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1.
Abstract

Salinity and sodicity effects on manganese (Mn) sorption in a mixed sodium‐calcium (Na‐Ca) soil system were studied. Soil samples were taken at 0–30 cm depth from Vertisols (El‐Hosh and El‐Suleimi) and Aridisols (El‐Laota) at three sites in Gezira scheme (Sudan). No Mn was applied to these soils. Prior to analysis the soils were equilibrated with NaCl‐CaCL2 mixed salt solutions to attain SAR values at different salt concentrations. The results indicated that saline soils sorbed less Mn and had higher equilibrium Mn concentrations. Sodic soils retained more Mn but had low equilibrium concentrations. Sodicity had a pronounced effect only on increasing Mn retention at higher SAR values. Salinity tended to alleviate sodicity effects on Mn retention, but soluble salts that increased soil pH decreased Mn concentration.  相似文献   

2.
Soil salinity (high levels of water-soluble salt) and sodicity (high levels of exchangeable sodium), called collectively salt-affected soils, affect approximately 932 million ha of land globally. Saline and sodic landscapes are subjected to modified hydrologic processes which can impact upon soil chemistry, carbon and nutrient cycling, and organic matter decomposition. The soil organic carbon (SOC) pool is the largest terrestrial carbon pool, with the level of SOC an important measure of a soil's health. Because the SOC pool is dependent on inputs from vegetation, the effects of salinity and sodicity on plant health adversely impacts upon SOC stocks in salt-affected areas, generally leading to less SOC. Saline and sodic soils are subjected to a number of opposing processes which affect the soil microbial biomass and microbial activity, changing CO2 fluxes and the nature and delivery of nutrients to vegetation. Sodic soils compound SOC loss by increasing dispersion of aggregates, which increases SOC mineralisation, and increasing bulk density which restricts access to substrate for mineralisation. Saline conditions can increase the decomposability of soil organic matter but also restrict access to substrates due to flocculation of aggregates as a result of high concentrations of soluble salts. Saline and sodic soils usually contain carbonates, which complicates the carbon (C) dynamics. This paper reviews soil processes that commonly occur in saline and sodic soils, and their effect on C stocks and fluxes to identify the key issues involved in the decomposition of soil organic matter and soil aggregation processes which need to be addressed to fully understand C dynamics in salt-affected soils.  相似文献   

3.
Abstract

The effect of soil sodicity [exchangeable sodium percentage (ESP)] on the growth, yield, essential oil composition, and cation accumulation of two cultivars (Bourbon and Cimpawan) of geranium (Pelargonium graveolens) were studied in a pot experiment. Irrespective of soil sodicity, two cultivars of geranium differed significantly in their plant height and herb and oil yield. Plant height was not significantly affected with increases in soil ESP from 0.7 (control) to 20.0 and 7.0, respectively, for cultivars (cv) Bourbon and Cimpawan, but further increase in soil ESP decreased the plant height. The herb yield of cv Bourbon significantly increased with increasing soil ESP to 16.0, and the oil yield increased with increasing ESP to 7.0. Further increase in soil ESP decreased the yield. The increase in yield of cv Bourbon was 13.1 and 15.1% in the herb and 40.0 and 15.2% in the oil over the control (ESP 0.7) at soil ESP of 7.0 and 16.0, respectively. Decreases in yield were 3.5, 4.9, 53.3, and 59.3% in the herb yield and 3.8, 5.7, 53.3, and 80.0% in the oil over control (ESP 0.7) at soil ESP of 20.0, 24.0, 28.0, and 30.0, respectively. The herb and oil yield of cv Cimpawan significantly decreased with increase in soil ESP. The decease in yield was 17.7, 20.2, 40.7, 53.1, 70.7, and 72.6% in the herb and 4.0, 6.8, 30.9, 45.4, 83.2, and 84.0% in the oil over control (soil ESP 0.7) at the soil ESP 7.0, 16.0, 20.0, 24.0, 28.0, and 30.0, respectively. The concentration of isomenthone, linalool, citronellyl formate, and geranyl formate in the essential oil increased at low levels of soil ESP (between 16.0 to 24.0) but decreased at high soil ESP (>28). The concentration of l‐citronellol, nerol, and geraniol gradually increased with increase in soil ESP. The increase in the soil ESP enhanced the concentration of sodium (Na) and decreased that of potassium (K) in shoot and root tissues of geranium as compared to control. The concentration of Ca in shoot tissues of cv Bourbon significantly decreased with increase in soil ESP, but in the cv Cimpawan, the Ca concentration was not significantly affected with increase in soil ESP from 0.7 to 16.0, and thereafter the Ca concentration significantly decreased with further increase in soil ESP. The concentration of Na, K, and Ca were relatively higher in shoot than in root tissues. The K/Na and Ca/Na ratios in shoot tissues of both cultivars of geranium decreased with increase in soil ESP. The K/Na and Ca/Na ratios in shoot were not found to be related to the differences in sodicity tolerance of the cultivars of geranium tested in this experiment. The concentration of zinc (Zn) in shoot tissues decreased with increase in soil ESP. The cv Bourbon maintained a higher concentration of Zn in shoot tissues at high sodicity than that of cv Cimpawan. The results suggest that the geranium is slightly to moderately tolerant of soil sodicity stress.  相似文献   

