水稻耐碱生理和遗传机制研究现状与展望

碱(化)土是指土壤胶体中含交换性钠较多(碱化度>15%)、呈强碱性反应(pH>8.5)、土壤结构性差、含盐量不高的一类土壤,常与盐土相伴存在,两者统称为盐碱土。与盐土中中性盐(NaCl)对作物造成的胁迫不同的是,碱土中碱性盐(NaHCO₃和Na₂CO₃)对作物造成的胁迫不仅包括离子毒害和渗透胁迫,更严重的是根外高pH值对作物的伤害。利用"以稻治碱"的传统方法可以大规模改良碱(化)土壤,增加农业耕地面积。因此,了解和掌握水稻对碱胁迫的适应性,创建碱地水稻高效栽培技术,培育水稻耐碱新品种,对提高碱(化)土地利用率,保障区域粮食安全具有重要的现实意义。本文基于近年来国内外研究报道,从水稻耐碱形态和生理特性、耐碱基因定位与克隆、耐碱种质鉴定筛选以及水稻耐碱性遗传改良等4个方面进行综述,并对未来水稻耐碱性研究进行展望,以期为"以稻治碱"、改土增粮提供一定的理论依据。     

Anthropogenic transformation of soil and vegetation resulting from afforestation in southern steppes

Recent data (2006–2008) on characteristics of the vegetation and soils of the solonetzic complex in areas with tree failures within the Volgograd-Elista-Cherkessk forest shelterbelt have been compared with those obtained prior to afforestation (1950). The results show that the vegetation and soils have changed profoundly. Solonetzic agrozems in tree failure sites have been occupied by herbaceous plant communities similar in composition to natural communities. Anthropogenically altered soils formed under forest plantations have no natural analogs. The initial strongly saline shallow (crusty) solonetz soils with a chloride-sulfate or sulfate-chloride composition of salts have transformed into slightly saline solonetzic and solonchakous agrozems with sodium sulfate salinity or with increased alkalinity in the middle of the soil profile and a dealkalized arable horizon.     

活性焦对晋北盐碱地土壤性质和两种植物生长的影响

固废基改良剂是盐碱地改良的有效手段之一。活性焦作为一种多孔废弃物,应用于盐碱地预期可以起到改善土壤性质、减缓植物盐碱胁迫的作用。为了阐明活性焦对晋北盐碱地的改良效应,本研究设置不同用量活性焦(CK, 0 g·kg^-1;A₁₀, 10 g·kg^-1;A₂₀, 20 g·kg^-1;A₅₀, 50 g·kg^-1),分析其对盐碱地土壤性质和植物生长的影响。结果表明: 施用活性焦能显著提高土壤的水稳性团聚体含量,并降低土壤盐分含量、pH值和电导率。与CK相比,种植碱茅和玉米土壤的团聚体平均重量直径增加5.1%～32.2%,pH值降低0.4%～4.1%,钠吸附比(SAR)降低4.8%～18.7%,电导率降低7.4%～8.2%。施用适量活性焦能够降低植物细胞的质膜损伤,提高叶片叶绿素和Ca²⁺含量,从而有效促进植物生长,碱茅和玉米的生物量均在A₂₀处理达到最大。表明盐碱土施用20 g·kg^-1活性焦(A₂₀)可改善根际土壤环境,提高植物对Ca²⁺等的选择性吸收,从而降低盐分对植物细胞的损伤,促进盐碱生境中植物的生长。     

The Roles of Soil Characteristics and Toxin Adsorption in Avian Geophagy

Geophagy, the intentional ingestion of soil, is a widespread phenomenon whose function is still debated. Recent studies suggest that consumed soils adsorb dietary toxins and provide sodium. However, quantification of soil choice has been absent from most studies, prohibiting the direct comparison of soil use and characteristics. To determine correlates among bird use and soil characteristics, we analyze physical structure, mineral composition, and alkaloid adsorption (14 soil characteristics in total) for 22 soil samples from a riverbank ‘clay lick’ used by macaws and parrots (family Psittacidae) in Amazon lowland forests in the Tambopata region of southeastern Peru. We quantified bird preferences through photographic mapping. Mineral concentrations were determined using analyses designed to approximate the mineral availability in the vertebrate stomach. The sodium levels in the soil were much higher than in food plants consumed by parrots in this region. Both adsorption of quinine, the model alkaloid used, and sodium concentration correlated significantly with bird use. Sodium explained a much higher percentage of the variation in bird use than quinine adsorption. However, the analyses were complicated by the high degree of correlation among soil variables: clay percentage and sodium concentration were highly correlated with each other and with bird use, making it impossible to determine which of these may have the greater contribution to bird preference. The results suggest that the soils consumed provide an important source of dietary sodium and adsorb alkaloid toxins.     

