P in sparsely soluble forms and of the possibility for plants to utilize added P. Simple regression analysis showed that the ratio P-AL/total P was correlated with clay (r= ?0.60???, significant at the 0.1% probability level), Tamm acid oxalate extractable Fe (r= ?0.63???), and Tamm acid oxalate extractable Al (r-= ?0.44???), but not with organic C and pH. Variation of Fe, Al and clay content could explain 50% of the variation of the ratio of P-Al/total P. Partial correlation coefficients showed that Fe was the most important factor explaining the variation of the ratio of P-AL/total P.  相似文献   

6.
Soil acidification limits livestock production in many parts of the world. Two experiments were carried out to investigate the effect of aluminium (Al) on pasture yield and animal production. In experiment 1, the effect of raising soil pH (in water) from 5.1 (acid soil, A) to 5.6 (corrected soil, C) was tested on forage and animal production. In experiment 2, Friesian calves were individually fed either silage with or without the addition of 2000 mg kg?1 of Al as aluminium sulphate. Al, P, Ca and Mg concentrations were measured in forage, and in animal blood and faeces. Live weight gain (LWG) was also measured. Soil acidification resulted in a 36% overall reduction in pasture yield in the A treatment (9.4 ± 0.31 and 14.7 ± 0.47 t ha?1 year?1 for the A and C treatments respectively) and in 15% reduction of the protein concentration in the herbage. No significant differences were found for the individual daily LWG (P > 0.05). Direct Al intake reduced animals daily LWG by 14% (P ≤ 0.05). The correction of soil acidification increased livestock production by 125% when stocking rate was strictly adjusted to grassland production.  相似文献   

7.
Al3+是植物铝毒害的主要形态,而其活性受环境pH值的影响,H+-ATPase通过调节根的质子分泌改变根际pH值。为探讨铝胁迫下根际pH值变化与小麦耐铝性的关系,以小麦品种ET8(耐铝型)、ES8(铝敏感型)为试验材料,采用溶液培养的方法对铝胁迫下根际pH值及根尖H+-ATPase活性变化进行了研究。结果表明,铝处理条件下,小麦根际pH值随培养时间的延长而升高;随培养液中铝浓度的增加,根际pH值上升幅度下降,相同铝浓度处理条件下ET8根际pH值显著高于ES8。根际pH值与根尖铝含量呈极显著负相关(R2=0.932 1),与根相对伸长率呈极显著正相关(R2=0.858 5),表明小麦通过提高根际pH值降低根尖铝含量,减轻铝毒害。根尖H+-ATPase活性随铝处理浓度升高而显著降低,100 μmol·L-1Al处理24 h ET8和ES8根尖H+-ATPase活性分别为各自无铝处理的69.8%和60.0%,根尖H+-ATPase相对活性与根际pH值呈极显著负相关(R2=0.831 9)。温度显著影响根的伸长,低温处理(9 ℃)根际pH值显著高于常温处理(25 ℃),而根尖铝含量却显著低于常温处理。表明小麦通过根尖H+-ATPase提高根际pH值降低铝毒害。综上所述,铝胁迫下小麦可通过提高根际pH值减轻铝毒害,不同耐铝性小麦品种根际pH值的显著差异是耐铝性差异显著的  相似文献   

8.
    
