盐胁迫下白蜡根际微域的营养元素状况

为揭示根-土界面微域养分的吸收、累积与亏缺状况,运用X-射线电子探针研究盐胁迫对白蜡根际和根内营养元素相对含量及其分布的影响。结果表明,与对照（0 g/L）相比,低浓度（3 g/L）盐分处理使白蜡根系吸收较多的Ca、Mg、Cl等元素; 而高浓度（9 g/L）处理则使根系吸收Ca、Mg、Cl的能力下降。白蜡根内Na、K、Fe的累积量和根际Na的含量随盐浓度增加均有升高; 其中,过量的Na会破坏白蜡根细胞原生质膜的结构,引起胞内营养大量外泌,造成植物营养缺乏,从而诱发盐害。因此,Na在根际微域的累积是引起白蜡盐害的主要原因。     

不同品种小麦根际磷转化及VA菌根对小麦根际磷转化的影响

采用三室根箱研究了磷高效小麦 81( 85)-5-3-3-3及磷低效NC37两个小麦品种根际磷转化及VA菌根对根际土壤磷转化的影响。结果表明 ,磷胁迫下 ,81( 85)-5-3-3-3的吸磷量略高于NC37,两种小麦品种根际土壤均形成了明显的Olsen-P ,Ca2-P ,Ca8-P ,Al P等形态磷的耗竭区。两种小麦品种在不施磷肥和施用磷肥下接种VA菌根 ,小麦的生物量、植株磷浓度、小麦根际Olsen-P,Ca2-P ,Ca8-P,Al-P ,Fe-P的消耗量均显著增加 ;根际、非根际土壤各形态磷素的浓度梯度明显降低。     

低磷胁迫下箭筈豌豆和毛叶苕子根际过程的差异比较

采用我国北方两个豆科绿肥品种: 箭筈豌豆（Vicia sativa L.）与毛叶苕子（Vicia villosa Roth）,在控制条件下通过不同供磷处理的营养液培养,研究了不同绿肥作物适应低磷胁迫根际过程的差异,并揭示其高效利用磷的机理。试验通过分次取样的方法,测定了两种豆科作物在缺磷与供磷条件下的生物量、根系质子释放速率、根系有机酸分泌速率以及根表酸性磷酸酶活性的动态。结果表明,箭筈豌豆与毛叶苕子在生长前期对低磷胁迫的响应存在明显差异。箭筈豌豆主要靠增大质子释放量和提高酸性磷酸酶活性来适应低磷胁迫; 而毛叶苕子主要通过提高根冠比、扩大根系生物量来对外界环境中的缺磷状况做出响应,在缺磷时其根表酸性磷酸酶的活性显著提高。箭筈豌豆与毛叶苕子可通过协调根系形态和生理的适应性变化提高对磷的吸收。     

Mobilization and turnover of soil phosphorus in the rhizosphere

Recent progress in methods enables a better understanding of the turnover of P in the rhizosphere. Examples of this progress are the separation of soil layers differing in proximity to the roots, improved methods for extraction and fractionation of soil P, application of ³²P isotope dilution analysis to follow P fluxes between various fractions and direct determination of microbially bound P and of root phosphatases.

• These methods were combined to investigate the following aspects
• –labile P pools, the P fluxes between these pools and their contribution to the P supply to growing maize roots
• –the role of microbial biomass in these interactions and the partition of mobilized P between plants and microorganisms
• –modifications of sorption and transport of P in the rhizosphere
• –plant availability of native and added organic phosphates, and the relative significance of root and soil phosphatases.