Soil Ecology of Coccidioides immitis at Amerindian Middens in California

Outbreaks of coccidioidomycosis and isolation of Coccidioides immitis have been reported from Amerindian middens. This study was undertaken to determine the most important ecological component(s) for the occurrence of C. immitis at archeological sites. Soils from 10 former Indian villages with no prior history of coccidioidal infection were collected and cultured. The physicochemical properties of the midden soils were compared with nonmidden soils and positive soils. The following theories for the sporadic distribution of the pathogen in the soil of the Lower Sonoran Life Zone were considered: (i) the Larrea tridentata (creosote bush) association, (ii) the preference for saline soils, (iii) isolation near rodent burrows, and (iv) animals as possible agents of dispersal. Results showed that a high percentage of the midden soils contained C. immitis, whereas none of the adjacent, nonmidden soils yielded the fungus. Physicochemical analyses revealed that the dark color and alkaline pH of the midden soils were due to past organic contamination. Repeated isolations were made from soils with low to moderate alkalinity. Alkalinity and sandy texture were consistent features of all soils in this study. However, the lack of any reports of nonsandy infested soils possibly indicates that the sandy texture and alkalinity may be factors in the distribution of this fungus. The organic content, soil parent material, and color were not important in the soil ecology. L. tridentata was not significant in the macroflora at the infested sites surveyed. Samples collected without reference to rodent burrows yielded a high percentage of recoveries. Animals, although not the major natural reservoir, cannot be ignored as possible factors in the ecology of C. immitis.     

Reclamation of highly calcareous saline sodic soil using Atriplex halimus and by-product gypsum

The removal of sodium salts from saline soils by salt tolerant crops, as alternative for costly chemical amendments, has emerged as an efficient low cost technology. Lysimeter experiments were carried out on a highly saline sodic soil (ECe = 65.3 dS m(-1), ESP = 27.4, CEC = 47.9 cmole+ kg(-1), and pH = 7.7) and irrigated with canal water (EC = 2.2 dSm(-1), SAR = 4.8) to investigate reclamation efficiency under four different treatments: control (no crop and no gypsum application) (C), gypsum application equivalent to 100% gypsum requirement (G100), planting sea orach (Atriplex halimus) as phytoremediation crop (Cr), planting sea orach with gypsum application equivalent to 50% gypsum requirement (CrG50). Soil salinity (ECe) and exchangeable sodium percentage (ESP) were significantly reduced compared to the control. Average ESP and ECe (dS m(-1)) in the top layer were 9.1, 5.8 (control), 4.8, 3.7 (Cr), 3.3, 3.9 (CrG50), and 3.8, 3.1 (G100), respectively. Atriplex halimus can be recommended as phytoremediation crop to reclaim highly saline sodic clay loam soils.     

Naturally Saline Boreal Communities as Models for Reclamation of Saline Oil Sand Tailings

