解磷菌剂对作物生长和土壤磷素的影响

利用课题组自行分离筛选的B2和B67解磷菌株研制的菌剂，在盆栽和大田试验过程中，菌剂在增加作物产量的同时，有提高土壤速效磷含量、培肥土壤的作用，而且是菌剂和化肥配合施用效果显著。施用了解磷菌剂或菌剂和化肥配合施用后，盆栽玉米的株高、鲜重和干重，较CK增加15．2％～89．2％，玉米单株吸养量较CK增加20％～146％；青菜的鲜重、干重和生物量较CK增加15．8％～41．6％，和CK比较差异显著；小麦的株高、有效小穗数、穗粒数、粒重以及生物量也较CK差异显著，大田试验的几种作物也有不同程度的增产。另外B2和B67接种到山西省典型土壤中，土壤速效磷含量较CK增加1．35～3．04倍，且发现其溶磷效果和土壤磷酸酶活性与有效活菌数相关，解磷菌剂在提高土壤速效磷含量的同时，也有提高土壤速效钾含量的作用。     

生物有机肥中磷细菌对难溶性磷的有效化研究

通过土壤盆栽试验，在生物有机肥中加入固氮菌、磷细菌、硅酸盐细菌等有益微生物并与磷矿粉混合施用来栽培玉米，研究其中的磷细菌对土壤中难溶性磷的有效化作用。结果表明，在不施肥、施用磷矿粉、含磷细菌生物有机肥、不含磷细菌生物有机肥4个处理中，处理3更能促进玉米的生长、增加植株体内NPK养分的积累，特别是在肥力较低的土壤上表现更为显著。处理3也提高了土壤中的速效磷养分含量。     

Molecular Aspect of Al Tolerance in Crop Plants: Novel Al-Activated Malate Transporter Gene in Wheat Roots

Aluminum (Al) is a major element in the soil; 30–40% of arable land is acidic. Solubilized Al ion in acid soils inhibits root elongation. Intensive research on the Al tolerance mechanism has been conducted in the past few decades. Mechanism of Al tolerance can be classified into Al exclusion mechanism and intracellular tolerance mechanism. Efflux of organic acids from roots upon receiving the Al signal is the major Al exclusion mechanism. Efflux of organic acids through the channel in the plasma membrane was confirmed, and the gene specifically encoding malate transporter in Al-tolerant wheat was discovered recently. The regulatory mechanism in the efflux of organic acids upon protein phosphorylation may be operative. The production of reactive oxygen species (ROS) and their scavenging system are thought to be important in the intracellular tolerance mechanism.     

豫东沙区冬小麦套作花生轮作制度中磷肥分配施用效果的研究

在豫东沙区进行冬小麦套作花生轮作制度中磷肥分配施用效果试验。结果表明:冬小麦套作花生生长周期中土壤速效磷的变化规律为“冬低夏高”,最低值出现在冬小麦出苗至起身期,最高值出现在花生苗期至结荚期,施用磷肥不改变这一规律;施用磷肥具有明显的以磷增氮效应,冬小麦和花生的氮素吸收利用率分别增加7%~20%和12%~24%;在冬小麦套作花生轮作周期中磷肥分配应掌握“重冬轻夏”的原则,但在土壤速效磷含量较低、磷肥相对不足情况下,一次大量集中施用应慎重。     

铝胁迫对小麦根尖细胞蛋白质及苹果酸分泌的影响

以一对近等位基因小麦品系(ET8和ES8)为材料,研究了铝胁迫条件下根系生长情况,根尖铝含量,根尖细胞质蛋白组分以及铝胁迫下两个小麦品系苹果酸分泌的差异。结果表明,小麦品系ET8的耐铝性明显高于ES8;而ET8根尖铝含量则明显低于ES8;50mol/L铝处理24h后ES8小麦的细胞质蛋白组成受到明显影响,而ET8则无明显影响。由于铝胁迫条件下ET8分泌的苹果酸的量明显高于ES8,因此可以认为,分泌的苹果酸一方面与铝结合使其无毒化;另一方面将铝排斥于根尖细胞外,从而阻止铝进入细胞质内对细胞产生毒害作用。     

Harmonisation, standardisation for soil and sediment fractionation studies, and usefulness in assessment and risk management

Single and sequential extraction procedures are often used to study the environmental fate of trace elements from soils and sediments. Although these schemes are quite popular, they are prone to various sources of errors, which require them to be thoroughly controlled. Owing to their operationally-defined character, the only way to compare analytical data is to stick closely to procedures that have been collaboratively studied and written in the form of an operating protocol. Groups of scientists have hence developed ‘harmonised’ procedures that are used as a reference for fractionation studies. A higher level is the formal standardisation of the procedures by official standardisation bodies, which also fulfils the need for achieving the comparability of data obtained by different laboratories from different countries. This paper discusses aspects of harmonisation (consensus obtained by groups of scientists) and standardisation (adoption of standards as mandated by an international organisation) as applied to single and extraction schemes for trace element fractionation studies, including quality control aspects.     

pH对针铁矿表面磷酸盐吸附的化学形态的影响

Chemical forms of the phosphate adsorbed on goethite surfaces and characteristics of the coordinate groups which exchange with P on goethite surfaces in solutions with different pll values were investigated.Results showed that the chemical forms of P on goethite surfaces changed from the dominance of monodentate corrdination to that of bidentate one with increasing pH of the solution.By influencing types of phosphate ions in solutions,pH affected the chemical forms of P on goethite surfaces,The amount of OH^- displaced by phosphae on goethite surfaces was the most at pH 7.0,the second at pH 9.0,and the least at pH 4.5.     

根－土界面区域磷酸盐的分布和移动: Ⅱ. 土壤水分含量和磷酸盐施用量的影响

The phosphate in the soil-root interface zone under various soil water contents and application rates of phosphate was still of depletion distribution which could be described by a power function in the form of C/Co= ax^b(C/Co is the relative content of fertilized phosphate in a distance from the root surface x, a and b are the regression constants). The depletion rate of phosphate in soil near the root surface was higher and the depletion range was narrower under lower soil moisture. On the contrary, at higher soil water content the depletion range was wider, generally. The application rate of phosphate led to the greater depletion intensity of phosphorus was higher in the heavier texture soils. In general, the depletion intensity in the soils, which decreased with increasing clay content or increasing buffering power of soil, decreased in the order as loessal soil and black lou soil > lou soil > yellow cinnamon soil when 50 or 100 mg of phosphorus were applied in the form of KH₂PO₄. This result indicated that the phosphate distribution and its movement in the soil-root interface zone closely related with the buffering capacity of soil.