Zinc transformations in acidic soil and zinc efficiency on maize by adding six organic zinc complexes

Experiments under laboratory and greenhouse conditions were conducted to study the response of maize (Zea mays L.) to Zn fertilizer applications (Zn-phenolate, Zn-EDDHA, Zn-EDTA, Zn-lignosulfonate, Zn-polyflavonoid, and Zn-heptagluconate) in an Aquic Haploxeralf soil. The application of Zn complexes significantly increased Zn uptake by the plant compared with that in the control soil. The highest enhancements were obtained in soil treated with Zn-EDTA, Zn-lignosulfonate, and Zn-EDDHA. The highest percentages of Zn taken up by the plants occurred when 20 mg x kg(-1) Zn was applied as Zn-EDTA fertilizer and 10 mg x kg(-1) as Zn-lignosulfonate fertilizer. In the greenhouse experiment, Zn speciation in soil after harvesting showed that almost all Zn was found in the residual fraction followed by metal in the water-soluble plus exchangeable fraction and metal bound to organic matter. The most effective fertilizers maintaining Zn in the most labile fractions were Zn-phenolate, Zn-EDTA, and Zn-lignosulfonate. Conversely, in the incubation experiment, only a small percentage of Zn was found in the water-soluble plus exchangeable fraction and no differences in the Zn distribution were observed between the different fertilizer treatments. The micronutrient content in maize was positively correlated with the water-soluble plus exchangeable Zn as well as with the available Zn determined by the diethylenetriaminepentaacetic acid and Mehlich-3 methods, in the greenhouse experiment. Results of this study showed that the incubation experiment in acidic soil is not a suitable tool to establish the different effectiveness of Zn chelates in plants.     

Effects of zinc complexes on the distribution of zinc in calcareous soil and zinc uptake by maize

The movement and availability of Zn from six organic Zn sources in a Typic Xerorthent (calcareous) soil were compared by incubation, column assay, and in a greenhouse study with maize (Zea mays L.). Zinc soil behavior was studied by sequential, diethylenetriaminepentaacetate, and Mehlich-3 extractions. In the incubation experiment, the differences in Zn concentration observed in the water soluble plus exchangeable fraction strongly correlated with Zn uptake by plants in the greenhouse experiment. Zinc applied to the surface of soil columns scarcely moved into deeper layers except for Zn-ethylenediaminetetraacetate (EDTA) that showed the greatest distribution of labile Zn throughout the soil and the highest proportion of leaching of the applied Zn. In the upper part of the column, changes in the chemical forms of all treatments occurred and an increase in organically complexed and amorphous Fe oxide-bound fractions was detected. However, the water soluble plus exchangeable fraction was not detected. The same results were obtained at the end of the greenhouse experiment. Significant increases were found in plant dry matter yield and Zn concentration as compared with the control treatment without Zn addition. Increasing Zn rate in the soil increased dry matter yield in all cases but Zn concentration in the plant increased only with Zn-EDTA and Zn-ethylenediaminedi-o-hydroxyphenyl-acetate (EDDHA) fertilizers. Higher Zn concentration in plants (50.9 mg kg(-)(1)) occurred when 20 mg Zn kg(-)(1) was added to the soil as Zn-EDTA. The relative effectiveness of the different Zn carriers in increasing Zn uptake was in the order: Zn-EDTA > Zn-EDDHA > Zn-heptagluconate >/= Zn-phenolate approximately Zn-polyflavonoid approximately Zn-lignosulfonate.     

Zinc transformations in neutral soil and zinc efficiency in maize fertilization

The effect of six Zn sources (Zn-phenolate, Zn-EDDHA, Zn-EDTA, Zn-lignosulfonate, Zn-polyflavonoid, and Zn-glucoheptonate) was studied by applying different Zn levels to a representative Calcic Haploxeralf neutral soil (the predominant clay is montmorillonite) in incubation and greenhouse experiments. Zinc soil behavior was evaluated by sequential DTPA and Mehlich-3 extraction procedures. In the incubation experiment, the highest percentage recovery values of Zn applied to soil occurred in the water-soluble plus exchangeable fraction (29%) in fertilization with 20 mg of Zn kg(-1) of Zn-EDTA fertilizer. In the greenhouse experiment with maize (Zea mays L.), a comparison of different Zn carriers showed that the application of six fertilizers did not significantly increase the plant dry matter yield among fertilizer treatments. The highest yield occurred when 20 mg of Zn kg(-1) was applied as Zn-EDDHA fertilizer (79.4 g per pot). The relative effectiveness of the Zn sources in increasing Zn concentration in plants was in the following order: Zn-EDTA (20 mg kg(-1)) > Zn-EDDHA (20 mg kg(-1)) approximately Zn-EDTA (10 mg kg(-1)) > Zn-EDDHA (10 mg kg(-1)) approximately Zn-phenolate (both rates) approximately Zn-polyflavonoid (both rates) approximately Zn-lignosulfonate (both rates) approximately Zn-glucoheptonate (both rates) > untreated Zn. The highest amounts of Zn taken up by the plants occurred when Zn was applied as Zn-EDTA fertilizer (20 mg kg(-1), 7.44 mg of Zn per pot; 10 mg kg(-1) Zn rate, 3.93 mg of Zn per pot) and when Zn was applied as Zn-EDDHA fertilizer (20 mg kg(-1) Zn rate, 4.66 mg Zn per pot). After the maize crop was harvested, sufficient quantities of available Zn remained in the soil (DTPA- or Mehlich-3-extractable Zn) for another harvest.     