Reclaimed landscapes after oil sands mining have saline soils; yet, they are required to have similar biodiversity and productivity as the predisturbance nonsaline landscape. Given that many species in the boreal forest are not tolerant of salinity, we studied the effects of soil salinity on plant communities in natural saline landscapes to understand potential plant responses during the reclamation process. Vegetation–soil relationships were measured along transects from flooded wetlands to upland forest vegetation in strongly saline, slightly saline, nonsaline, and reclaimed boreal landscapes. In strongly saline landscapes, surface soil salinity was high (>10 dS/m) in flooded, wet‐meadow, and dry‐meadow vegetation zones as compared to slightly saline (<5 dS/m) and nonsaline (<2 dS/m) landscapes. Plant communities in these vegetation zones were quite different from nonsaline boreal landscapes and were dominated by halophytes common to saline habitats of the Great Plains. In the shrub and forest vegetation zones, surface soil salinity was similar between saline and nonsaline landscapes, resulting in similar plant communities. In strongly saline landscapes, soils remained saline at depth through the shrub and forest vegetation zones (>10 dS/m), suggesting that forest vegetation can establish over saline soils as long as the salts are below the rooting zone. The reclaimed landscape was intermediate between slightly saline and nonsaline landscapes in terms of soil salinity but more similar to nonsaline habitats with respect to species composition. Results from this study suggest it may be unrealistic to expect that plant communities similar to those found on the predisturbance landscape can be established on all reclaimed landscapes after oil sands mining.     

Studies on the Characteristics of Normal and Alkali Soil Profiles from an Alkali Infested Area in Allahabad,India

The development of the profile is mainly the consequence of movement of water in the soil and we may distinguish the following three possibilities:

Firstly under humid condition there is an excess of rainfall over evaporation. Thus, there is a general tendency of downward movement of soil moisture and the soil is subjected to a leaching process, whereby the constituents are carried downwards and are either deposited in the lower horizons or completely removed in drainage water.

Secondly, under arid conditions with an excess of potential evaporation over rainfall, rain moistens the soil to a limited depth. After cessation of rain, the soil moisture rises again to the surface under the influence of evaporation with the result that translocation occurs in both directions, and in final stages of dessication, the deposition of salts from solution may occur throughout an appreciable depth of surface soil.

Thirdly, downward movement may be prevented by the presence of ground water, or the occurrence of impervious sub-soil layer. In such cases water movement can only occur laterally over the horizon of impedence. The impedence may not be complete, but intermediate stages can also be observed.

The development of alkali soil profile is governed either by the second or third or by the combination of both the processes mentioned above.

In India, saline soils, saline-alkali soils and alkali soils are commonly distributed. Leached soils are of very rare occurrence.     

应用Illumina MiSeq高通量测序技术分析河西走廊地区盐碱土壤微生物多样性

【目的】以甘肃省河西走廊地区的9个盐碱土壤样品(原生盐碱土、次生盐碱土、农田土)为材料,研究该地区盐碱土壤中微生物群落的多样性。【方法】提取土壤微生物总DNA,应用Illumina Mi Seq高通量测序技术进行分析。【结果】从分布在河西走廊3个流域的9个盐碱土样品中共获得325 089条微生物的16S r RNA基因序列。冗余分析和热图分析表明,原生盐碱土与次生盐碱土、原生盐碱土与农田土微生物群落构成差异较大,次生盐碱土与农田土微生物群落差异较小。土壤p H对微生物群落组成的影响最显著。多样性指数和稀释性曲线分析得出,在9个土壤样品中,S6号Shannon指数最大,S1号Shannon指数最小,S1号Simpson指数最大,S6号Simpson指数最小,说明原生盐碱土的微生物群落多样性最低,次生盐碱土的微生物群落多样性最高。盐碱土壤中主要的微生物群落包括9个门,其中变形菌门占主导地位,其余依次是放线菌门、拟杆菌门、酸杆菌门、浮霉菌门、绿弯菌门、芽单胞菌门、厚壁菌门和疣微菌门。原生盐碱土和农田土中占优势的微生物群落是变形菌门,次生盐碱土中占优势的微生物群落是放线菌门。【结论】河西走廊地区盐碱土壤中微生物多样性非常丰富,存在大量的微生物类群,尤其是在次生盐碱土壤中。     

河西走廊酒泉地区盐碱土未培养放线菌多样性

采用免培养技术对河西走廊酒泉地区的原生盐碱土、次生盐碱土和农田土中的放线菌群落结构及其多样性进行分析.结果表明: 河西走廊酒泉地区原生盐碱土克隆文库分归于19个OTUs,分属于微球菌亚目、丙酸杆菌亚目、棒状杆菌亚目、弗兰克氏菌亚目、假诺卡氏菌亚目和放线菌目未知类群;次生盐碱土克隆文库分归于14个OTUs,分属于微球菌亚目、丙酸杆菌亚目和放线菌目未知类群;农田土克隆文库分归于7个OTUs,分属于微球菌亚目和棒状杆菌亚目;微球菌亚目是3种不同类型土壤中的共有种群,是原生盐碱土和农田土中的优势种群.多样性指数和稀释性曲线分析结果显示,3种不同类型土壤中放线菌种群丰富度为原生盐碱土>次生盐碱土>农田土;原生盐碱土、次生盐碱土的稀释性曲线均未趋于平稳,说明盐碱土中放线菌多样性比实际更加丰富.     

