改性磷矿粉在石灰性土壤上的生物有效性及其机理研究

为缓解磷资源危机,充分利用不适于化学加工的磷矿资源,对磷矿采用活化技术开发利用,由此生产的改性磷肥已被证明在酸性土壤上有很高的生物有效性,但在石灰性土壤上的研究还比较少。本文选择4种不同产地(云南昆明、四川德阳、四川绵竹和贵州开阳)的磷矿粉,分别用有机活化剂和无机活化剂进行活化处理,制备改性磷矿粉,并就其在石灰性土壤对苗期春小麦的生物有效性进行了盆栽试验。结果表明,4种磷矿粉经活化处理后有效磷和水溶性磷含量均明显增加,无机活化剂提高了有效磷的含量,而有机活化剂对水溶性磷的提高幅度较大。改性磷矿粉处理均不同程度提高了石灰性土壤上春小麦的生物量干重、植株吸磷量和磷利用效率,有机活化剂处理制备的改性磷矿粉对春小麦生长的促进作用更为明显。运用红外光谱谱学技术对4种磷矿粉及相应的8种改性磷矿粉结构分析结果表明,磷矿粉经改性后其结构发生了明显变化,H2PO4和HPO42的特征谱带明显增加,增加的程度因磷矿粉的产地和活化剂种类不同而有差异。对磷矿粉化学成分分析结果表明,不同产地的磷矿粉其磷以及钙、铁、铝、镁等化学成分的含量差异较大,活化剂对磷矿粉的活化效果与磷矿粉本身的氧化物含量有关。在本试验条件下,磷矿粉Ⅲ(四川绵竹)的活化效果相对最好,与其氧化镁含量最高、总氧化物含量最低有关。不同类型活化剂对磷矿粉的活化效果不同,红外光谱分析结果表明,无机活化剂活化效果较好,而土培试验结果表明有机活化剂的活化效果较好,这一结果有待进一步的研究。     

RESIDUAL EFFECTS OF PHOSPHORUS SOURCES IN GRAIN AMARANTH PRODUCTION

Productivity of grain amaranth can be improved at a reduced cost through combined use of low-cost rock phosphate (RP) phosphorus sources as well as selection of amaranth varieties with high phosphorus (P) use efficiencies. Rock phosphate sources are known to exhibit differences with respect to grain yield, disease tolerance and P use efficiency (PUE) in amaranth varieties. However, very little is known about their residual release of P. It is probable that the differential performances exhibited by the RPs might be a function of their P residual properties after cropping. Based on these premises this study was carried out to evaluate the residual effects of P sources under continuous croppings for grain amaranth production. The study was a factorial experiment with four replications. Four P sources: single super phosphate – SSP, ogun rock phosphate – ORP, sokoto rock phosphate – SRP, and control; three amaranth varieties: NH84/493, NH84/445 and NH84/452 were factorially combined with two soil types: Kandiudult and Haplustalf. In order to monitor the residual effects of the P sources the experimental plots were cropped consecutively three times. Results from the study revealed that sandy loam Haplustalf was better than the clayey Kandiudult soil in improving grain amaranth yield under continuous cropping system. Grain yield and relative agronomic efficiency (RAE) decreased with continuous cropping for SSP but increased with continuous cropping for ORP and SRP till second cropping, thereafter there was a decrease. Averaged over the three continuous consecutive croppings, SRP and ORP were 68.9% and 73.5% as effective as SSP in increasing grain yield respectively. It was concluded therefore that ORP and Haplustalf soil are best options for grain amaranth production under continuous cropping system.     

