不同铁形态对水稻根表铁膜及铁吸收的影响

通过溶液培养试验研究了FeCl2?4H2O和FeCl3?6H2O对水稻根表铁膜数量及铁吸收的影响。结果表明,FeCl2处理时水稻根表铁膜浓度是FeCl3处理的197%～233%。利用EDTA-BPDS对铁膜形态分析看出,根表铁膜中Fe3+占85%～92%,Fe2+占8%～15%。水稻天优998根表铁膜数量显著高于培杂泰丰,其铁吸收是培杂泰丰的115%～138%。两种铁形态处理明显提高水稻的根系活力,其中,FeCl2处理时水稻根系活力增加24%～69%,FeCl3为16%～54%。FeCl2处理时水稻根系SOD、POD和CAT活性分别增加11%～32%、15%～30%和30%～31%,但FeCl3处理没有明显影响。上述结果表明一定浓度铁处理明显增加水稻根表铁浓度和铁吸收;与FeCl3处理相比,FeCl2处理能提高根系抗氧化酶活性,增加水稻的铁吸收和根表铁膜数量。     

根系氧化力不同的水稻品种磷锌营养状况的研究

采用琼脂培养和土壤培养试验研究了根系氧化能力不同的水稻品种磷、锌的营养状况。 结果表明, 在选用的 5 个水稻品种中, 根系氧化力较高的品种 LR-2、TZ88-145 和 YY-1, 其根表铁膜数量明显高于根系氧化力较弱的品 种KZ89-113 和KZ89-112。 根系氧化能力高, 根表形成的铁膜数量多, 富集的磷、锌数量也多, 反之则少。 这就构成 了“ 根系氧化力不同的水稻品种—根表形成的铁氧化物胶膜数量不同—富集在铁膜上的磷、锌数量不同—水稻的 磷、锌营养状况不同” 的连锁关系。     

鄱阳湖湿地植物根表铁膜形成的影响因素分析

湿地植物为了适应渍水环境,形成了大量的通气组织,植物可以通过通气组织将氧气输送到根系,从而将Fe2+氧化成铁的氧化物或氢氧化物沉积在植物的根表,形成铁膜。淹水土壤中植物根表形成铁膜必须具备两个条件,一是植物根际处于局部氧化状态,二是生长介质中存在大量的Fe2+。通过溶液培养和土-砂联合培养法,研究了Fe2+浓度、植物种类、诱导时间、p H值、水位变化、根系分泌物对根表铁膜形成的影响。结果表明:苔草和虉草根表铁膜的含量随Fe2+浓度的增加而增加,随诱导时间的延长呈上升的趋势,根系分泌物浓度与铁膜的量呈负相关,随水位的增加呈现先升高后降低的趋势,在水位2~3 cm,p H为5.5~6时根表铁膜的生成量达到最大值。     

水稻根表铁氧化物胶膜对水稻吸收磷的影响

本文采用营养液培养方法研究了根表铁氧化物胶膜对水稻吸收磷的影响。结果表明，水稻报表的铁氧化物胶膜随营养液中Fe2+浓度的增加而增加。铁氧化物胶膜可富集生长介质中的磷，根表铁膜数量越多，富集的磷量也越多。根表铁股可促进水稻对磷的吸收，但这种促进作用的大小依赖于根表铁膜数量。根表铁膜数量为24570mp／kg时，促进作用达到最大，此后随着铁膜数量的增加，水稻吸收磷的数量下降，但仍高于根表没有铁膜的水稻。因此，水稻根表形成的铁氧化物胶膜在一定程度上是一个磷富集库，对水稻吸收磷起促进作用。在此过程中，缺铁条件下水稻根分泌物中的植物铁载体对淀积铁氧化物胶膜的水稻根系吸收磷没有明显的作用。     