There is a significant transformation of P in the rhizosphere with a corresponding redistribution among fractions of different plant availability. About 9% of the inorganic ³²P added to soil were incorporated within 2 weeks into microbial and organic fractions. The transfer of P from non-exchangeable forms exceeded the depletion of the exchangeable P by a factor of 5. About 53% of the mobilized P originated from inorganic, the remaining 47% from organic fractions. Of the mobilized P 80% was taken up by the plants and 20% was found in the microbial biomass. Up to 90% of the P in the rhizosphere soil solution was organic with a maximum just outside the root zone. Soluble inositol hexaphosphate modified the sorption of inorganic P, thus shifting its equilibrium solution concentration. The phosphatase activity of the roots is considerable. Both root phosphatase activity and the utilization of inositol hexaphosphate depend on the P supply and nutritional status of plants with regard to P. It is concluded that the rhizosphere is a key site of P transformation with a significant mobilization of P from the non-exchangeable inorganic and organic fractions. Organic P fractions not only play a significant role as a P source but also modify important soil parameters related to the sorption and transport of P in the rhizosphere.     

Calculating changes of legume rhizosphere soil pH and soil solution phosphorus from phosphorus uptake

Abstract

Some legumes are known to reduce rhizosphere soil pH which in turn usually increases soil solution P, P_li and therefore increases P uptake. In an initial experiment with a nonlegume [corn (Zea mays L.)], observed P uptake agreed closely with predicted P uptake while with a legume [alfalfa (Medicago sativa L.)], observed P uptake was greater than predicted P because the rhizosphere was acidified, P_li increased, and more P was absorbed. Using a pot experiment, this investigation calculates the change in rhizosphere pH and P_li necessary to have predicted P uptake obtained with a mechanistic uptake model agree with observed P uptake. The pot experiment was conducted with alfalfa, faba bean (Vicia faba L.) and Austrian winter pea (Lathyrus hirsutus) grown on Chalmers silt loam (fine‐silty, mixed, mesic Typic Haplaquolls) limed to pH levels of 5.72, 6.30, 7.22 and 8.30. Predicted phosphorus uptake at each pH level was calculated with the uptake model using the data for bulk soil. The relation of predicted P uptake to initial soil pH was determined, then this relation was used with observed P uptake to calculate rhizosphere pH. Subsequently, P_li as a function of pH was determined and used to calculate rhizosphere P_li. In this study, the calculations indicate that legumes reduced rhizosphere soil pH by 0.39 to 0.77 units and increased P availability by 20.8 to 241.7%.     

Techniques for observing phosphorus mobilization in the rhizosphere

Summary The techniques described here were developed to visualize the dissolution of sparingly soluble calcium phosphate and the presence of root-borne phosphatase in the rhizosphere. Newly formed calcium phosphate precipitate was suspended in agar containing other essential nutrients. The agar was poured into Petri dishes and acrylglass boxes and was used as a growth medium for seedlings of wheat, rape, buckwheat, and rice. With NH ₄ ⁺ applied as the N source, the precipitate dissolved in the root vicinity and this was attributed to acidification. No dissolution occurred with NO ₃ ^– as the N source. The release of a neutral phosphatase from roots was verified by embedding the roots of young seedlings in agar at pH 7 containing phenolphthalein phosphate. After pH was raised to the alkaline range by adding sodium hydroxide, the agar around the roots turned purple, especially around the roots of P-deprived plants. The most intensive phosphatase activity was found in apical root regions.     

烤烟根际磷库特征及其对有机无机肥配施的响应

为综合分析烤烟根际土壤磷库特征及其对有机无机肥配施的响应,通过田间小区试验,分析比较了烤烟产量、产值、不同等级烤烟比例以及根际土壤磷库特征的差异。结果表明,有机无机肥配施显著提高了烤烟的产量、产值、上等烟比例以及不同形态的磷组分含量。与常规施肥(处理2)相比,化肥减量20%配施有机肥(处理3)、配施生物有机肥(处理4)以及化肥减量30%配施有机肥和生物有机肥(处理5)的产量、产值和上等烟比例平均显著增加了30.00%、59.57%和82.42%,活性磷、中活性磷、稳定性磷以及难溶性磷含量平均显著增加了48.36%、67.15%、16.51%和12.46%,其中活性磷对烤烟产量的形成贡献最大,占到了所有磷组分可解释量的68.23%,以树脂磷Resin-Pi为首要贡献因子,占到了活性磷组分可解释量的68.70%,其次为17.30%的活性磷NaHCO3-Pi和14.10%的活性磷NaHCO3-Po,特别是处理4,各磷组分含量最高,显著增加烤烟产量、产值和上等烟比例的同时,显著降低了中下等烟比例,体现出化肥减量配施生物有机肥的明显产量优势和减肥增效效应。     