Effect of two moisture regimes on P-release from P treated soils

Understanding phosphorus (P) release under different climatic or moisture regimes will facilitate effective management of plant nutrition. The objective of this study is to evaluate the effect of two soil moisture regimes on P release from Ogun rock phosphate (ORP) and Sokoto rock phosphate (SRP) in two soil types. Soil was poured into soil columns to form lower and top layers. Top layer was mixed with 400 kg ha^?1 P from ORP, SRP, single super phosphate (SSP) and leached with 35.4 cm³ water representing low moisture regime (LMR; 400 mm rainfall) and 106.1 cm³ water for high moisture regime (HMR; 1200 mm rainfall). P concentrations of leachates, available P in soil and soil pH were determined. Cumulative P leached was higher under HMR than LMR in both soils. There was more leaching with SSP (0.41–0.97 mg P) than both phosphate rocks (0.008–0.19 mg P) indicating leaching potential of SSP. Cumulative P leached from SSP treated Olokemeji soils was twice that of acidic Sapoba under LMR while they were similar (Olokemeji, 0.97 mg P; Sapoba, 0.94 mg P) under HMR suggesting that LMR enhances fixation of P in acidic soils. Irrigation of P fertilized soils may reduce P sorption in acidic soils.     

草酸青霉菌HB1溶磷能力及作用机制

一些功能微生物具有溶磷能力且同一菌株对不同难溶性磷酸盐的溶解能力存在差异。该研究以草酸青霉菌HB1为研究对象,通过固体平板培养试验、摇瓶培养试验和土壤培养试验系统研究了不同磷源(磷酸钙、磷矿粉、磷酸铁、磷酸铝)与氮源(铵态氮、硝态氮)供应下HB1溶磷能力及其作用机制,并验证了其在高、低不同磷水平土壤中的溶磷能力。结果表明,接种HB1的不同磷源培养基上均有溶磷圈出现,根据溶磷圈直径/菌落直径初步确定HB1溶解磷酸钙的能力较强;摇瓶培养试验表明供试磷源为磷酸钙、磷酸铁时HB1发酵液中有效磷含量为884、265 mg/L(铵态氮),或945、206 mg/L(硝态氮),其溶磷能力不受氮源形态影响;磷矿粉为磷源时,HB1发酵液中有效磷含量可达199 mg/L(供应铵态氮),为硝态氮供应的7.14倍;而磷酸铝为磷源时,HB1发酵液中有效磷含量为120 mg/L(供应硝态氮),为铵态氮供应的3.29倍;此外,供应铵态氮条件下,HB1对难溶性磷酸盐的溶解能力与介质中pH值呈显著的负相关关系。HB1接种于不同磷水平的土壤中培养21 d,在低磷和高磷土壤中HB1均能有效定殖且增加了土壤有效磷含量,比不接菌对照分别增加45.00%和14.17%。综上,草酸青霉菌HB1对磷酸钙和磷矿粉的溶磷效果较好,并通过分泌氢质子酸解含磷矿物实现溶磷作用,且HB1在低磷土壤中溶磷能力较强。     

Changes in Biological Properties in Soil Amended with Rock Phosphate and Waste Mica Enriched Compost using Biological Amendments and Chemical Fertilizers Under Wheat-Soybean Rotation

The main aim of this research work is to prepare an enriched compost using rice straw mixed with rock phosphate, waste mica and Aspergillus awamori and to study their effect on changes in microbial properties in soils with and without chemical fertilizers under wheat-soybean rotation. Data revealed that significant increase in microbial biomass carbon (MBC), dehydrogenase activity, phosphatase activities, and microbial biomass phosphorus (MBP) in soil were maintained in enriched compost than ordinary compost after both the crops. Significant increase in MBC, dehydrogenase activity, phosphatase activities, and MBP were found in surface soil. The maximum microbial activities were observed in the treatment receiving 50% recommended dose of fertilizer (RDF) + enriched compost at 5 t ha^?1 indicating that integrated use of chemical fertilizers and enriched compost significantly improved the biological properties of soil under wheat–soybean rotation thereby enhanced soil fertility and crop production.     

改性磷矿粉对油菜幼苗生长和土壤性质的影响

用γ-聚谷氨酸（γ- PGA）与摩洛哥磷矿粉（MPR）混合处理后,在红壤、黄棕壤、黄褐土上分别进行了油菜幼苗盆栽试验和土壤培养试验。结果表明,盆栽试验中,3种土壤上改性磷矿粉处理的生物量都高于其它处理。红壤上,改性磷矿粉处理与对照（CK）和磷酸二氢钙（SP）相比达到显著差异。改性磷矿粉处理的油菜幼苗含磷量和吸磷量都高于相应的单施磷矿粉处理,甚至显著高于SP;并可提高植株的磷吸收效率和磷肥利用率。在土壤培养试验中,磷矿粉施入3种土壤后,均能提高土壤pH值、有效磷和交换性钙镁含量,降低红壤中交换性铝含量。上述各指标增加或降低幅度大小顺序均为:改性磷矿粉磷矿粉对照。     

