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根系分泌物在土壤-植物养分循环和缓解植物环境胁迫方面具有重要作用。根系分泌物的收集是研究植物根系过程和相应机制的基础。通常所用的溶液收集法简单易操作,但由于人为扰动大,不能反应根系分泌物的真实情况。介绍了一种新型根系分泌物原位连续采样装置,该装置由根系生长箱和根系分泌物收集装置二部分组成。根系生长箱中土壤和根系之间由滤膜隔开,土壤中的营养元素可以透过滤膜供应植物生长,带有真空抽气泵的根系分泌物收集装置可以实现用去离子水原位淋洗根系、收集根系分泌物的目的。该收集装置外源葡萄糖加标回收率为89%±2%。小麦种植在根系生长箱中,在小麦生长42 d期间,用新型采样装置和溶液收集法分别收集了根系分泌物,研究了小麦根系分泌DOC能力随生长时间的变化。结果表明,收集方法不同,小麦根系分泌DOC能力随生长时间变化不同。在新型收集装置法中,小麦根系分泌DOC能力随着生长时间呈现降低的态势,而溶液收集法则呈现出上升的态势。新型采样装置能实现植物土壤生长条件下原位收集根系分泌物,采样中扰动小,为根系分泌物研究提供了较好的收集方法。但也存在设备复杂、采样流量不易控制等缺点,是今后需要改进的方向。 相似文献
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一种新型根系分泌物收集装置与收集方法的介绍 总被引：2，自引：0，他引：2
根系分泌物在养分活化、改善环境胁迫方面具有重要作用,很多科技工作者对根系分泌物的研究表现出极大兴趣,取得了一系列进展。但土壤栽培条件下,根系分泌物收集是一个难点。本文介绍了一种新型根系分泌物的收集装置与收集方法。该装置由根系生长箱和分泌物收集箱组成,植物在生长箱土壤中生长,通过定向引导作用,根系从生长箱穿过琼脂层进入收集箱中生长,待收集箱内积累一定根系后,通过淋洗收集箱内的介质,实现根系分泌物收集。研究发现,利用该装置收集分泌物,植物总根尖数的90%分布在收集箱。外源有机酸加样回收率可达70%以上。土壤栽培条件下,随生长时期延长,大豆有机酸分泌量逐渐增加,苹果酸分泌量高于柠檬酸。而且土壤栽培条件下大豆柠檬酸和苹果酸分泌量是溶液栽培时的11.4倍和6.7倍。上述研究表明,该装置可以用于土壤栽培条件下根系有机酸的分泌研究。 相似文献
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根系分泌物是植物保持根际微生态系统活力的关键因素，也是根际物质循环的重要组成部分，对根际土壤生态环境中的物质循环具有重要的驱动作用。根系分泌物可以刺激微生物生长，增强其活性，加速根际养分循环，增加土壤养分利用率，并在小规模空间引起温室气体通量的变化。此外，它也是植物参与竞争的重要策略，植物通过根分泌物以获取种间长期生存的养分，甚至分泌对自身有害的化感物质来排挤其他植物，实现自我生存，即使存在自毒作用或引起连作障碍等。植物的健康生长依赖于自身与土壤微生物复杂动态群落的相互作用，但是根际微生物群落结构和组成却又受植物物种、植物生长期、土壤性质、功能基因等因素影响，这些因素的动态变化可能导致根系分泌物的多样化，从而形成复杂多变的根系分泌物与植物的关系，进而影响植物的健康生长。目前，对植物根系分泌物的研究是土壤生态学、植物营养与代谢等领域的研究热点，且随着分析技术手段的快速发展，根系分泌物相关研究也逐渐深入，进一步揭示植物与微生物间的协同作用机理对农、林等行业生产具有重要的指导意义。 相似文献
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植物对不同形态磷响应特征研究进展 总被引：2，自引：1，他引：1
磷是植物生长发育所必需的大量营养元素之一,参与植物体内许多重要化合物的合成与代谢。土壤中磷素具有多种形态,且不同形态磷的植物有效性差异较大;植物在不同形态磷环境下,体内会形成相应的适应性机制。植物吸收积累磷通常与根形态、根系分泌物、体内磷转运等因素有关,受到特异基因表达的调控。了解植物对磷的吸收积累特性是筛选磷高效植物或磷富集植物的前提,也是充分利用土壤磷素资源、修复磷过剩环境的关键。根据国内外研究现状,本文从磷素吸收积累、根系形态特征、磷酸酶与植酸酶的变化以及磷营养高效的分子机制,综述了植物对不同形态磷的响应特征,并对未来该领域的研究进行了展望。 相似文献
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土壤—植物根际磷的生物有效性研究进展 总被引：14，自引：0，他引：14
探讨土壤－植物根际磷素养分状况及利用机理，提高土壤磷的生物有效性，使土壤中潜在的难溶性磷库活化，提高磷肥利用率，对促进农业生产的持续发展和陆地生态系统的良性循环具有重大的现实意义。文章从这一角度出发，论述了根际土壤中根际微生物，根际pH值，根系分泌物，菌根，根际土壤磷酸酶等各种因素对提高土壤磷素利用率的机理。 相似文献
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南方黏质红壤土壤机械阻力高,本文采用两种植物根系分泌物处理土壤,分析其对两种压实情况下的土壤机械阻力（SPR）影响。通过水培法提取须根系植物香根草和主根系紫花苜蓿根系分泌物,分析其组成特征、并冷冻干燥获取分泌物干物质。分泌物干物质按照4种施加水平处理土壤,之后对平衡后的重塑环刀土壤实施两种压实处理,并分析土壤SPR、含水量（SWC）、团聚体和容重。结果表明：紫花苜蓿根系分泌物中芳香基碳类、烷氧基碳类和羰基碳类相对含量（3.23%、6.83%、55.09%）较香根草高（1.64%、4.12%、45.78%）,而疏水物质/亲水物质则呈现相反趋势。SPR随分泌物施加水平升高而降低,但只有施加水平≥0.2 mg·g-1时引起土壤SPR显著降低,且紫花苜蓿降低SPR幅度较香根草明显。相关性和回归分析证明根系分泌物中较低的疏水性物质/亲水性物质比和较高的烷氧基碳类相对含量,通过增加SWC和团聚体平均质量直径降低土壤SPR。综上所述,主根系植物根系分泌物对黏质红壤SPR的缓解效果优于须根系植物。 相似文献
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The rate of phosporus (P) release from soils can significantly influence P fertility of soils. The objectives of this study were to investigate the effects of land‐use types on the kinetics of P release under different management practices and the relationship between kinetic parameters and soil physical and chemical properties from calcareous soils. The kinetics of P release in 0.01 M CaCl2 was studied in surface samples of 30 calcareous soils planted to garlic, garden, pasture, potato, vegetables, and wheat. Trend in P‐release kinetics was similar between land‐use types. Significantly different quantities of P were released under different land use. The maximum amount (average of five soils) (46.4 mg kg–1) of P was released in soil under potato and the minimum amount (10.4 mg kg–1) under pasture. The kinetics of P release from soils can be described as an initial rapid rate followed by a slower rate. Different models were used to describe P release. In general, parabolic diffusion and power equation were found to be appropriate for modeling P release. The P‐release rate for the soils was estimated by parabolic equation for the studied land‐use types. The constant b was lower for pasture and wheat than for garlic and potato. The relationship between the rate of P release with Olsen‐P was linear, while it was curved with respect to the CaCl2‐P, indicating that release of P was diffusion‐controlled. When the kinetic parameters of models were regressed on soil properties, CaCl2‐P and CaCO3 appeared to be the most important soil properties influencing P‐release rates in these soils. 相似文献