水稻根际氮素状况及其利用

A greenhouse pot experiment was conducted with hybrid rice(Oryza Sativa L.) in order to study N Status and utilization in the rhizosphere of rice,The experiment was composed of three treatments:without N,15NH4-N and 15NO3-N .Plant roots were separated from the soil by a nylon cloth,and 1 mm increments of soil,moving laterally away from the roots,were taken and analyzed for various N froms.The labelled N in the plants ranged from 67\51%to 69.24% of the total amount of N absorbed by the rice seedlings with the labelled fertilizer N treatments.This shows that the N in the Plants came mainly from the fertilizers.However,the N absorbed by the rice seedlings accounted for less than 35% of the total amount of the N depletion in the soil near the rice roots,indicating an important N loss in the rhizosphere of rice.The soil redox potential(all treatments)and the concentration of the labelled NO3-N(the labelled NH4-N treatment only) decreased as the distance from the rice roots increased in the rhizosphere of rice.In contrast,the concentration of the labelled NH4-N increased as the distance uincreased in the same soil zone.These results suggested that nifrification occurred in the soil around the rice roots.Therefore,the reason for the N loss in the rhizosphere of rice might be the NO3 movement into the reductive non-rhizosphere soil(submerged) where denitrification can take place.     

Phosphine-induced phosphorus mobilization in the rhizosphere of rice seedlings

Purpose

The aim of this study was to evaluate the role of phosphine in the mobilization of phosphorus in the rhizosphere soil of rice seedlings and to determine the relative efficiency of phosphine in plant P acquisition.

Materials and methods

An indoor simulation experiment was conducted and the matrix-bound phosphine (MBP), phosphorus fractions, and phosphatase activity in the rhizosphere soil samples from rice cultivation, biomass, the plant P, and the root system activity were measured under different phosphine concentrations (0, 1.4, 4.2, and 7.0 mg m^?3) for a period of 30 days.

Results and discussion

The results indicated that phosphine treatments enhanced MBP, inorganic P (resin–P_i, NaHCO₃–P_i, and NaOH–P_i), and phosphatase activity, as well as the root system activity, and the content of P in the rice seedlings was stimulated with increasing phosphine concentrations. However, organic P (NaHCO₃–P_o and NaOH–P_o) accumulation occurred in the rhizosphere of the rice seedlings. In addition, the content of organic P in the soil samples decreased with increased phosphine concentration.

Conclusions

Therefore, relatively high concentrations of phosphine in paddy field could have a positive impact on the effectiveness of phosphorus in rice plants via influencing the rhizosphere properties.

     

施磷量对玉米 -大豆间作根际红壤无机磷形态及磷吸收的影响

通过盆栽模拟试验,探讨不同施磷量对玉米 -大豆间作作物生长及磷吸收的影响,并分析根际红壤中各无机磷形态的变化。结果表明:与单作相比,玉米 -大豆间作显著提高了作物地上部生物量及磷素吸收量,并具有明显的产量优势。与常规施磷水平(P100)下的单作相比,玉米 -大豆间作条件下,磷肥减施 1/2(P50)并未降低作物籽粒产量与玉米的磷吸收量。间作种植显著降低了玉米、大豆根际红壤总无机磷含量,并且无机磷减少量主要以O-P、Fe-P和 Ca-P为主。玉米、大豆根际土壤Fe-P、Al-P、Ca-P与 O-P占土壤总无机磷含量的比例主要受磷水平的调控,而种植模式对玉米和大豆根际土壤中各无机磷形态的比例(除 Fe-P外)均没有影响。在本试验条件下,玉米 -大豆间作通过根系交互作用主要促进土壤中 Fe-P、Ca-P和 O-P的活化来增加玉米与大豆的磷吸收,并具有节约磷肥、维持作物产量和磷吸收的潜力。     