细菌溶磷作用与磷矿粉伴生性重金属元素的释放

以4株溶磷细菌和5种磷矿粉为材料,对细菌溶磷作用与磷矿粉伴生性重金属元素释放间的关系进行了研究。结果表明,溶磷细菌在促进磷矿粉中磷溶出的同时,还促进了磷矿粉中伴生性重金属的释放,在测定的6种伴生性金属元素(Zn、Pb、Cu、Co、Ni、Cd)中,Zn最容易随细菌溶磷作用而释放,最多可占该磷矿粉中总Zn量的97.0%,Pb和Cd随细菌溶磷释放率皆低于10%;细菌溶磷作用强度与磷矿粉中各伴生性重金属释放量间的关系因磷矿粉产地和伴生性重金属种类而异。细菌作用于湖南石门磷矿粉和四川马边磷矿粉的溶磷量与Zn、Cu、Co、Ni释放量间(四川马边磷矿粉中Co除外)正相关,但未达到显著水平(r=0.50~0.95,P>0.05),但在溶解贵州开阳磷矿粉时,Zn、Co、Ni的释放量都与溶磷量显著正相关(r>0.88,P<0.05)。     

表面吸附层对磷矿石磷素释放的影响

次生磷矿石表面的Ｃａ－Ｐ吸附层对磷矿石磷的释放有重要影响,以ＮａＣｌ,ＫＣｌ或ＮＨ４Ｃｌ浸提除去磷矿石表面的吸附态Ｃａ,导致了随后的水提取磷的大量增加。认为磷矿石表面的吸附层给磷灰石的加速溶解提供了Ｃａ的接收率。     

Cultivar selection as a tool for managing soil phosphorus and faba bean yield ‎sustainability

ABSTRACT

A sustainable agricultural tactics for countering a possible phosphate shrinking should comprise the releasing of legacy soil phosphorus (P), in parallel to lowering P fertilizer load, and increasing the use of recycled P sources with economic crop yield in mind. Therefore, a field trail was conducted to estimate the possibility of choosing the appropriate cultivar as a tool to raise the use efficiency of reserved soil P. Herein, three faba bean cultivars (Sakha-3, Nubaria-1 and Giza-843) were evaluated under five applications of P fertilizer (rock phosphate, super phosphate, Bacillus megaterium, rock phosphate+B. megaterium, and super phosphate+B. megaterium). Findings showed that the lowest value of estimated available P in soil after harvest was obtained from plots sown by Sakha-3 plants and fertilized with super phosphate+B. megaterium. Plots sown with Nubaria-1 and fertilized by rock phosphate+B. megaterium or B. megaterium (for weight of 100 seeds and seed yield) in addition to super phosphate+B. megaterium (for seed yield) produced the maximum increases. The highest P recovery efficiency was achieved with Nubaria-1 inoculated by B. megaterium alone. In conclusion, super phosphate+B. megaterium × Nubaria-1 achieve maximum crop returns and secure high short-term recovery of applied P.     

中低品位磷矿资源高效利用机制与途径研究进展

磷矿是生产磷肥的原料,是不可再生的重要战略资源。高品位磷矿开采过度,面临枯竭。充分利用中低品位磷矿,是磷资源可持续高效利用的关键。中低品位磷矿有效磷含量低,提高磷的活化利用效率是综合利用中低品位磷矿的核心。然而,对中低品位磷矿的利用大多重视物理和化学方法的活化效应,忽视了植物自身根际效应的活化作用。植物通过调控根系形态与生理,以及根际互作效应,促进对中低品位磷矿养分的活化与吸收。这种基于根际过程的生物活化是磷资源高效利用的重要途径。本文在总结中低品位磷矿中磷的活化方法的基础上,提出了通过强化作物根际效应,挖掘植物的生物学潜力,提高作物对中低品位磷矿的综合利用效率,为磷资源的可持续利用提供科学依据。本文主要从根际效应层面剖析了中低品位磷矿高效利用的技术原理与途径。充分发挥作物高效利用磷的生物学潜力,有效利用作物的根际特性,实现土壤–作物–磷肥的匹配,开发“绿色”新型磷肥将是未来实现磷资源可持续利用的有效途径。加强磷矿中全量养分的综合利用也是未来研究的重点方向。     