硒(Ⅳ)预处理下根表铁膜对水稻幼苗吸收和转运汞的影响

采用水培试验的方法研究硒(Se,Ⅳ)预处理下,根表铁膜对水稻幼苗吸收和转运汞(Hg)的影响。将水稻幼苗置于Se0和Se0.5(mg L-1)培养液中培养2周,再用4种不同浓度的Fe2+溶液(0、25、50和100 mg L-1即Fe0、Fe25、Fe50、Fe100)诱导水稻根表形成不同数量的铁膜,随后置于0.3 mg L-1的Hg Cl2培养液中继续培养72 h。结果表明,根表铁膜对水稻幼苗生长无显著影响,但硒可以增加其生物量。碳酸氢钠―柠檬酸三钠―连二亚硫酸钠(DCB)提取液(即根表铁膜)中含铁比例(57.3%~96.2%)显著高于水稻幼苗地上部(1.1%~17.5%)和根部(2.7%~25.9%),水稻幼苗的大部分铁被积累至DCB提取液中。随着根表铁膜数量的增加,根和地上部汞含量均显著降低。在Fe50和Fe100处理中,硒的加入显著减少了地上部和根部的汞含量,也显著降低了汞的分配系数,Se(Ⅳ)预处理能明显提高铁膜固持汞的量。综上所述,Se(Ⅳ)预处理和根表铁膜均能阻碍水稻幼苗对汞的吸收和向地上部的转运,减轻水稻汞胁迫,从而起到保护水稻避免汞毒害的作用。本研究对于提高汞污染区稻米质量和保证粮食安全具有一定的现实意义。     

铁膜对水稻根表面电化学性质和氮磷钾短期吸收的影响

通过水培试验研究了水稻根表铁膜对根表电化学性质、根表对NH4+、K+和磷酸根吸附和吸收的影响。结果表明,铁膜降低根表阳离子交换量,使根表zeta电位绝对值减小,说明根表负电荷数量减少。与对照相比,铁膜抑制了水稻根表对NH4+和K+的吸附,但促进了其对磷酸根的吸附。6 h培养实验结果表明,铁膜使水稻对NH4+、K+、H2PO4-的吸收速率分别降低了21.1%、42.7%、59.1%。因此,作为物理、化学屏障或者临时储存库,铁膜抑制了水稻对大量营养元素的短期吸收。     

水稻根表铁膜形成机制及其生态环境效应

许多水生植物的根系表面及其根际微环境都具有形成铁膜的能力,根表铁膜是植物适应水生环境的重要机制。本文叙述了水稻根表铁膜的形成条件、化学组成与空间分布,分析了根表铁膜形成的生理与分子机理。探讨了根系氧化酶、氧化性物质、根系泌氧能力、根际氧化性微生物活性及相关基因在铁膜形成过程中的作用; 在此基础上,进一步分析了水稻根表铁膜的营养效应和阻止重金属离子对根系的毒害效应。最后就根表铁膜的研究方法与调节机制进行了展望。     

镉处理根表铁膜对水稻吸收镉锰铜锌的影响

本试验利用营养液和土壤培养系统,研究不同Fe、 Cd处理下根表铁膜对水稻吸收Cd、 Mn、 Cu、 Zn的影响。土壤中Fe的水平为0、 1、 2 g/kg Fe（以FeSO47H2O的形式供应）,Cd 的水平为0、 2、 10 mg/kg Cd（以3CdSO48H2O的形式供应）。营养液中Fe和Cd的水平分别为0、 10、 30、 50、 80、 100 mg/L Fe 和 0、 0.1、 1.0 mg/L Cd。收获后测定水稻根表、 根中和地上部Cd、 Fe、 Mn、 Cu、 Zn 含量。试验结果表明,两种培养方式下,随着介质中Fe浓度的增加,水稻根表铁膜（DCB-Fe）逐渐增多。土壤培养方式下,根表铁膜中Cd 和 Mn 含量随铁膜量增加而略有增加,所有元素含量均表现为根中大于铁膜中。营养液培养条件下,根表铁膜中Mn和Cu含量在高量 Fe 供应时有所增加, Mn、 Cu、 Zn表现为铁膜中大于根中。根表铁膜中Zn含量在两种培养方式下均未呈现一定规律性变化。根中和地上部 Cd、 Mn、 Cu、 Zn 含量一般都随介质中Fe浓度的增加而下降,Cu和Zn含量在加Cd处理中下降。以上结果证明,铁膜对Cd 的吸附阻挡能力有限,对Mn、 Cu、 Zn 的吸附作用因培养方式和元素种类不同而有所差异,植株体内微量元素含量的下降主要与它们之间的相互抑制作用有关。     