Soil salinity delays germination and limits growth of hyphae from propagules of arbuscular mycorrhizal fungi

Colonisation of plant roots by some arbuscular mycorrhizal (AM) fungi is reduced in the presence of sodium chloride (NaCl), probably due to a direct effect of NaCl on the fungi. However, there appear to be differences between the fungi in their ability to colonise plants in the presence of NaCl. This experiment tested the hypothesis that propagules of different isolates and species of AM fungi from saline and nonsaline soils would differ in their ability to germinate and grow in the presence of NaCl in the soil solution. Spores or pieces of root colonised by a range of AM fungi were incubated between filters buried in soil to which NaCl had been added at concentrations of 0, 150 or 300 mM in the soil solution. At regular intervals, filters were removed from the soil and both the percentage of propagules which had germinated and the length of proliferating hyphae were determined. Germination of spores of AM fungi studied was delayed in the presence of NaCl, but the fungi differed in the extent to which germination was inhibited. Two isolates of Scutellospora calospora reached maximum germination in 300 mM NaCl, but neither of two isolates of Acaulospora laevis germinated in the presence of NaCl. Germination of spores of the other fungi, including some isolated from saline soil, fell between these extremes. For some fungi, the specific rate of hyphal extension was reduced by NaCl. For others, the specific rate of growth was similar in the presence of NaCl to that in the control treatment, but overall production of hyphae was reduced in the NaCl treatments because germination was reduced.     

Salt uptake and salt tolerance by sunflower

Summary A normally grown crop of sunflower on red sandy loam soils was found to remove considerable quantities of chloride and sodium. On heavy clay soils with saline patches sunflower plants removed large quantities of sodium followed by chloride and sulphate. In view of its salt tolerance, it is suggested that intercropping or rotation with sunflower might help reduce soil salinity and improve soil conditions where salinity problems are coming up especially in heavy clay soils with low permeability. re]19720711     

Influence of ionic strength on sodium-calcium exchange of two temperate climate soils

Salt-affected soils have been studied extensively with respect to their Na–Ca exchange properties. These studies have focused on soil environments of the arid West. However, because of irrigation and oil well brine discharges in the temperate region of the U.S. there is need to understand sodicity behavior of such soils. In this study, two Kentucky soils (Pembroke and Uniontown) at the 0–10 cm depth were studied to evaluate the influence of ionic strength (I) and sodium adsorption ratio (SAR) on cation selectivity coefficients. The data showed that both soils exhibit at least two classes of exchange sites and in general the apparent affinity for Na⁺ increased when solution ionic strength increased. Furthermore, both soils under all three ionic strengths tested showed greater affinity for Na⁺ than the average agricultural saline soil of the arid West. The data suggested the need for establishing critical salt dispersion thresholds for temperate climate soils and developing effective brine management approaches.     

Retention of applied Cu++ by soils

Summary The Cu⁺⁺ retaining power of the three soils used in our experiments was found to be of the order: alkali soil > black soil > red soil. The alkali soil retained the applied Cu⁺⁺ in basic copper carbonate and hydroxide forms due to its high carbonate (soluble + insoluble) and high pH values, and the red soil retained the least amount of Cu⁺⁺ because of its low pH value and negligible carbonate content, whilst the black soil, being fairly rich in CaCO₃, organic matter and suitable pH, occupied an intermediate position.When the original samples were treated with H₂O₂, H₂O₂ + HCl or were ignited at 600°C for 1 hour the retention of applied Cu⁺⁺ decreased more or less as a result of destruction of organic matter, carbonate and dehydration of sesquioxides leaving an inert material.Saturation of original soils with H⁺ (by HCl) resulted in lower Cu⁺⁺-retention, whilst the conversion of H-soils to Ca⁺⁺-soils showed a higher Cu⁺⁺-retention but never approached the amount of Cu retained by original soils. This is due to lowering of pH of the samples, removal of carbonates as well as due to antagonistic effect of H⁺-ions. A greater percentage of the Cu⁺⁺ retained by these samples exists in the exchangeable forms in comparison to original soils.It has also been observed that addition of CaCO₃, at the rate of 1 to 2 per cent (to the hydrogen samples) resulted in a precipitation of practically all the applied Cu⁺⁺ and non-existence of exchangeable forms of Cu⁺⁺.     