磷肥减施对玉米根系生长及根际土壤磷组分的影响

【目的】 我国农业过量和不合理施用磷肥现象普遍存在,导致磷资源的浪费,对环境也造成潜在威胁。研究减少磷肥用量对玉米产量、根系形态及根际中磷转化特征的影响,为集约化农业生产体系中磷肥合理施用提供技术基础。 【方法】 在河北省衡水小麦玉米轮作体系下连续三年进行了田间试验,在冬小麦季设置4个P₂O₅用量处理:0、112.5、150.0、187.5 kg/hm2,收获后在原处理小区免耕播种夏玉米。利用WinRHIZO根系分析系统分析获取根长、直径等数据,测定玉米籽粒产量、生物量和地上部磷含量及根际土壤中磷形态等指标。 【结果】 与农民习惯磷肥用量(P₂O₅187.5 kg/hm2)相比,3年磷肥用量减施20%~40%处理(P₂O₅150和112.5 kg/hm2),玉米籽粒产量、根系长度与直径和土壤有效磷含量尚未发生明显变化。但3年不施磷处理,根际土壤有效形态磷含量和玉米籽粒产量开始出现下降趋势。2009年和2010年玉米收获期,不施磷肥处理根际土壤有机磷含量低于非根际土壤。2008年玉米苗期和收获期土壤有机磷分组中,中等活性有机磷含量最高;磷肥减施20%~40%处理苗期根际中中等活性有机磷含量显著低于非根际土壤。土壤无机磷形态分组研究发现:从玉米苗期到收获期,各磷肥处理根际和非根际土壤中Ca₂-P下降明显;而不同磷肥处理间土壤中Ca₁₀-P、Ca₈-P、O-P (闭蓄态磷)、Al-P和Fe-P含量差异不显著。减施磷肥处理2008年玉米苗期根际土壤微生物量P含量较非根际土壤高;与习惯施肥量相比,磷肥减施未明显降低根际土壤微生物量磷。 【结论】 在华北小麦玉米轮作种植体系下,在土壤肥力水平较高地区,连续3年将小麦季磷肥的习惯用量减少20%~40%,对夏玉米产量、根系形态以及根际土壤无机磷、有机磷、微生物量磷含量影响尚不明显,因此,该地区磷肥施用量可从习惯用量的P₂O₅180 kg/hm2减至112.5 kg/hm2。     

Dynamics and availability of phosphorus in the rhizosphere of a temperate silvopastoral system

A field rhizosphere study was carried out over a period of 12 months on a 6-year-old silvopastoral trial in New Zealand. The trial comprised radiata pine (Pinus radiata) with lucerne (Medicago sativa) and perennial ryegrass (Lolium perenne) understoreys. The study was initiated because of the unique interrelationships between roots in silvopastoral systems and a paucity of understanding about the processes involved in phosphorus (P) dynamics in temperate silvopastoral systems. Improving our understanding in this area has important implications for nutrient management in silvopastoral systems. Rhizosphere soils were analysed to determine inorganic (Pi) and organic (Po) P fractions, macroporous resin Pi and Po, phosphatase enzyme activity, microbial biomass carbon and pH. Concentrations of labile Pi were consistently greater and Po lower in tree rhizosphere soil compared to the companion understorey, indicating that radiata pine when grown with a productive understorey mineralised Po to a greater extent than either understorey species. Tree rhizosphere soil from under lucerne and lucerne rhizosphere soil contained the lowest concentrations of total Pi and Po compared with tree under ryegrass and ryegrass rhizosphere soils. This was partly attributed to higher levels of phosphatase enzyme activity in the lucerne rhizosphere soils. The results suggest the combination of lucerne with radiata pine may enhance greater utilisation of soil P, although this requires further investigation. Lower levels of labile Po, and higher levels of labile Pi and phosphatase enzyme activity, were determined in tree and understorey lucerne and ryegrass rhizosphere soils in spring compared with autumn. This data confirmed that overall rates of soil organic P mineralisation are greatest in spring.     