不同土壤的还原状况对铁镉形态转化和水稻吸收的影响

采用土壤-蛭石联合培养,以填充蛭石的网袋模拟根际,置于红壤、水稻土、盐土中后淹水栽培水稻13 d.试验结果表明,水稻栽培期问,红壤、水稻土、盐土pH变化范围分别为6.05 ～6.78、6.47 ～7.33、6.42 ～7.44;有机质处理下,除红壤根际pH明显升高外,其余土壤根际和非根际pH均有所下降.各土壤对照根际Eh保持在233 ～ 385 mV;有机质处理使根际Eh下降,同时也导致除盐土外的非根际Eh上升.土壤还原溶解Fe与蛭石吸附Fe的90％以上均米自铁锰氧化物结合态铁(Oxide-Fe)组分,与溶液Eh、pe+ pH均有显著相关性,表明两表面同为Fe的氧化还原反应,但方向相反.水稻根表Fe膜的形成与根际氧化还原状况有关,在对照根际(高Eh)环境下,根表Fe含量随pH升高而降低,在有机质处理根际(低Eh)环境下则随pH升高而升高;在红壤中,根表Fe膜阻碍Fe的吸收,在水稻土和盐土中,根表Fe膜促进Fe吸收.根表Cd含量与根内Cd、地上部Cd有显著正相关;在红壤中,根表Fe膜阻碍了水稻Cd的吸附和吸收;水稻土和盐土中,根表Fe膜促进了水稻Cd的吸附和吸收.     

干湿交替对作物根际特征及铁膜形成的影响研究进展

铁膜普遍存在于水生植物的根系表面,根际周围Fe~(2+)的浓度和根系氧化力决定了根表铁膜的数量。干湿交替是农业生产中常用的灌溉技术。在干湿交替过程中,水分和氧气含量的变化导致根际土壤发生一系列物理、化学和生物学变化,从而对根表铁膜的形成产生影响。本文综述了干湿交替过程对根际特征变化的影响,分析了根表铁膜的形成条件、化学组成与空间结构和根表铁膜的形成过程,并在此基础上探讨了干湿交替对铁膜形成的影响以及干湿交替诱导铁膜形成的可能机制。最后对干湿交替诱导铁膜形成的研究方法与应用前景进行了展望。     

磷饥饿诱导水稻根表铁膜形成机理初探

采用溶液培养的方法,初步探索了磷饥饿诱导水稻根表铁膜形成的机理。磷饥饿24h后水稻的根表出现了明显的红棕色物质的沉积,扫描电镜的能谱分析结果显示,红棕色物质是铁的氧化物。针对这一现象,首先研究了没有水稻生长的正常磷营养液和缺磷营养液的变化,结果表明二者之间全波长的扫描图谱没有出现差异。采用酸碱混合指示剂的琼脂染色方法,观察了水稻根系表面及根际pH值的变化情况,并分别测定了正常磷营养（P）和缺磷（P0）2种条件下水稻的根系活力。结果看出,缺磷时水稻根系活力高于磷营养正常的处理,尤其是基因型Jin23A,其P和P0处理间根系活力差异极显著。水稻根表三价铁的浓度高于二价铁,并且缺磷根系表面三价铁和二价铁浓度均明显高于供磷处理;缺磷处理水稻根质外体沉积的铁浓度也明显高于供磷处理。因此,初步确定磷饥饿诱导水稻根表铁膜形成是生物学基础上的化学反应过程。     

硅缓解水稻根系铁毒害

Silicon (Si) can enhance the resistance of plants to many abiotic stresses. To explore whether Si ameliorates Fe2+ toxicity, a hydroponic experiment was performed to investigate whether and how Si detoxifies Fe2+ toxicity in rice (Oryza sativa L.) roots. Results indicated that rice cultivar Tianyou 998 (TY998) showed greater sensitivity to Fe2+ toxicity than rice cultivar Peizataifeng (PZTF). Treatment with 0.1 mmol L-1 Fe2+ inhibited TY998 root elongation and root biomass significantly. Reddish iron plaque was formed on root surface of both cultivars. TY998 had a higher amount of iron plaque than PZTF. Addition of Si to the solution of Fe treatment decreased the amount of iron plaque on root surface by 17.6% to 37.1% and iron uptake in rice roots by 37.0% to 40.3%, and subsequently restored root elongation triggered by Fe2+ toxicity by 13.5% in the TY998. Compared with Fe treatment, the addition of 1 mmol L-1 Si to the solution of Fe treatment increased xylem sap flow by 19.3% to 24.8% and root-shoot Fe transportation by 45.0% to 78.6%. Furthermore, Si addition to the solution of Fe treatment induced root cell wall to thicken. These results suggested that Si could detoxify Fe2+ toxicity and Si-mediated amelioration of Fe2+ toxicity in rice roots was associated with less iron plaque on root surface and more Fe transportation from roots to shoots.     