The effect of some soil amendments on chemical and microbiological properties of an alkali soil

Summary A representative alkali soil sample from Tal-El-Kebir was treated in pots with different rates of gypsum or sulphur. These amounts were calculated according to the exchangeable sodium present in the soil. Chemical and microbiological properties were studied during reclamation process.Addition of gypsum in appropriate amounts to replace exchangeable sodium on the clay complex is much faster and more superior to the addition of the corresponding amounts of sulphur.Counts of total microbial flora, Azotobacter, nitrifiers, and aerobic cellulose-decomposers increased as the reclamation proceeded, on the other hand, counts of spores of aerobic sporeformers, streptomyces, and clostridia decreased.Cultivation of such reclaimed soils exerted beneficial effect on its microbial flora. Plant vigor which was taken as a resultant of the improvement of the physico-chemical and biological properties of the soil due to reclamation was found to be superior in case of addition of an amount of gypsum equivalent to the amount of adsorbed sodium.     

Microbial community biomass and structure in saline and non-saline soils associated with salt- and boron-tolerant poplar clones grown for the phytoremediation of selenium

Poplar trees (Populus spp.) are often used in bioremediation strategies because of their ability to phytoextract potential toxic ions, e.g., selenium (Se) from poor quality soils. Soil microorganisms may play a vital role in sustaining health of soil and/or tolerance of these trees grown in poor quality soils by contributing to nutrient cycling, soil structure, overall soil quality, and plant survival. The effect of naturally occurring salts boron (B) and Se on soil microbial community composition associated with poplar trees is not known for bioremediation strategies. In this study, three Populus clones 13–366, 345–1, and 347–14 were grown in spring 2006 under highly saline, B, and Se clay-like soils in the west side of the San Joaquin Valley (SJV) of CA, as well as in non-saline sandy loam soils located in the east side of the SJV. After 7 years of growing in the respective soils of different qualities, soil samples were collected from poplar clones grown in saline and non-saline soils to examine and compare soil quality effects on soil microbial community biomass and composition. The phospholipid fatty acid (PLFA) analysis was used to characterize microbial community composition in soils from trees grown at both locations. This study showed that microbial biomass and the amount and proportion of arbuscular mycorrhizal fungal (AMF) community were lower in all three poplar clones grown in saline soil compared to non-saline soil. Amounts of Gram + bacterial and actinomycetes PLFAs were significantly lower in poplar clone 13–366 grown in saline soil compared to non-saline soil; however, they did not differ significantly in poplar clones 347–14 and 345–1. Additionally, amounts of saprophytic fungal, Gram ? bacterial and eukaryotic PLFA remained similar at saline and non-saline sites under poplar clones 347–14, 345–1, and 13–366. Therefore, this study suggested that salinity and B do have an impact on microbial biomass and AMF; however, these poplar clones still recycled sufficient amount of nutrients to support and protect saprophytic fungal and bacterial communities from the effects of poor quality soils.     

A California grasslands alkali specialist,Hemizonia pungens ssp. pungens,prefers non‐alkali soil