4.
Abstract

Growth, yield, essential oil composition, and cation accumulation of two species of Ocimum (viz., O. basilicum and O. sanctum) in response to soil sodicity was studied in pot experiments. The herb yield of O. basilicum significantly decreased with increases in soil exchangeable sodium percentage (ESP). The oil yield of O. basilicum significantly increased with increase in soil ESP from 4.0 (control) to 16.0, and further increases in soil ESP decreased the yield. The decrease in the yield of O. basilicum was 4.7, 13.1, 13.6, 23.7, and 24.3% in herb and 3.8, 11.5, 15.4, 23.0, and 26.9% in oil yield the over the control (ESP 4.0) at soil ESP values of 24.0, 32.5, 36.0, 45.0, and 50.0, respectively. The herb and oil yield of O. sanctum significantly increased with an increase in the soil ESP from 4.0 (control) to 24.0, and further increases in soil ESP decreased the yield. The maximum increase in the herb and oil yield of O. sanctum was 18.2% over the control (ESP 4.0) at the soil ESP of 24.0. At high sodicity, the decrease in yield of O. sanctum was 12.4 and 23.2% in the herb and 12.7 and 20.9% in the oil yield over control (ESP 4.0) at soil ESP values of 45.0 and 50.0, respectively. The concentration of methyl chavicol in the essential oil of O. basilicum and that of eugenol in the essential oil of O. sanctum was significantly higher at moderate soil sodicity levels as compared to the control (ESP 4.0). Increases in soil ESP enhanced the concentration of sodium (Na) and decreased that of calcium (Ca) and magnesium (Mg) in shoot tissues of both the Ocimum species. The concentration of potassium (K) in shoot tissues of O. sanctum gradually decreased with increase in soil ESP, and that of K in the O. basilicum increased with increase in soil ESP from 4.0 (control) to 36.0. Further increases in soil ESP decreased the K content. These results indicate that both these Ocimum species are highly tolerant to soil sodicity stress.  相似文献   

5.
Manganese content of cereals, maize and beet as indicator of soil acidity Soil and plant samples with and without growth depressions were taken from 479 agricultural fields (sand - loam) in the former GDR and analysed for pH and Mn and Mg respectively. Depressions in growth accompanied with symptoms of Mn excess and sometimes also of Mg deficiency were observed for barley, wheat, oats, maize and beets at soil pH < 4, 7, for rye at pH < 4, 1 - 4, 4. Soil pH correlated highly negatively with the Mn concentration of plants in early growth stages. Thus toxicity levels of Mn concentration in young plants could be derived. Mn concentrations > 140 mg/kg dry matter in spring barley, > 150 mg/kg in winter barley, > 160 mg/kg in wheat, > 200 mg/kg in rye, > 300 mg/kg in oats, > 350 mg/kg in maize and > 800 mg/kg in beet indicate growth depressions because of soil acidity. In the case of simultaneous Mg deficiency these Mn values are lower for oats and rye.  相似文献   