除草剂对土壤温室气体排放的影响

试验设对照、尿素、尿素＋草甘膦和尿素＋丁草胺4个处理,尿素氮用量为200mg·kg-1干土,除草剂用量为10mg有效成分·kg-1干土。在实验室恒温培养条件下,研究除草剂对菜田土壤温室气体排放的影响。结果表明,菜田土壤中施用氮肥显著增加了温室气体N2O、CO2和CH4的排放。尿素氮肥中添加草甘膦显著抑制N2O、CO2的排放,分别比尿素处理降低48.4%和20.2%;添加丁草胺显著抑制N2O排放,比尿素处理降低23.2%,对CO2排放略有减少但不显著;草甘膦和丁草胺对CH4排放都无明显影响。这说明除草剂对土壤温室气体的排放具有显著影响,但不同除草剂品种的效应也存在明显差异。因此,在农田温室气体排放估算时应考虑除草剂的施用对温室气体减排所产生的效果。     

长期施肥对潮土耕层土壤和作物籽粒微量元素动态的影响

Micronutrient status in soils can be affected by long-term fertilization and intensive cropping.A 19-year experiment (1990-2008) was carried out to investigate the influence of different fertilization regimes on micronutrients in an Aquic Inceptisol and maize and wheat grains in Zhengzhou,China.The results showed that soil total Cu and Zn markedly declined after 19 years with application of N fertilizer alone.Soil total Fe and Mn were significantly increased mainly due to atmospheric deposition.Applications...     

Effect of liming and applied phosphorus on growth and P uptake of maize (Zea mays subsp.) plant grown in acid soils of West Wollega,Ethiopia

The study aimed at investigating effects of lime and mineral P fertilizers on P uptake and growth of maize (Zea mays subsp.) in greenhouse pot experiment. Combination of four P rates and four lime rates were applied to four highly acidic soil samples and the soils were incubated for a total of 112?days after which maize (Zea mays subsp.) was planted. The maize plants were harvested for analysis after 42?days of growth. Control experiments were also included. Available P (Bray I) and pH were significantly increased after incubation. Maximum available P was obtained in the soils that received the highest P rate and optimum lime rate. Levels of exchangeable acidity were significantly decreased in the P and lime treated soils compared to the control experiments. Plant biomasses and P uptake of maize increased significantly (p?≤?0.001) with application of P and lime compared to the control experiments.     

Measuring the CO2 production from maize‐straw‐amended soil columns— a comparison of four methods

A soil‐column experiment with maize‐straw application at different depths was carried out to investigate the accuracy of CO₂‐measurement systems in a greenhouse experiment with sandy and loamy soils. The classical approach of CO₂ absorption in NaOH solution was compared with three other methods using dynamic chambers. These methods were gas chromatography (GC), a portable infrared analyzer (IR), and a portable photo‐acoustic system (PAS). The cumulative CO₂ production over the 57‐day incubation period was significantly affected by the method and soil‐specifically by the treatments. The NaOH and GC method always formed a pair of lowest cumulative CO₂ production in all treatments with maize‐straw addition. In the treatments with bottom application of the maize straw, IR and PAS methods gave values at identical levels in both soils. In the treatments with top application of the maize straw, the IR method gave significantly highest values in the sandy soil and the PAS method in the loamy soil. The correlation coefficients between the cumulative CO₂ production of the three dynamic‐chamber methods (GC, IR, and PAS) and the static NaOH method were all significant, with r values between 0.90 and 0.93. The C balance can be used for testing the plausibility of CO₂‐production data. Roughly 102% (NaOH and GC) and 114% (IR and PAS) were recovered, including the CO₂‐production data in the C balance of the sandy soil. The respective data were 97% (NaOH and GC) and 104% (IR and PAS) for the loamy soil.     