Abstract

Loss of soil‐water saturation may impair growth of rainfed lowland rice by restricting nutrient uptake, including the uptake of added phosphorus (P). For acidic soils, reappearance of soluble aluminum (Al) following loss of soil‐water saturation may also restrict P uptake. The aim of this study was to determine whether liming, flooding, and P additions could ameliorate the effects of loss of soil‐water saturation on P uptake and growth of rice. In the first pot experiment, two acid lowland soils from Cambodia [Kandic Plinthaqult (black clay soil) and Plinthustalf (sandy soil)] were treated with P (45 mg P kg?1 soil) either before or after flooding for 4 weeks to investigate the effect of flooding on effectiveness of P fertilizer for rice growth. After 4 weeks, soils were air dried and crushed and then wet to field capacity and upland rice was grown in them for an additional 6 weeks. Addition of P fertilizer before rather than after flooding depressed the growth of the subsequently planted upland rice. During flooding, there was an increase in both acetate‐extractable Fe and the phosphate sorption capacity of soils, and a close relationship between them (r2=0.96–0.98). When P was added before flooding, Olsen and Bray 1‐extractable P, shoot dry matter, and shoot P concentrations were depressed, indicating that flooding decreased availability of fertilizer P. A second pot experiment was conducted with three levels of lime as CaCO3 [to establish pH (CaCl2) in the oxidized soils at 4, 5, and 6] and four levels of P (0, 13, 26, and 52 mg P kg?1 soil) added to the same two acid lowland rice soils under flooded and nonflooded conditions. Under continuously flooded conditions, pH increased to over 5.6 regardless of lime treatment, and there was no response of rice dry matter to liming after 6 weeks' growth, but the addition of P increased rice dry matter substantially in both soils. In nonflooded soils, when P was not applied, shoot dry matter was depressed by up to one‐half of that in plants grown under continuously flooded conditions. Under the nonflooded conditions, rice dry matter and leaf P increased with the addition of P, but less so than in flooded soils. Leaf P concentrations and shoot dry matter responded strongly to the addition of lime. The increase in shoot dry matter of rice with lime and P application in nonflooded soil was associated with a significant decline in soluble Al in the soil and an increase in plant P uptake. The current experiments show that the loss of soil‐water saturation may be associated with the inhibition of P absorption by excess soluble Al. By contrast, flooding decreased exchangeable Al to levels below the threshold for toxicity in rice. In addition, the decreased P availability with loss of soil‐water saturation may have been associated with a greater phosphate sorption capacity of the soils during flooding and after reoxidation due to occlusion of P within ferric oxyhydroxides formed.  相似文献   

9.
    
Kochia sieversiana (Pall.) C. A. Mey is a forage plant in the family Chenopodiaceae, which can grow in extremely alkalinized grasslands at pH levels of 10 or higher. Kochia sieversiana often contains a large amount of oxalic acid. In the present study, seedlings of K. sieversiana were exposed to the following conditions: nonstress, salt stress (molar ratio of NaCl : Na2SO4 = 1:1, salinity: 200 mM), and alkali stress (molar ratio of NaHCO3 : Na2CO3 = 1:1, salinity: 200 mM). By determining and analyzing various physiological factors such as the concentrations and distribution of different organic acids (including oxalic acid) in various parts of K. sieversiana, the concentrations of inorganic ions (K+, Na+, Cl, SO$ _4^{2-} $ , etc.), the organic solutes (proline, betaine, and soluble sugar) in shoots, and the accumulation and distribution of oxalic acid in K. sieversiana, the physiological contribution of oxalic acid to K. sieversiana adaptability to saline and alkaline conditions was investigated. Results show that oxalic acid mainly accumulated in shoots, and that its concentration was highest in mature functional leaves where photosynthesis productivity was based and lowest in old stems and roots, regardless of plant treatment (nonstress, salt, or alkali conditions). Under nonstress, salt, and alkali conditions, the concentrations of oxalic acid in mature leaves were 8%, 10%, and 12% of their dry weights, respectively, and were 1%, 0.7%, and 0.6% of dry weights, respectively, in roots. There were varying effects of salt and alkali conditions on oxalic acid concentrations in different parts of K. sieversiana. Oxalic acid concentration increased in leaves, did not change significantly in young stems, and decreased in old stems and roots. The present analysis shows that oxalic acid exists as an organic anion in K. sieversiana. Consequently, oxalic acid not only plays a crucial role in osmoregulation and pH adjustment, but it also is the dominant contributor of negative charge, playing a key role in maintaining ionic balance in vivo. Oxalic acid in K. sieversiana shoots is a key substance on which the adaptation to saline and alkaline conditions is based.  相似文献   