6.
An evaluation of the factors determining the occurrence and the properties of soils with low permeability occurring in vast areas in S Portugal was carried out taking into account the terrain morphology and the geology of the region. This paper deals with the variation patterns of the physical and chemical characteristics of soils from several soil toposequences that occur under different gradient slopes and on different parent rocks. Spatial variation of soil properties mainly depends on the composition of their cation‐exchange complex, as the role of other factors, such as the mineralogy of the clay fraction, were of minor importance. There is often a stronger increment of Na and/or Mg than of Ca with depth, causing a variable degree of sodicity in some of these soils, to which waterlogging tendency of their upper horizons is related. Though the occurrence of these features is determined by the nature of the parent rock, their degree of expression varies primarily according to the topographic position of soils. Therefore, a catenary distribution including nonsodic Cambisols or Luvisols in the hillcrests and Stagnic Solonetz or Sodic Luvisols or Sodic Stagnosols in the topographic lows is common. Such soil characteristics are of utmost importance for irrigation suitability and management of these soils, and for environmental impacts assessment, as the region is vulnerable to desertification.  相似文献   

7.
The adverse effects of sodicity on plant growth are difficult to quantify using naturally occurring soils because of the confounding variation in other soil properties, particularly salinity, pH, organic matter, soil nutrients, mineralogy, and texture. We applied a method involving the equilibration of large soil volumes with solutions varying in sodium adsorption ratio (SAR), followed by excess salt removal with solutions of similar SAR but lower ionic strength. Application of this method to a calcareous nonsodic, nonsaline Vertosol from Narrabri, New South Wales, resulted in soils with exchangeable sodium percentage (ESP) values between 2% and 25% but with similar magnesium and potassium concentrations and constant electrical conductivity (～2.7 dS/m). Soil pH and solution phosphorus concentrations automatically increased as the ESP of the soil rose, which is important to consider when addressing plant growth results. This method can successfully minimize the confounding of sodicity with other soil properties that so often plagues sodic soil research.  相似文献   

8.
The ability of three soil Na indices to predict soil conduciveness or suppressiveness to disease caused by the soil fungus Fusarium oxysporum f. sp. cubense was evaluated in seven banana plantations from the Canary Islands (Spain). These indices were exchangeable sodium percentage (ESP), soluble Na (SS0) and sodium adsorption ratio (SAR0) in 1:2.5 soil-water extracts (SARw and total cationic concentration (TCCw)=0. Sodium selectivity coefficients (KG0,K0) and TCC0 were calculated from soil exchange and solution data. The effects of ESP, SAR0, SS0, TCC0, KG0 and K0 on soil available iron (Fe extracted from soil by DTPA) and aggregate stability in water (water-stable aggregates (WSA), 200-2000 μm) were also studied. Our results showed that SAR0 calculated using cationic concentrations in 1:2.5 extracts might be a good indication of a relationship between SS0 and soluble divalent cations in conducive and suppressive volcanic soils to Fusarium. Both TCC0 and dispersion-flocculation concentrations seem to be not linked to soil suppressiveness or conduciveness to Fusarium wilt. These results suggested that soil physical properties seem to be not controlled by Na behaviour in these type of soils and, therefore, sodicity and salinity should not be a problem from a physical point of view. Moreover, SS0 and SAR0 were always greater in suppressive areas than in conducive areas. SAR0 was significantly correlated with SS0 but correlations between ESP against SS0 and SAR0 were weak. For SAR0 values above 2.5 (mmolc l−1)1/2 and ESP values below 15%, the exchangeable Na did not seem to be related to the capacity of suppressive areas to release more Na to soil solution. Larger values of SS0 were observed in suppressive areas for these values of SAR0 and ESP. It implies a lower quantity of soluble Na salts in conducive samples. A high Na salt content in soil can produce an increase of soil pH, which exerts a negative influence on available Fe release to soil solution. A clear separation between conducive and suppressive samples from relations between SS0 and SAR0 against WSA and Fe-DTPA showed that SS0 and SAR0 can be satisfactory indices to study the influence of Na concentrations on the incidence of Fusarium wilt. The mass of WSA increase in conducive areas might be favoured by the smaller amounts of soil solution Na found in these samples. In conclusion, our data provide evidence that release of Na to soil solution could favour soil suppressiveness to Fusarium wilt limiting soil aggregation and the availability of Fe, at least in soils of volcanic nature that are not affected by salinity or sodicity processes.  相似文献   