缺铁水稻根表铁膜对硒的转运和吸收的影响

Under anaerobic conditions, ferric hydroxide deposits on the surface of rice roots and affects uptake and translocation of certain nutrients. In the present study, rice plants were cultured in Fe-deficient or sufficient solutions and placed in a medium containing selenium （Se） for 2 h. Then, FeSO4 was added at the various concentrations of 0, 10, 40, or 70 mg L-1 to induce varying levels of iron plaque on the root surfaces and subsequent uptake of Se was monitored. The uptake of Se was inhibited by the iron plaque, with the effect proportional to the amount of plaque induced. The activity of cysteine synthase was decreased with increasing amounts of iron plaque on the roots. This may be the important reason for iron plaque inhibition of Se translocation. At each level of iron plaque, Fe-deficient rice had more Se than Fe-sufficient rice. Furthermore, with plaque induced by 20 mg Fe L-1, plants from Fe-deficient media accumulated more Se than those from Fe-sufficient media, as the Se concentration was increased from 10 to 30 or 50 mg L^-1. We found that phytosiderophores, highly effective iron chelating agents, could desorb selenite from ferrihydrite. Root exudates of the Fe-deficient rice, especially phytosiderophores in the exudates, could enhance Se uptake by rice plants with iron plaque.     

Uptake and Accumulation Characteristics of Arsenic and Iron Plaque in Rice at Different Growth Stages

Arsenic (As) uptake by rice plants and its toxicity to human beings have caused worldwide concerns. Investigating the characteristics of As accumulation in rice in relation to root surface iron plaque during the whole growth of rice would provide important information for devising measures to mitigate rice As uptake in As-polluted areas. Uptake and accumulation characteristics of As in rice at different growth stages as well as iron plaque on rice root surfaces were investigated in a pot culture experiment in a greenhouse. The results showed that As concentrations in roots, stems, and leaves increased with rice growth, while As concentration in spikelets decreased with grain development: 53.63% of As content in leaves, 61.51% in spikelets, and 82.09% in stems were found at both the jointing and booting stages, which suggested that the two stages were the key stages of As uptake. Root surface iron plaque at different growth stages was extracted by DCB (dithionite-citrate-bicarbonate). DCB-extractable iron (Fe) and DCB-extractable As were significantly increased with rice growth (P < 0.001), and there was a significant positive correlation between DCB-extractable Fe and As (P < 0.001), indicating that iron plaque was very important to sequester As on rice root surfaces.     

Tropical Rice Cultivars from Lowland and Upland Cropping Systems Differ in Iron Plaque Formation

In iron toxic wetlands, ferric hydroxide is commonly deposited on rice roots. This study aims to to evaluate the differences in iron plaque formation in rice cultivars from different cropping systems. Thirty days old seedlings of Brazilian rice cultivars from the lowland cropping system (‘BRS Atalanta’ and ‘Epagri 107’) and upland cropping system (‘Canastra’) or both systems (‘BRSMG Curinga’) and the cultivar ‘Nipponbare’ were exposed to iron excess [4 mM iron sulfate heptahydrate (FeSO₄.7H₂O)] for seven days in nutrient solution. It was observed iron plaque formation and ruptures of the root epidermal cells. The lowland cultivars showed higher Fe content in iron plaque. Iron stain was detected in the root hairs, epidermis, hypodermis, and exodermis. The root exodermis may be contributed to prevent the deposit of iron in the cortex of the lowland cultivars and in the cultivar ‘BRSMG Curinga’. It was observed in plants with iron plaque formation significant reductions in the shoot content of phosphorous, manganese and magnesium due to different causes. The differences in iron plaque formation among the cultivars might be an indicative of variations in exodermis selectivity, root oxidative capacity, and iron nutrition mechanisms.     

Formation of manganese oxide plaque on rice roots in solution culture under varying pH and manganese (Mn2+) concentration conditions

Roots of rice (Oryza sativa L.) exposed to 25, 50, and 100 ppm concentrations of manganese (Mn²⁺) in solution culture at pH 4.0, 5.0, 6.0, 7.0, and 8.0 for 48 hours developed visible brown coatings (plaque) of oxidized Mn. Most plaque was deposited on a region of the root 1–6 cm long above the root tip. Manganese in root plaque was removed by dithionite‐bicarbonate‐citrate extraction and internal root Mn released by pressure digestion. Concentrations of Mn were determined by atomic absorption spectrometry. Mean concentrations of Mn in plaque exceeded concentrations of Mn remaining in roots after the DCB wash in all treatment conditions. Concentrations of plaque and internal Mn increased with increasing pH and Mn²⁺ concentration in the treatment solution. Significant positive correlations existed between plaque and internal Mn concentrations at high pH. A larger percentage of total root metal remains in Mn plaqued roots after DCB treatment than has been previously observed in similarly treated iron (Fe) plaqued roots.