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《Communications in Soil Science and Plant Analysis》2012,43(18):2188-2199
A column leaching experiment using three soils (Inceptisol, Ultisol, and Andisol) and seven livestock manure composts that had different characteristics was conducted for 19 weeks to investigate the interactive effects of composts and soils on the phosphorus (P) leaching potential of compost-amended soils and to identify the principal variables that affect P leaching. Cumulative total P leaching (TPcum) tended to increase with increasing total and available P concentration in the soils. Among various compost properties, total P concentration was positively correlated with TPcum from the compost-amended soils, except for the Andisol, which has a high P-sorption capacity. There was no significant relationship between TPcum and water-extractable P concentration of the composts, suggesting that total P rather than inorganic P concentration of composts may be successfully used in predicting P leaching potential from compost-amended soils except for soils that have a high P-sorption capacity, as in Andisol. 相似文献
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《Communications in Soil Science and Plant Analysis》2012,43(7):1259-1271
We investigated effects of phosphorus (P) and iron (Fe) on root elongation (RE) of lettuce in arsenic (As)–spiked soils using response surface methodology (RSM). To stabilize interactions between As and Fe in a soil preparation, the sequential incorporation method using Fe and P (SIMFe-P) was applied. From a phytotoxicity assay, As in roots (Asroot) was negatively associated with RE, Fe in soils, and P in roots and soils. The P in roots was also positively related to RE. In a model study, As and interaction factor between P and Fe showed negative coefficients but others showed positive ones. From a confirmation study, RE on exposure to As was verified to be much greater in soils treated by SIMFe-P than in soils separately treated with both elements. These results indicated that application of SIMFe-P to As-contaminated soils might be expected to have an advantage during the early stage of plant root growth. 相似文献
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The relationship between organic P status of 4 soils, 20 microorganisms isolated from these soils (2 bacteria and 3 fungi for each soil) and 13 dominant plant species of typical natural ecosystems of these soils was evaluated. The soils used were represented by two pairs with different ratios of monoester and diester P, and of DNA and other diester P. A Dystric Podzoluvisol and an alpine Umbric Leptosol were characterized by a relatively high proportion of diester P including much DNA P, while a Calcic Chernozem and subalpine Umbric Leptosol had lower proportion of diesters containing relatively less DNA P. The proportions of P compounds in bacteria and plants were very similar on average, based on the monoester to diester P ratio and on the proportions of different diesters in alkaline extract, whereas fungi contained considerably higher proportions of monoesters and polyphosphates, and a higher proportion of phospholipids in the diester fraction. The results showed that the Porg composition of NaOH extracts from different soils was more similar to the composition of extracts from different groups of microorganisms. There was no clear correspondence between soil and microbial diester P proportion and composition. A high proportion of polyphosphate P including pyrophosphate P in soil extracts indicates a significant contribution of fungal P compounds in the soil while the monoester to diester P ratio, and DNA to non-DNA P ratio should be used with caution to interpret the origins of soil Porg. The relative contributions of microorganisms and plants to monoester and diester P in soils is only partially understood. 相似文献