9.
Al tolerance of horse bean, yellow lupin, barley and rye. II. Mineral element concentrations in shoots and roots as affected by Al supply Inhibition of seminal root elongation by Al in solution culture gave the following ranking for Al tolerance: yellow lupin (Lupinus luteus ?Schwako”?) ? rye (Secale cereale ?Kustro)”? « horse bean (Vicia faba ?Herz Freya”?) > barley (Hordeum vulgare ?Roland”?). Exclusion from uptake by inactivation of Al outside the root was not responsible for the higher Al tolerance of lupin and rye, because comparable inhibition of root elongation occured at much higher Al concentration of the root and the root tips (5 mm) compared to barley and horse bean. The plant species differed considerable in nutrient concentrations of the roots: higher Ca concentrations in horse bean and rye, higher Mg concentrations in rye and lupin and higher P concentration in lupin. Al supply reduced Ca and Mg concentrations (Ca > Mg) in shoots and roots of all species. P concentrations were hardly affected. The nutrient concentrations in the root tips did not indicate that induction of nutrient deficiency was responsible for the effect of Al on root elongation and Al sensitivity of barley and horse bean. The considerable differences in Ca, Mg and P concentrations of the roots between the Al-tolerant plant species rye and lupin do not suggest a common physiological mechanism responsible for Al tolerance.  相似文献   

10.
AI tolerance of horse bean, yellow lupin, barley and rye. I. Shoot and root growth as affected by Al supply In solution culture considerable differences existed in Al tolerance between the plant species horse bean (Vicia faba ?Herz Freya”?), yellow lupin (Lupinus luteus ?Schwako”?), barley (Hordeum vulgare ?Roland”?) and rye (Secale cereale ?Kustro”?): compared to barley (0.05 μg Al l?1 = 1.85 μM Al) an 80 fold higher concentration of Al was necessary for lupin and rye for comparable growth depression and for horse bean a 5 times higher Al concentration. Injury by Al after 7 days of Al treatment was most effectively and sensitively characterized by an inhibition of elongation of seminal and especially of lateral roots. Numbers of laterals were also reduced. Dry matter production of roots and shoots was less affected by Al. In lupin, low Al supply even slightly increased the dry weight. The high Al tolerance of rye and yellow lupin in solution culture during the seedling stage is in good agreement with their adaptation to acid mineral soils.  相似文献   

11.
The effects of irrigation-induced salinity and sodicity on the size and activity of the soil microbial biomass in vertic soils on a Zimbabwean sugar estate were investigated. Furrow-irrigated fields were selected which had a gradient of salinity and sugarcane yield ranging from good cane growth at the upper ends to dead and dying cane at the lower ends. Soils were sampled under dead and dying cane, poor, satisfactory and good cane growth and from adjacent undisturbed sites under native vegetation. Electrical conductivity (EC) and sodium adsorption ratio (SAR) of saturation paste extracts was measured, as well as the exchangeable sodium percentage (ESP). There was a significant negative exponential relationship between EC and microbial biomass C, the percentage of organic C present as microbial biomass C, indices of microbial activity (arginine ammonification and fluorescein diacetate hydrolysis rates) and the activities of the exocellular enzymes β-glucosidase, alkaline phosphatase and arylsulphatase but the negative relationships with SAR and ESP were best described by linear functions. By contrast, the metabolic quotient increased with increasing salinity and sodicity, exponentially with EC and linearly with SAR and ESP.Potentially mineralizable N, measured by aerobic incubation, was also negatively correlated with EC, SAR and ESP. These results indicate that increasing salinity and sodicity resulted in a progressively smaller, more stressed microbial community which was less metabolically efficient. The exponential relationships with EC demonstrate the highly detrimental effect that small increases in salinity had on the microbial community. It is concluded that agriculture-induced salinity and sodicity not only influences the chemical and physical characteristics of soils but also greatly affects soil microbial and biochemical properties.  相似文献   