Nutrient distribution across wheat rhizosphere with oxamide and ammonium sulfate as N source

Analysis of the behavior of slow releasing nitrogen fertilizers in the rhizosphere soil of agricultural crops is essential for their effective use. This work presents a comparative study of the effects of oxamide and ammonium sulfate as different N sources on the relative mobility of some nutritionally important anions and cations and their relevance to plant growth, root development, and pH distribution pattern in the rhizosphere of wheat (Triticum aestivum cv. Nourin No. 61). Experiment was conducted on a Japanese upland alluvial soil through a rhizobox approach. In the central compartment (CC) of the oxamide and ammonium sulfate treated rhizoboxes, four uncontaminated and homogeneous wheat seedlings germinated on a sterile petridish were grown for nearly two months. During the growing period plant height was recorded weekly. After the growing period, rhizoboxes were dismantled for soil sampling and photography of roots. Soil samples from each compartment of the two rhizoboxes were used for the analysis of CI^-, N0₃ ^-, SO₄ ^2-, Ca²⁺, Mg²⁺, K⁺, NH₄ ⁺-N, N0₃ ^--N and measurement of pH. Compared with ammonium sulfate, the distribution of anions and cations from the distant compartments to the central ones over a distance of 3–5 mm along with a better plant growth, high rooting density, and high pH confirmed that oxamide was an efficient nitrogen fertilizer.     

Nutrient status of wheat crop in Ludhiana

Abstract

Samples of wheat plants from 5 selected villages of Ludhiana (Punjab, India) were analysed for P, K, Ca, Mg, Zn, Cu, Fe and Mn. The dominant nutritional deficiencies are found to be those of zinc and copper. The extent of hidden hunger is in the order of Zn > Mg > Cu > K. The low concentrations of Zn and Cu are ascribed to the inherent poor fertility status associated with the lighter texture and low organic matter content. The data suggest that the low concentrations of Mg may be due to high availability of K in some soils. A sharp decline in the higher concentrations of P, K, Mg and Zn with the advancement in the growth stage suggests the importance of stage of growth at the sampling time in evaluating the leaf analysis data.     

一株溶磷细菌的分离、鉴定及其溶磷特性研究

从作物根际土壤样品中筛选到一株溶 P 能力强的菌株 GJT-1,结合生理生化指标和16S rDNA 序列分析鉴定其为假单胞菌(Pseudomonas sp.).菌株 GJT-1 对磷酸三钙、磷酸铝、磷酸铁有一定的溶解能力,28℃培养到第 3 天对磷酸三钙液体培养基的溶 P 量可达 224.51 mg/L.该菌对开阳磷矿粉和宜昌磷矿粉的溶 P 量分别为 194.25 mg/L 和 120.59 mg/L.通过扫描电镜观察到接种活菌处理的磷矿粉表面凹凸且有黏性物质附着,表明菌株 GJT-1 可利用磷矿粉.     

Carbon and phosphorus transformations during decomposition of pine forest floor with different phosphorus status