Changes in Nutrient Status During Preparation of Enriched Organomineral Fertilizers Using Rice Straw,Low‐Grade Rock Phosphate,Waste Mica,and Phosphate Solubilizing Microorganism

An experiment was carried out to study the changes in nutrient contents during preparation of enriched organomineral fertilizers using rice straw, low‐grade rock phosphate (RP), waste mica, and phosphate‐solubilizing microorganism (Aspergillus awamori). Composting reduced the total carbon (C) but increased total nitrogen (N) content with the progress of composting. This was reflected in the decrease of the C/N ratio. Significant increases in total phosphorus (P) and potassium (K) were also observed where both RP and waste mica was added along with Aspergillus awamori. Ammonium N (NH₄ ⁺‐N) decreased while nitrate N (NO₃ ^?‐N) increased at the end of composting. Olsen P content increased up to 90 days, thereafter decreased up to day 150, whereas ammonium acetate K (NH₄OAc‐K) increased gradually with the progress of composting. The study thus revealed that crop residue could be converted into a value‐added product through composting technology using low‐grade rock phosphate and waste mica along with phosphate‐solubilizing microorganisms.     

Do cover crops change the lability of phosphorus in a clayey subtropical soil under different phosphate fertilizers?

Plants have developed different mechanisms to absorb and solubilize phosphorus (P) in the soil, especially in environments with low P availability. This study evaluated the effects of different winter cover crops on soil P availability in a clayey subtropical (Hapludox) soil receiving soluble P fertilizer and a rock phosphate applied to the summer crop, under no‐tillage. The experiment was carried out over 3 yrs (2009–2011) with five different cover crop species: common vetch, fodder radish, ryegrass, black oat, white clover and fallow as control. The soil was sampled after the third year of cover crop cultivation and analysed for inorganic and organic P forms according to the well‐established Hedley fractionation procedure. Phosphate fertilizers promoted accumulation of both labile and nonlabile P pools in soil in the near surface layer, especially under rock phosphate. Fertilizer applications were not able to change P fractions in deeper layers, emphasizing that the Brazilian clayey soils are a sink of P from fertilizer and its mobility is almost nil. Although the cover crops recycled a great amount of P in tissue, in a short‐term evaluation (3 yrs) they only changed the content of moderately labile P in soil, indicating that long‐term studies are needed for more conclusive results.     

超微活化条件对磷矿粉磷素形态及肥效的影响

采用化学分析、红外光谱分析以及盆栽试验研究了活化剂添加量及研磨时间对超微活化磷矿粉磷素形态及生物有效性的影响.结果表明,与普通磷矿粉相比,磷矿粉经超微活化处理后有效磷提高了45.1％～58.7％,活性磷提高了169.4％～203.6％,水溶性磷含量随活化剂添加量的增加也明显提高;当活化剂添加量达到5％时,3次水溶性磷的累积释放量较相同条件下制得的超微细磷矿粉提高84倍以上.适当延长研磨时间有利于磷矿粉磷素的释放,但效果不显著.红外光谱分析结果表明:超微细活化磷矿粉中与PO3-、HPO2-相关的特征吸收峰强度较普通磷矿粉显著增强,且生成了与PO43-、HPO42-相关的新特征吸收峰,使磷矿粉中的磷向有效状态转变.盆栽试验结果进一步表明,超微活化磷矿粉处理的玉米生物量、磷素利用率均显著高于磷矿粉、普通超微细磷矿粉以及过磷酸钙和磷酸二铵等常规水溶性磷肥,可增强抗固定能力而显著提高土壤有效磷含量.超微活化磷矿粉较高的活性磷总量和水溶性磷持续适度的供磷强度是其生物有效性高的原因.     