12.
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13.
Waterlogging + sodicity proved more harmful than sodic or waterlogging stress individually. Wheat genotypes were evaluated for waterlogging tolerance in neutral (pH 7.8) and sodic (pH 9.3) soils. There was 50% greater reduction in overall grain yield when genotypes were waterlogged for 15 days in sodic soil than in neutral soil. This was associated with proportional reductions in biomass and productive tillers. Severe effects of waterlogging were observed on grain yield in sodic soil and the extent of damage depends heavily on the stage of development, duration, and temperature. Waterlogging reduced the concentration of macro elements (K, Ca, and Mg), whereas effects on microelements concentration were mixed, with some elements increasing (Fe, Al, Mn, and Na) and others decreasing (Cu and Zn). Significant genotypic variation was observed for grain yield and biomass under the stress treatments and KRL 3–4, KRL 99, KRL 210, and Kharchia 65 were the top performers.  相似文献   

14.
采用室内盆栽试验,研究复合污染土壤中施加氮肥（NH4Cl）、磷肥（Na2HPO4）和钾肥（KCl）对高生物量经济作物玉米（Zeamays L.）幼苗生长以及吸收和积累重金属的影响。结果表明,不同施肥方式和浓度处理对玉米生物量变化以及吸收重金属有不同影响,NH4Cl能显著提高玉米地上部生物量、土壤Pb、Cd有效态含量,增加玉米对重金属Pb、Cd、As的提取量,最大分别可提高1.7、2.0倍和1.2倍。不同施肥方式和处理浓度均显著影响土壤有效态Pb含量,Na2HPO4在中浓度处理时显著降低土壤Pb的有效性,高浓度时则显著增加土壤有效态As含量,使玉米地上部对As的积累量有明显提高。在不同的浓度水平下,钾肥处理使玉米提取Pb含量显著高于氮肥和磷肥,其中低浓度KCl处理使玉米提取Pb量比对照增加2.4倍。对Pb-Cd-As复合污染农田土壤来说,施用氮肥（NH4Cl）处理对强化玉米的修复效果最好。  相似文献   

15.
松嫩平原盐渍土钠吸附比推算土壤碱化度研究   总被引：2，自引：0，他引：2  
Soil exchangeable sodium percentage (ESP) and sodium adsorption ratio (SAR) are commonly used to assess soil sodicity.Correlation between ESP and SAR of saturated pasted extract (SAR e) or of 1:5 (m:m) mixture soil to water (SAR 1:5) has been documented to predict ESP from SAR.However limited studies have been undertaken to model soil ESP based on soil SAR in the Songnen Plain,Northeast China.In this study,117 soil samples were used to predict ESP from SAR e and SAR 1:5 of salt-affected soils in western Songnen Plain.Soil ESP was highly related (r 2 > 0.76,P < 0.001) with SAR e and SAR 1:5.ESP of salt-affected soils in the Songnen Plain could be predicted using a logarithmic regression equations of ESP=10.72 · ln(SAR e) 15.36 and ESP=11.44 · ln(SAR 1:5) + 5.48.  相似文献   

16.
The study reports a case of bioreclamation of a once barren sodic landscape in the middle part of Gangetic alluvial plain at Banthra Research Station (National Botanical Research Institute, Lucknow, India) (80° 45′ – 53′E and 26° 40′ – 45′N) which began about four decades ago. The investigations were carried out to ascertain the changes in soil characteristics caused by different land‐use systems adopted consistently over three decades. The results showed that the anthropogenic effect on alteration of surface texture through addition of sand in soils of Typic Natrustalfs is still distinct but persistent sodicity is retained. The soils of Inceptic Haplustalfs are markedly improved showing pH value around 8 and ESP > 4 with negligible CaCO3. The soils of Aeric Endoaquepts supporting stands of forest trees are now devoid of sodicity to about 0\5 m depth, whereas the soils of Aeric Halaquepts though under cultivation have mild sodicity. Soils of Typic Halaquepts occurring on a low physiographic position with aquic soil moisture regime have high sodicity. Summarizing the results of changes in the surface (0 – 15 cm) soil characteristics caused by continuous cultivation irrespective of any crop grown on any soil type reveals that there is perceptible reduction in soil pH and ESP after three decades of reclamation using organic amendments coupled with regular cultivation and afforestation in different locations. Copyright © 2000 John Wiley & Sons, Ltd.  相似文献   