Question: Edaphically severe habitats commonly support edaphic endemics, specialized plant species that do not occur elsewhere. The endemism of native plant species in edaphically specialized habitats suggests either (a) that these native endemic species are uniquely specialized to survive and grow better under the conditions prevalent in these harsh areas, or (b) that these areas represent refuges from competition with other (often exotic) species. Location: Central Valley, California, USA. Methods: We surveyed the vegetation distribution in alkali sinks and carried out a reciprocal transplant greenhouse experiment crossed with a competition treatment to examine the interplay between interspecific competition and edaphic factors in determining relative performance of an alkali endemic forb (Hemizonia pungens ssp. pungens) and its exotic grass competitor (Lolium multiflorum). Results: Lolium consistently performed better in non‐alkali soil. In contrast, Hemizonia, in the absence of competition, performed significantly better on the non‐alkali soils, but in competition with Lolium, performed equally well on alkali and non‐alkali soils. Conclusions: These results suggest that Hemizonia does not inherently prefer harsh alkali soil, but is better able to tolerate alkali soil and may be excluded from more moderate soils by competition. Therefore, edaphic and biotic effects may interact to determine the spatial distribution of this edaphic endemic. Our data suggest a mechanism by which competition between native and exotic species on impoverished soils leads to dominance of native species and creation of refugia for native species where exotic species are unable to thrive.     

Comparative adsorption of human enteroviruses, simian rotavirus, and selected bacteriophages to soils.

Virus adsorption to soils is considered to be the most important factor in removing viruses after land treatment of wastewater. Most of the studies on virus adsorption to soils have utilized poliovirus as the model system. In the present study, comparative adsorption of a number of different types and strains of human enteroviruses and bacteriophages to nine different soil types was studied. Under the experimental conditions of this study, greater than 90% of all viruses adsorbed to a sandy loam soil except echovirus types 1, 12, and 29 and a simian rotavirus (SA-11), which adsorbed to a considerably lower degree. A great deal of variability was observed between adsorption of different strains of echovirus type 1, indicating that viral adsorption to soils is highly strain dependent. Of the five phages studied, f2 and phi X174 adsorbed the least. In addition to being dependent on type and strain of virus, adsorption was found to be influenced also by type of soil. Thus, soils having a saturated pH of less than 5 were generally good adsorbers. From these results, it appears that no one enterovirus or coliphage can be used as the sole model for determining the adsorptive behavior of viruses to soils and that no single soil can be used as the model for determining viral adsorptive capacity of all soil types.     

Comparative adsorption of human enteroviruses, simian rotavirus, and selected bacteriophages to soils.

Virus adsorption to soils is considered to be the most important factor in removing viruses after land treatment of wastewater. Most of the studies on virus adsorption to soils have utilized poliovirus as the model system. In the present study, comparative adsorption of a number of different types and strains of human enteroviruses and bacteriophages to nine different soil types was studied. Under the experimental conditions of this study, greater than 90% of all viruses adsorbed to a sandy loam soil except echovirus types 1, 12, and 29 and a simian rotavirus (SA-11), which adsorbed to a considerably lower degree. A great deal of variability was observed between adsorption of different strains of echovirus type 1, indicating that viral adsorption to soils is highly strain dependent. Of the five phages studied, f2 and phi X174 adsorbed the least. In addition to being dependent on type and strain of virus, adsorption was found to be influenced also by type of soil. Thus, soils having a saturated pH of less than 5 were generally good adsorbers. From these results, it appears that no one enterovirus or coliphage can be used as the sole model for determining the adsorptive behavior of viruses to soils and that no single soil can be used as the model for determining viral adsorptive capacity of all soil types.     

盐度对滨海土壤细菌多样性和群落构建过程的影响

滨海盐土是重要的农业土地后备资源。微生物是土壤中物质循环的关键动力,然而盐度对土壤微生物群落特征影响的研究还很缺乏。本研究采集滨海地区的土壤样品,研究非盐、轻盐和高盐3组不同盐度对土壤细菌数量、多样性和群落构建的影响。结果表明: 与非盐和轻盐土壤相比,高盐土壤的脱氢酶活性和细菌数量显著降低,而细菌α多样性没有变化,细菌群落结构发生分异。利用零模型反演群落构建过程,发现盐度是细菌群落构建过程的主控因子,盐度主导的高确定性过程控制了滨海盐土细菌的群落结构。说明在现有的盐度范围内,高盐土壤中同样含有丰富的微生物种质资源,具有盐土改良的生物学基础,然而由于高确定性的群落构建机制,外源物种很难定殖于滨海盐土。因此,在利用微生物技术改良滨海盐土时,应尽可能筛选耐盐的土著菌种,提高定殖效率。