垃圾堆肥对难溶性磷转化及土壤磷素吸附特性影响

在城市生活垃圾进行工厂化堆肥过程中，加入难溶性磷矿粉，探讨堆肥对难溶性磷的转化能力及堆肥产品培肥后对土壤磷素吸附特性的影响。结果表明，加入磷矿粉可使堆肥中活性有机磷、中等活性有机磷、中稳性有机磷、高稳性有机磷及速效磷含量均有不同程度的提高，与对照相比分别增加212.69%、80.36%、61.21%、62.74%、157.89%。通过电镜观察表明，堆肥后磷矿粉典型的矿物特征消失，表面呈蜂窝状。将堆肥后的产品进行培肥试验表明，富磷垃圾肥处理可明显改善土壤磷素的吸附特性，与施化肥相比，最大吸附量(Q_m)下降8.76%，最大缓冲容量(Q_m·K)下降13.58%，而磷素的吸附饱和度(DPS)、零净吸附浓度磷(EPC₀)则呈不同程度的增加，幅度依次为98.52%、7.13%。试验结果显示，通过堆肥生产富磷垃圾肥可为解决中国磷素资源缺乏、化学磷肥利用率低等问题提供一条生物学途径。     

Phosphorus Sources and Rates Associated with Nitrogen Fertilization in Mombasa Grass Yield

Nitrogen (N) and phosphorus (P) deficiency is one of the important causes of degradation of cultivated pasture under tropical conditions. The aim of this study was to evaluate phosphate rates and sources, and N rates on the concentration and uptake of N and P, and shoot dry mass (SDM) yield of Megathyrsus maximum grass cv Mombasa in an Ultisol. The trial was carried out in a greenhouse in pots with 4.0 dm^?3 of soil. The experiment was arranged in a completely randomized design with four replicates. The 3 × 3 × 3 factorial treatments consisted of phosphorus sources [reactive rock phosphate from Morocco (RPM), reactive rock phosphate from Algeria (RPA) and triple superphosphate (TSP)], three phosphorus rates (0, 150, and 300 mg kg^?1), and three N rates (0, 250, and 500 mg kg^?1). The SDM and tillering of Mombasa grass were significantly influenced with the TSP, RPM, and RPA application associated with N fertilization. The RPM, RPA, and TSP met the nutritional demands of Mombasa grass. The three P sources showed the same effect on the total N uptake by Mombasa grass. The P use efficiency (PUE) when fertilizer-P sources were added alone by Mombasa grass was <12% of the added P, and PUE decreased as follows: TSP > RPA > RPM. When P and N-fertilizer were added together, the fertilizer-N use efficiency (NUE) was 62%. The reactive phosphate (RPM and RPA) is an efficient P sources for Mombasa grass, but requiring higher rate of application compared to TSP source.     

Physico‐chemical characterization of humic‐metal‐phosphate complexes and their potential application to the manufacture of new types of phosphate‐based fertilizers

The aim of this review is to describe the main physicochemical characteristics of diverse types of humic‐metal‐phosphate acid complexes. The effects of these complexes on phosphorus (P) fixation in soils with different pH values and physicochemical features and on plant phosphorus uptake are also discussed. Humic‐metal‐phosphate complexes have apparent stability constants in the same range as those of metal‐humic complexes, in solutions with diverse pH and ionic‐strength values. Likewise, the molecular‐size distribution of humic‐metal‐phosphate complexes as a function of pH is similar to that of potassium or sodium humates and metal‐humic complexes. Humic‐metal‐phosphate complexes are able to decrease phosphate fixation in soils and increase plant growth and phosphate uptake. Phosphorus fertilizers containing humic‐metal‐phosphate complexes proved to be efficient to improve plant growth and P uptake with respect to conventional fertilizers such as single superphosphate. The values of parameters related to plant phosphorus‐utilization efficiency (PUt E) suggest that the regulation of root acquisition of phosphate from these complexes could involve the interregulation of a system for the optimization of metabolic P utilization in the shoot and another system involving stress responses of roots under phosphorus deficiency.     