10.
铵态氮/硝态氮对水稻铝吸收的影响及其机制研究   总被引:2,自引:0,他引:2       下载免费PDF全文
选用两个水稻品种武运粳7号(耐铝品种)和扬稻6号(铝敏感品种)作为实验材料,利用水培试验,通过长期和短期处理相结合的方式研究了NH4+-N和NO3--N对水稻Al吸收的影响及其作用机制。结果表明,与NH4+-N相比,NO3--N促进了水稻对Al的吸收。而且随着NO3--N浓度的提高,水稻根中Al含量显著增加,随着NH4+-N浓度的提高,水稻根中Al含量显著降低。这些结果表明NH4+-N和NO3--N对水稻Al吸收的影响具有浓度效应。当向Al溶液添加pH缓冲剂后,NH4+-N和NO3--N对根尖Al累积的影响变小,表明NH4+-N和NO3--N处理下溶液pH的变化可能是NH4+-N和NO3--N对水稻Al吸收影响不同的一个原因。  相似文献   

11.
    
《Soil Use and Management》2018,34(3):343-353
Acid soil amelioration was measured annually over an 11 year experiment. Lime, and superphosphate were surface‐applied under combinations of three rates of lime, viz. nil, lime to raise pHC a of 0–10 cm to 5.0 (low rate) and 5.5 (high rate) respectively, two rates of superphosphate (125 kg/ha every 2 to 3 yr, 250 kg/ha/yr) and two sheep stocking rates. Soils were sampled at 0–2.5, 2.5–5, 5–7.5, 7.5–10, 10–15 and 15–20 cm. Soil pH stratification developed after lime application. By 11 yr lime had not raised pHC a to either 5.0 or 5.5 in the 5–10 cm profile. However, pHC a >5.0 or >5.5 were observed in the 0–5 cm profile. Under high P, low lime application, soil pHC a was higher in the 0–2.5 cm profile at low stocking rate. Effects of applied lime on pHC a declined with time and depth under low lime and the relationship with Alex which increased as pHC a declined, was modelled. A rarely reported relationship showed that as soil C increased the apparent solubility of Al decreased. At the lowest pHC a considered, there was a strong negative association between Alex and total C, becoming weaker with positive pHC a increments. Higher P rates increased pHC a under low lime contrasting with lesser effects on pHC a under low P at the same lime rate. Slow and limited lime movement means that farmers growing acid sensitive plants must apply lime early enough and at rates and frequencies sufficient to ensure downward movement.  相似文献   

12.
刘奕媺  于洋  方军 《土壤与作物》2018,7(2):201-211
土地盐碱化严重影响农业生产发展,是世界范围内农业发展所面临的重大问题。因此,了解盐碱胁迫对植物造成的危害、植物对盐碱胁迫的响应及耐盐碱植物的耐逆机制,将为增强作物的耐盐碱能力和开发利用盐碱地奠定坚实的理论研究基础。盐胁迫对植物造成的伤害主要包括离子胁迫、渗透胁迫和氧化胁迫,而碱胁迫在盐胁迫基础上还增加了高pH胁迫,对植物的伤害表现得更为严重和复杂。铁离子是植物生长发育不可或缺的重要金属离子,然而在盐碱土壤中植物对铁离子的吸收利用效率大大降低,严重影响了植物的正常生长和代谢。本文总结了盐碱胁迫对植物造成的生理伤害及耐盐碱植物资源的相关研究,综述了植物盐碱胁迫信号转导及分子机制研究进展,重点阐述了铁的转运吸收与盐碱胁迫的关系,以期为耐盐碱基因的挖掘、耐盐碱作物新品种的培育及开发利用改良盐碱地资源提供理论基础。  相似文献   

13.
    