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Microbial biomass phosphorus and its significance in predicting phosphorus availability in red soils
《Communications in Soil Science and Plant Analysis》2012,43(5-6):655-667
Abstract Red soils are widespread in Southern China and other subtropical regions in the world. An improved management of phosphorus (P) is crucial for sustainable agriculture and environmental quality in red soil regions. Plant‐availability of P in red soils mainly depends on fertilization and biological cycling. Both laboratory analyses and greenhouse experiments were conducted to examine the relationships between plant P uptake, chemical index of P, and microbial biomass P in red soils with different fertility levels. Microbial biomass P ranged from 2.1 to 43 mg kg‐1 in the red soils and was significantly correlated with total P (r=0.84*), organic P (r=0.87*), or Bray I extractable P (r=0.94**). Extractable P plus organic carbon accounted for >85% of the variation in microbial biomass P in the red soils. The significant relationship between microbial biomass P and extractable P suggests that microbial biomass P has a great potential in predicting P‐supply ability in soil. Greenhouse experiments showed that there were close relationships between ryegrass dry matter yield, plant P uptake or tissue P concentration and microbial biomass P in the red soils. The corresponding correlation coefficients were 0.79*, 0.90*, and 0.91*, respectively. These results imply that microbial biomass P plays an important role in the availability of P to plants, and is a potential biological index of P availability in the red soils. 相似文献
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《Communications in Soil Science and Plant Analysis》2012,43(6):619-628
Abstract Four important soils of Thailand were studied in the laboratory and greenhouse to determine the relationship between the relative uptake of P by tomato plants, the P in the presence of added P absorption maximum, and the bonding energy. The relative uptake of P was higher in soils which had low initial available soil P and was lower in soils that had an initially high P status. The sorption of P was less in those soils which had the higher initial water‐soluble P. Generally, as the absorption maximum and bonding energy of the soils decreased, the relative yield response to added P increased. 相似文献
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Organic P was investigated in humic acids extracted from mountain soils developed in the subalpine, upper subalpine and alpine zones of the Northern Caucasus. P contents of humic acids varied between 3.4 and 14.2 g P kg?1, depending on P contents of the parent vegetation and on site conditions. Organic P was accumulated at sites where microbial activity is restrained due to soil acidity, low soil temperature and hydromorphy.31 P NMR spectroscopy revealed that orthophosphate monoesters were the dominent P species (72–85% of extract- able P), orthophosphate diesters amounted to 12–21%, and phospho- nates ranged between 0 and 9%. Humic acids of soils under cold and wet climatic conditions showed highest concentrations in phospho- nates and orthophosphate diesters. Hence, the accumulation of organo-P in the Caucasian mountain soils was partly due to increasing proportions of potentially available organic P species. 相似文献
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Phosphorus (P) speciation in 21 basaltic and four non-basaltic Irish grassland soils was determined by NaOH–EDTA extraction and 31 P NMR spectroscopy. Organic P in basaltic soils ranged between 30 and 697 mg P kg−1 and consisted of phosphate monoesters (84–100%), DNA (0–16%) and phosphonates (0–5%). Inorganic P was mainly phosphate (83–100%) with small concentrations of pyrophosphate (0–17%). Phosphate monoesters were more important as a proportion of extracted P in basaltic soils, probably because of their greater oxalate-extractable Fe and Al contents. Phosphate monoesters appeared to be strongly associated with non-crystalline Al and increased with total soil P concentration, indicating that they