17.
盐化和有机质对土壤结构稳定性及阿特伯格极限的影响   总被引：14，自引：1，他引：14  
对甘肃景电灌区盐化和有机质对土壤团聚体的稳定性、黏粒的分散性及阿特伯格极限进行了调查研究。研究结果表明该灌区盐化土壤中水溶性盐以钠盐为主,土壤具有钠质现象。随含盐量和交换性钠离子百分率（ESP）的增加土壤团聚体的稳定性显著降低,黏粒的分散性显著增加,阿特伯格极限具有降低的趋势,明确地说明盐化和伴随着的钠质化是土壤结构性能退化的主要原因。随有机质含量的增加,土壤团聚体的稳定性显著增加,黏粒的分散性显著降低,阿特伯格极限显著增加,说明增加有机质含量可以显著改善盐化土壤的结构性能。可以根据如下公式利用有机质含量（OM）和ESP预测团聚体的稳定性:WSAR=19.4 0.98OM-1.43 ESP（R2=0.5741,n=67）。团聚体稳定性、黏粒分散性、流限和塑限互相之间显著相关,说明流限和塑限可以作为反映盐化土壤结构状况的指标。  相似文献   

18.
Abstract

Sodic water and spring water percolated through clay, clay loam, and sandy loam (SL) soils with exchangeable sodium percentages (ESPs) of 0, 10, 30, and 50. Reduction in saturated hydraulic conductivity and water stable aggregates recorded at higher ESPs. At ESP ≈30, application of sodic and spring water to clay soil (C) reduced saturated hydraulic conductivity from 1.2 to 3 mm hr?1, whereas in SL soil, the values were 2.8 and 6.2 mm hr?1, respectively. Results indicated that at any ESP and water source, the highest free swelling obtained was in the C soil. This study has practical importance to the management of irrigation water quality with respect to soil deterioration.  相似文献   

19.
A greenhouse pot experiment was carried out to investigate the effect of the arbuscular mycorrhizal fungus Glomus etunicatum on the uptake of atrazine (ATR) and cadmium (Cd) from soil by maize (Zea mays L.). Mycorrhizal colonization led to an increase in the accumulation of Cd and ATR in maize roots but a decrease in the shoots. Atrazine alleviated the adverse effects of Cd on maize growth, and this was more pronounced in the inoculated plants. An increase in Cd accumulation by maize roots was observed when ATR was also present. After harvest, the residual ATR concentration in the soil decreased markedly. With mycorrhizal inoculation the amount of residual ATR decreased more in the bulk soil but less in the rhizosphere soil compared to the noninoculated controls. Cadmium application significantly decreased the ATR residual concentrations in both the rhizosphere and bulk soils irrespective of inoculation treatment.  相似文献   

20.
The use of biochar in agriculture is a promising management tool to mitigate soil degradation and anthropogenic climate change. However, biochar effects on soil nutrient bioavailability are complex and several concurrent processes affecting nutrient bioavailability can occur in biochar‐amended soils. In a short‐term pot experiment, the concentration of N, P, K, S, Ca, Mg, Cu, Zn, Mn, B, Fe, and Na in the shoots of maize grown in three different soil types [sandy soil (S1), sandy loam (S2), and sandy clay loam (S3)] was investigated. The soils were either unamended or amended with two different biochars [wheat straw biochar (SBC) or pine wood biochar (WBC)] at two P fertilizer regimes (–/+ P). We used three‐way ANOVA and Principal Component Analyses (PCA) of transformed ionomic data to identify the effects of biochar, soil, and P fertilizer on the shoot nutrient concentrations. Three distinct effects of biochar on the shoot ionome were detected: (1) both biochars added excess K to all three soils causing an antagonistic effect on the uptake of Ca and Mg in maize shoots. (2) Mn uptake was affected by biochar with varying effects depending on the combined effect of biochar and soil properties. (3) WBC increased maize uptake of B, despite the fact that WBC increased soil pH and added additional calcite to the soil, which would be expected to reduce B bioavailability. The results of this study highlight the fact that the bioavailability of several macro and micronutrients is affected by biochar application to soil and that these effects depend on the combined effect of biochar and soils with different properties.  相似文献   

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