An 8-year field study measured soil pH changes annually at various depth increments. Limestone was applied to tilled and untilled field strips annually for 8 years at either a 2.0 Mg/ha rate (100% calcium carbonate efficiency) and once every 4 years at the 8.0 Mg/ha rate (100% calcium carbonate efficiency), or as a water-treatment-plant limestone by-product in two replicated field trials. Liming materials increased soil pH in the 0- to 5-cm and 5- to 10-cm depths with time in untilled soils. Incorporated liming materials increased soil pH faster at the 5- to 10-cm depth and increased soil pH at the 10- to 15-cm depth. Mean maize and soybean grain yields increased for all liming materials, and maize ear leaf P and soybean shoot P and Ca increased after liming at the last year of the study. Consistent surface applications of liming materials without incorporation can mitigate acidification and improve crop yields in highly buffered soils.  相似文献   

14.
Toxicity of aluminium for the earthworm Eisenia andrei was studied in artificial soil at different pH levels. In a range-finding test, effects of three different aluminium salts on earthworm survival were determined. AlCl3 appeared to be most toxic, with LC50 values of 316, 359 and >1000 mg Al/kg dry soil at pHKCl of 3.5, 4.4 and 6.7, respectively in the control soils. Effects of this salt interfered with a strong decrease of soil pH with increasing aluminium concentration. Al2(SO4)3 was less toxic with LC50 values of 457, >4000 and >4000 mg Al/kg dry soil at pH 3.24, 4.86 and 7.22, respectively. Al2O3 did not affect earthworm survival at concentrations of 5000 mg Al/kg and pH levels between 2.4 and 7.1.In the main test, earthworms were exposed for 6 weeks to soils treated with Al2(SO4)3. As in the range-finding test, aluminium sulfate was most toxic at a pH of 3.4 with an LC50 of 589 mg Al/kg dry soil. At this pH, growth and cocoon production of earthworms were significantly reduced at 320 mg Al/kg dry soil, while at 1000 mg Al/kg dry soil all earthworms died. Survival was not affected by 1000 mg Al/kg dry soil at pH 4.3 and 7.3. At pH 4.3, growth was significantly reduced at 1000 mg Al/kg dry soil and cocoon production at 320 and 1000 mg Al/kg dry soil. At pH 7.3, aluminium only affected cocoon production at the two highest exposure levels. At the highest two exposure levels at pH 7.3, growth was significantly increased, suggesting a trade-off between growth and reproduction. These effects of aluminium at the highest soil pH could not be explained from the concentration of extractable, monomeric (labile) aluminium in soil, which decreased with increasing soil pH.  相似文献   

15.
采用悬空气培法,研究低pH(3.5、4.5、5.5)和铝毒(0、50、100μmolL-1)及其交互作用对荞麦根长、根边缘细胞活性及其分泌的黏液层厚度的影响。处理12h,Al3+浓度由50μmolL-1增至100μmolL-1时,pH3.5的根伸长量分别降低18.6%和31.9%,pH4.5时分别降低18.9%和26.8%,pH5.5时各降低8.5%。处理24h的根伸长量变化与12h类似。pH降低至3.5时,边缘细胞的活性下降28.6%,黏液层厚度无明显变化。Al3+浓度升高至100μmolL-1时,黏液层增厚64.6%,而边缘细胞活性变化不大。pH3.5与100μmolL-1Al3+的处理,边缘细胞活性最低,黏液层厚度最大,两者间存在极显著的交互作用。可见低pH加剧铝毒发生,外围黏液层产生可以减轻Al3+对边缘细胞的伤害。  相似文献   