do accumulate in grassland soils. In non-basaltic soils myo -inositol hexakisphosphate constituted between 20 and 52% of organic P, while scyllo -inositol hexakisphosphate constituted between 12 and 17%. These compounds were not quantified separately in basaltic soils because of poor NMR resolution in the phosphate monoester region, but appeared to represent a considerable proportion of the organic P in most samples. DNA concentrations were greater in basaltic soils compared with non-basaltic soils and were associated with acidic pH and large total C contents. The inability of the Olsen P test to assess effectively the P status of basaltic soils may result from strong phosphate sorption to Fe and Al oxides, inducing plant utilization of soil organic P. Phosphorus nutrient management should account for this to avoid over-application of P and associated financial and environmental costs. 相似文献
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《Communications in Soil Science and Plant Analysis》2012,43(10):1540-1556
Evaluation of five soil phosphorus (P) extractants was done on southwestern Nigerian soils from sedimentary and basement complex parent materials to determine the relationship between the extractants and the most appropriate extractant for the soils. The soils differed in properties. Generally, soils from the basement material had less available P compared with sedimentary material. Olsen extracted the greatest P. Bray 1 measured 67% of Olsen P, Hunter measured 52%, Mehlich measured 42%, and Ambic measured 24%. Positive and significant regression (P < 0.001) existed among Bray 1, Olsen, Mehlich, Hunter, and Ambic extractants. The strongest relationship was found among Olsen, Mehlich, and Ambic P. The relationship between maize P uptake and extracted P was quadratic, whereas the relationship with Mehlich was logarithmic. Bray, Mehlich, and Olsen P were the significant contributors to the maize P uptake and dry-matter yield. Extractants in order of P extraction were Olsen > Bray 1 > Hunter > Mehlich > Ambic. 相似文献
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澳大利亚东部地区一些酸性硫酸盐土壤磷的特征 总被引：1，自引：0，他引：1
Forty-five acid sulfate topsoil samples (depth < 0.5 m) from 15 soil cores were collected from 11 locations along the New South Wales coast, Australia. There was an overall trend for the concentration of the HC1-extractable P to increase along with increasing amounts of organic C and the HCl-extractable trivalent metals in the topsoils of some less-disturbed acid sulfate soils (pH < 4.5). This suggests that inorganic P in these soils probably accumulated via biological cycling and was retained by complexation with trivalent metals or their oxides and hydroxides. While there was no clear correlation between pH and the water-extractable P, the concentration of the water-extractable P tended to increase with increasing amounts of the HCl-extractable P. This disagrees with some established models which suggest that the concentration of solution P in acid soils is independent of total P and decreases with increasing acidity. The high concentration of sulfate present in acid sulfate soils appeared to affect the chemical behavior of Pin these soil systems. Comparison was made between a less disturbed wetland acid sulfate soil and a more intensively disturbed sugarcane acid sulfate soil. The results show that reclamation of wetland acid sulfate soils for sugarcane production caused a significant decrease in the HCl-extractable P in the topsoil layer as a result of the reduced bio-cycling of phosphorus following sugarcane farming. Simulation experiment shows that addition of hydrated lime had no effects on the immobilization of retained P in an acid sulfate soil sample within a pH range 3.54.6. When the pH was raised to above 4.6, soluble P in the soil extracts had a tendency to increase with increasing pH until the 15th extraction (pH 5.13). This, in combination with the poor pH-soluble P relationship observed from the less-disturbed acid sulfate soils, suggests that soluble P was not clearly pH-dependent in acid sulfate soils with pH < 4.5. 相似文献