Summary Information on the mineralization of inorganic phosphate (P_i) from organically bound P (Po) during decomposition of forest floor and soil organic matter is vital for understanding P supply in forest ecosystems. Carbon (C) and phosphorus (P) fluxes were determined for forest floor samples from three Pinus radiata plots which had received no P (Control), 62.5 kg P ha^–1 (Low P) and 125 kg P ha^–1 (High P) 20 years before sampling. The P concentration of the forest floor samples had increased with fertilizer application, and the C:P ratio ranged between 585 and 1465. During a 9-week laboratory incubation 8.2–19.0% of the forest floor C was evolved as CO₂-C. The amount of CO₂ evolved from the forest floor of the Control plot was more than twice the amounts from the Low P and High P plots. There was little change in net P mineralization in the Control and Low P treatments throughout the incubation, but it increased slightly for the High P samples, suggesting a critical forest floor C:P ratio of 550 for net P mineralization. Changes in the ³²P-specific activities of the P_i and microbial P pools during incubation, and concurrent changes in microbial-³²P and ³²P_i, indicated internal P cycling between these pools. The rate of internal P cycling varied with forest floor quality, and was highest in the High P forest floor. The High P samples had microbial C:P ratios of 22 : 1 which remained constant during the incubation, suggesting the microorganisms had adequate P levels. Received: 2 July 1997     

磷素供应对三种蔬菜磷吸收分配的影响

采用营养液培养的方法,研究不同磷浓度对小白菜、樱桃萝卜和菜豆的干重以及磷素吸收的影响。结果表明,3种蔬菜各器官的干重和吸磷总量与溶液磷浓度呈抛物线形关系,高磷浓度显著抑制了3种蔬菜根部的生长,与对照相比,小白菜、樱桃萝卜和菜豆在P浓度2.0 mmol/L处理的根部干重分别降低了20.0%、26.3%和20.0%,差异达到显著水平。随溶液磷浓度的增加,3种蔬菜的根冠比逐渐降低,蔬菜各器官(除豆荚外)的全磷含量显著增加。樱桃萝卜、小白菜和菜豆各处理茎叶的全磷含量比对照分别增加了47.5%~94.9%、45.6%~87.7%和44.6%~70.8%。高磷浓度下蔬菜奢侈吸收磷养分。菜豆各处理豆荚的全磷含量无显著差异,且随溶液磷浓度提高,豆荚吸磷量占总吸磷量的比重逐渐降低。     

Soil phosphorus mobilization in the rhizosphere of cover crops has little effect on phosphorus cycling in California agricultural soils

Phosphorus (P) is a key limiting factor in many terrestrial ecosystems because most soil P is bound to soil minerals or organic matter. Increasing P cycling rates can increase P availability, including in agricultural soils that receive external P inputs. For example, cover crops may increase P cycling rates via plant uptake and P release during microbial decomposition. Cover crops and associated microbes may also change rhizosphere properties and stimulate soil P mobilization. We studied the potential of legume – fava bean (Vicia faba), vetches (Vicia dasycarpa, Vicia sativa, Vicia benghalensis) pea (Pisum sativum) – and cereal – rye (Secale cereale), wheat (Triticum aestivum), oat (Avena sativa) – cover crops to stimulate P cycling across management practices in two long-term systems trials in California. We measured cover crop biomass and nutrient content, P-mobilizing capacity (pH, organic acids, phosphatase activity) and soil P fraction changes in the rhizosphere. Cereals generally produced more biomass with similar P content compared to legumes, but higher C:P in cereal residues could favor microbial immobilization, delay residue mineralization and reduce P cycling rates. Legumes, especially fava bean, had the largest effect on rhizosphere properties by reducing pH and increasing organic acids concentrations and phosphatase activity. However, these changes in rhizosphere properties had a modest impact on soil P and did not increase soil P availability. Furthermore, we found no strong effect of management practices or soil P concentrations on soil P mobilization. Our results suggest that P mobilization in the rhizosphere of legumes is unlikely to increase P cycling rates in these soils, whereas P uptake and release in cereal biomass could have stronger effects.     

玉米田间根际微区钾养分状况的研究

选取１５年长期定位试验的ＣＫ、ＮＰ与ＮＰＫ等３个处理小区,用自制的根箱埋入田间进行研究。结果表明,生长３０天时,ＣＫ和ＮＰＫ处理在距表根１～２ｍｍ处出现了钾的富集,ＮＰ处理则处于亏缺;生长６０天时,３个处理均处于亏缺状态,亏缺区和亏缺率明显比３０天时变宽和加大。