16.
Plants in which growth was reduced by low and high Al applications were designated as Al-sensitive plant (Hordeum vulgare) and Al-medium tolerant plants (Leucaena leucocephala, Ischaemum barbatum, Stylosanthes guianensis, and Fagopyrum esculentum), respectively, while plants in which growth was not affected or was stimulated by Al application were designated as Al-tolerant plant (Brachiaria ruziziensis) and Al-stimulated plants (Melastoma malabathricum, Melaleuca cajuputi, Acacia mangium, Hydrangea macrophyila, Vaccinium macrocarpon, Polygonum sachalinense, and Oryza sativa), respectively. Plants tolerant to or stimulated by Al were further classified based on the criteria of Al accumulation: 1) Al-excluders such as M. cajuputi, A. mangium, L. leucocephala, I. barbatum, S. guianensis, and O. sativa, 2) Al root-accumulators such as V. màcrocarpon, B. ruziziensis, and P. sachalinense, and 3) Al-accumulators such as M. malabathricum, H. macrophylla, and F. esculentum. The growth and N, P, and K uptake in M. malabathricum, M. cajuputi, A. mangium, L. leucocephala, H. macrophylla, V. macrocarpon, I. barbatum, P. sachalinense, F. esculentum, and O. sativa were stimulated by Al application, especially P uptake, while in H. vulgare (Al-sensitive plant) they were reduced by Al application. Ca and Mg uptake of many plants was inhibited by Al application, while that of some plants adapted to low pH soils was not affected at all (Ca and Mg: M. cajuputi, H. macrophylla, V. macrocarpon, I. barbatum, and S. guianensis; Mg: B. ruziziensis and P. sachalinense). In M. malabathricum, the relationship between Al and Ca (or Mg) was antagonistic because the Ca and Mg contents decreased by Al application even though dry matter, N, P, and K accumulation was stimulated by Al application. Plants adapted to low pH soils grew poorly in the no-Al treatment. Since the effect of the pH on plant growth was less conspicuous than that of Al, growth stimulation by Al application was ascribed not only to the alleviation of H+ toxicity but also to the increase of root activity such as P uptake.  相似文献   

17.
Abstract

Two greenhouse studies were conducted to evaluate the effect of B, Mn and Zn on nodulation and N2‐fixation of southernpea (Vigna unguiculata (L.) Halp.) cultivars ‘Freezegreen’, ‘Mississippi Silver’ and ‘Pinkeye Purple Hull’. The cultivars were grown in plastic pots with a Norfolk sandy loam (fine, loamy siliceous thermic, Typic Paleudult) soil treated with B, Mn and Zn at rates of 0, 5, 10 and 20 kg/ha each at pH levels 5.5, 6.0 and 6.5. At pH 6.5 all micronutrient treatments significantly increased nodulation and N2‐fixation over the control (no micronutrient applied). The effects of B, Mn and Zn on nodulation and N2‐fixation depended on the cultivar and soil pH. For plants given the 5 kg/ha B and Mn treatments, ‘Mississippi Silver’ produced the highest number of nodules and ‘Pinkeye Purple Hull’ the least. At 20 kg/ha Zn, nodulation of ‘Freezegreen’ was highest and ‘Pinkeye Purple Hull’ the lowest. As a whole, maximum nodulation was at 5 kg/ha B and Mn and 20 kg/ha for Zn. Nitrogen fixation rates responded similarly except that the optimum rate for Zn was 10 kg/ha. Seed yield of plants peaked at 5 kg/ha for B and 10 kg/ha for Zn, indicating a possible relation of N2‐fixation to seed yield.  相似文献   

18.
    
ABSTRACT

The effects of long-term (1959–2005) liming in combination with cattle manure application on the chemical properties and aggregate stability of acid soil were investigated in the whole soil profile to a 100 cm depth. Investigations were performed in a long-term liming and fertilizing field trial at Vezaiciai Branch of Lithuanian Research Centre for Agriculture and Forestry situated in West Lithuania. The soil of the study site is Bathygleyic Distric Glossic Retisol (WRB 2014) with a texture of moraine loam. Acid soil had been periodically limed and manured at different intensity for 47 years. The experiment involved the following treatments: (1) unlimed and unfertilized (control); (2) unlimed and 60 t ha?1 manure; (3) limed and unfertilized; and (4) limed and 60 t ha?1 manure. During the 47-year period, liming was performed using pulverized limestone at a rate 1.0 (by hydrolytic soil acidity) every 7 years. During the whole study period, the soil received 38.7–36.5 t ha?1 CaCO3; 840 t ha?1 cattle manure, 2740 kg ha?1 mineral nitrogen; 3030 kg ha?1 phosphorus and 3810?kg?ha?1 potassium. The data showed that long-term (47 years) periodic liming of different intensities in combination with cattle manure application significantly changed the chemical properties of the whole soil profile. The soil acidification was neutralized in the topsoil and subsoil to the 60?cm depth when the soil had been systematically limed with 1.0 rate every 7 years in combination with 60?t?ha?1 manure application every 3–4 years. Periodic long-term liming in combination with manuring had a positive effect on the improvement of chemical properties of acid soil profile in the ElB1 and ElB2 horizons. The data of the soil structure in the topsoil and subsoil showed that such liming practice together with manuring had a positive effect on soil aggregate stability.  相似文献   

19.
    