一株红壤花生根际溶磷真菌的分离、鉴定及溶磷能力的研究

为提高磷素利用率,从花生根际土壤样品中筛选到一株溶磷能力强的菌株B1-A,结合菌落形态特征和ITS rDNA序列分析将其鉴定为黑曲霉(Aspergillus niger)。菌株B1-A的不同接种量(1%,3%,5%)在两种难溶性磷酸盐(FePO4,AlPO4)培养液的溶磷量和pH随时间动态变化表明溶磷量均与pH呈显著负相关,B1-A的溶磷量与接种量、培养时间、磷矿粉浓度有关,实验结果表明菌株B1-A在接种量为3%～5%、培养时间168 h、云南磷矿粉浓度为3 g L-1、江西磷矿粉浓度为5 g L-1时溶磷效果较好。菌株B1-A对磷酸三钙、磷酸铝、磷酸铁、磷矿粉有较强的溶解能力,最高溶磷量分别为418.7、942.3、242.2、177.4 mg L-1,有望为开发高效红壤微生物磷肥提供种质资源。     

Phosphorus Solubilization from Low-Grade Rock Phosphates in the Presence of Decomposing Soybean Leaf Litter

Abstract

The natural phenomenon of defoliation of mature soybean leaves onto the soil surface provides a large quantity of easily decomposable organic matter in the form of leaf litter. The potential of decomposing soybean leaf litter (SLL) to solubilize phosphorus (P) from two low‐grade rock phosphates, Jhabua rock phosphate (JRP) and Hirapur rock phosphate (HRP), alone or amended with pyrite, was assessed in an incubation study. Decomposing SLL solubilized P both from JRP and HRP and concurrently increased water‐soluble as well as organic P contents. Amending rock phosphates with pyrite (in a 1∶2 P to S ratio) promoted P solubilization. Approximately 71 to 92% of the total solubilized P was converted to organic P. The rate of P solubilization increased with SLL decomposition time, reaching its peak at 60 days with rock phosphates alone and at 90 days with pyrite‐blended rock phosphates. The maximum P solubilization (as a percentage of total P added) with different rock phosphates and their mixtures with pyrite followed this order: HRP (11.4%)<HRP+pyrite (16.5%)<JRP (20.2%)<JRP+pyrite (26.5%). These findings clearly suggest that the decomposing SLL has the potential to solubilize P from the otherwise insoluble low‐grade rock phosphates and can offer a natural opportunity for direct use of rock phosphates in the cropping systems that have soybean as a component crop.     

一株土生克雷伯氏杆菌(k.pneumoniae)溶磷能力的初步研究

本文采用固、液体无机磷培养基研究了一株从土壤中分离得到的土生克雷伯氏杆菌102菌株,在室内纯培养条件下的溶磷能力。平板透明圈试验结果表明:菌落与菌落+透明圈直径之比为2.4~4.0;液体纯培养条件下,在无可溶性磷存在时其溶解磷矿粉的量高达72.83mg P L-1,在含有10mg P L-1、20mg P L-1磷酸二氢钾时102菌溶解磷矿粉的量分别为61.92、66.36mg P L-1;高效液相色谱测定102菌发酵液中主要含有乙酸、乳酸等有机酸。     

Introduction of composted rock phosphate and poultry manure enhances winter wheat phosphorus use efficiency,grain yield and soil quality

This field study evaluates the integrated impact of poultry manure (PM), rock phosphate (RP), composted rock phosphate (CRP) and single super phosphate (SSP) on the growth, yield, and phosphorus use efficiency (PUE) of winter wheat and their effect on postharvest soil characteristics. The seven treatments were as follows: T₁ = control; T₂ = SSP full; T₃ = PM full; T₄ = RP full; T₅ = CRP full; T₆ = 50% SSP + 50% CRP (50:50); T₇ = 50% PM + 50% CRP (50:50) at a recommended P rate of 90 kg ha^?1. The combined treatment with PM + CRP produced the highest straw yield of 3582 kg ha^?1, grain yield of 2226 kg ha^?1, P uptake of 21.3 kg ha^?1, and PUE of 18%. The postharvest soil organic carbon, total nitrogen and soil available phosphorus were sig-nificantly higher in integrated treatments.