In the context of pollution‐control strategies to minimize the detrimental effects of soil acidification, there is a need to know how and to what extent soils respond to acidifying substances. The purposes of this study were to assess the sensitivity of soil to acidification, in particular to a decrease in pH and in base saturation (BS), and the risk of Al toxicity for vulnerable plants using chemical indicators. These indicators were derived from soil data (pH, exchangeable cations, amount of fine earth) measured in the mineral horizons of 257 soil profiles throughout Switzerland. Based on the analysis of the distribution of pH and BS values in the soil collective, we assessed the sensitivity of soils to a decrease in pH and in BS. Soils that were considered sensitive to a decrease in pH had pH values between 4.8 and 7.0. The degree of sensitivity was estimated with the proportion of fine earth in the critical pH range to a depth of 100 cm. Soils that were considered sensitive to a decrease in BS had pH values between 3.6 and 5.5 and a BS between 10% and 95%. Since the effective cation‐exchange capacity (CECeff) of the fine earth might dampen the decrease in BS when acidity is added, the disposition for a decrease in BS was related to the relative amount of fine earth in the sensitive BS and to the mean CECeff of this fine‐earth fraction. The risk of Al toxicity for vulnerable plants was estimated using the ratio of base cations to Al at the cation‐exchange sites (BC : Alexc). A BC : Alexc of 0.2 was taken as a threshold value below which the risk for sensitive plants increases. The degree of risk was based on the proportion of fine earth in the critical BC : Al range (≤0.2) in the soil profile. These indicators taking into account the various aspects of soil acidification are derived from usually available data and represent therefore a cost‐effective tool to assess the sensitivity of soils to an input of acidity.  相似文献   

20.
    
A stratified subsurface layer of acidic soil can develop in minimally disturbed soil such as no‐till receiving injection of N fertilizer (e.g., anhydrous ammonia). The objective of this study was to evaluate the effectiveness of subsurface band treatments in alleviating soluble Al3+ and Mn2+ toxicities on sorghum growth. Soil columns 40 cm in length were packed with soil (Valentine fine sand mixed mesic Typic Ustipsamment and Thurman loamy sand mixed Mesic Udorhentic Haplustoll) with treatments applied at the 10–18 cm depth to mimic soil pH stratification. The treatments at this depth were: (1) entire layer at soil pH of 3.7; (2) band of soil 6 cm wide at pH of 5.8 with the rest of the soil at pH 3.7; (3) band of soil 6 cm wide at pH of 6.3 with the rest of the soil at pH 3.7; and (4) entire layer at soil pH of 5.8. The soil above and below the 10–18 cm depth was at pH 5.8. Sorghum (Sorghum bicolor L. Moench) was grown in the soil columns under a controlled environment for 6 weeks. High concentration of Al in soil solution was found in soil at soil pH 3.7 which was overcome by either banding to pH 5.8, 6.3, or having the soil layer at pH 5.8. Treatment with pH of 5.8 throughout the soil 10–18 cm depth produced significantly greater top growth, although all other pH or liming strategies performed better than the soil pH 3.7 treatment. The banded treatments at pH 5.8 and 6.3 allowed roots to grow below the 10–18 cm layer of soil, but root growth was still significantly less than in the soil where the entire soil treatment layer was at pH 5.8. The increase in biomass yield with soil pH of 5.8 in the entire treatment layer was higher compared to band treatment at pH 5.8; however, the lime requirement would be 3.4 times more with liming the entire layer compared to banding a portion of the soil to pH 5.8 and would thus be translated into a higher liming cost.  相似文献   

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