设施菜田土壤pH和初始C/NO3– 对反硝化产物比的影响

【目的】设施菜田土壤反硝化作用是N₂O排放和氮素损失的重要途径。本研究通过室内厌氧培养试验,在不同pH和初始C/NO₃–条件下,比较设施菜田土壤反硝化氮素气体排放及产物比的变化特征。【方法】以设施菜田土壤为研究对象,通过添加一定量低浓度的酸碱溶液调节土壤pH分别为酸性、中性和碱性条件,调节后的实测pH分别为5.63、6.65和7.83;同时以谷氨酸钠作为有效性碳,除未添加有效性碳作为对照处理 (CK) 外,其他有效性碳与硝酸盐 (C/NO₃–) 的比值分别调节为5∶1、15∶1和30∶1,三种pH条件下均设置 4 个 C/NO₃– 水平,每个水平3次重复。利用自动连续在线培养系统 (Robot系统),在厌氧条件下监测不同处理土壤产生的 N₂O、NO、N₂和CO₂浓度的动态变化,通过计算N₂O/(N₂O + NO + N₂)指数估算反硝化过程N₂O的产物比。【结果】增加土壤的pH能显著减少设施菜田土壤N₂O和NO的产生量,酸性 (pH 5.63) 土壤的N₂O、NO产生量峰值在不同初始C/NO₃– 比下均显著高于中性 (pH 6.65) 和碱性 (pH 7.83) 土壤 (P < 0.05)。中性和碱性土壤在高C/NO₃– 下有利于减少反硝化过程N₂O的产生,而酸性土壤条件下差异并不显著。中性土壤条件下增加有机碳含量会降低NO产生量,而在酸性和碱性土壤上有机碳的添加对NO产生量没有显著影响。土壤pH和初始C/NO₃– 比对土壤N₂O的产生有极显著的交互效应 (P < 0.001)。酸性和中性土壤上添加有机碳能够显著增加土壤N₂的产生速率 (P < 0.05),且与对照相比,不同pH的土壤添加有机碳后均显著促进反硝化过程中N₂O向N₂的转化。在不同初始C/NO₃– 下碱性土壤的CO₂产生量显著高于酸性和中性土壤,同时与对照相比,添加有机碳显著增加了土壤的CO₂产生量 (P < 0.05)。酸性土壤的N₂O产物比在不同初始C/NO₃– 下均极显著高于碱性土壤 (P < 0.01),且不同初始C/NO₃– 下的土壤N₂O产物比随pH的增加显著下降,二者呈极显著线性负相关关系 (P < 0.01)。【结论】土壤pH降低是设施菜田土壤N₂O和NO排放量较高的重要原因。而且,增加初始土壤有效碳含量促进了土壤的反硝化损失,并在中性和碱性土壤中N₂O的产生量减少。土壤pH升高和初始C/NO₃– 增加均降低了产物比,但增加了土壤反硝化作用速率。在利用N₂O排放通量和产物比估算土壤反硝化氮素损失时,土壤pH和有效碳含量是必须考虑的两个重要因素。     

Sugarcane Bagasse Biochar: Preparation,Characterization, and Its Effects on Soil Properties and Zinc Sorption-desorption

ABSTRACT

Application of alkaline biochar has been proposed as an alternative to lime for remediation of acidic soils. However, questions remain as to how the reactions and fate of metals in acidic soils can be affected by biochar amendment. To find out how biochar addition might affect sorption-desorption behavior of zinc (Zn) in acidic soils, a soil with an initial pH value of 4.67 was treated with different levels [0 (control), 1%, 3%, and 6%] of biochar produced from pyrolysis of sugarcane bagasse at 600°C and incubated for 30 days under 80% of water holding capacity. At the end of the incubation period, important soil chemical properties were measured and batch isotherm experiments were performed to determine soil Zn sorption-desorption parameters. The results showed that the biochar-amended soils had higher pH values (up to 2.5 pH units), electrical conductivity (up to 2.66 times), and cation exchange capacities (up to 42%) relative to the un-amended acidic soil. Biochar addition also led to significant enhancements in soil exchangeable calcium, magnesium, sodium, and potassium cations. Both sorption and desorption isotherm experiments revealed the significantly higher capacity of the biochar-amended soils to retain Zn than that of the control. Moreover, the biochar-amended soils exhibited a higher affinity for Zn sorption than did the un-amended acidic one. It can be concluded that biochar derived from sugarcane bagasse could serve as a good amendment material to reclaim acidic soils and to reduce Zn mobility and toxicity in acidic metal-contaminated soils.     

Mobility of heavy metals in polluted soils near zinc smelters

The distribution and the availability of Cd, Zn, Cu, and Pb along the entire profile of two highly polluted soils located near Zn smelters have been related to the chemical and mineralogical composition of the soil. Lead and Cu deposits always remain in the surface layers and their availability measured by neutral ammonium acetate extraction was very weak. The behavior of Cd and Zn appears different in sandy acidic podzolic soils and in neutral loamy soils. These metals are associated with the organic matter migration in podzolic soils, while they remain in the upper layers in loamy soils provided that the pH is higher than 6. When the pH drops below 6, the mobility of Cd increases while that of Zn increases only below pH 5. The availability of heavy metals is lower in neutral loamy soils than in sandy acidic soils due to precipitation of carbonates and phosphates. With increasing depth, Cd and Zn are more available if the soil is acid; but, if the soil is neutral and loamy the availability is kept low by adsorption on clays and free oxides. The results of the complex trace metals interactions with the soil components show a higher accumulation capacity for loamy soils than for sandy soils notwithstanding the fact that their CEC is similar.     

Availability of Cu and Zn in an acidic sludge-amended soil as affected by zeolite application and liming

Purpose  

Acidic soils exhibit high trace element availability compared to neutral pH soils, and thus, when trace metals are added (e.g. due to sewage sludge application), measures should be taken to reduce their mobility. In this experiment, we tested two such methods, liming and zeolite addition. The aim was to measure the availability, in ryegrass (Lolium perenne L.), of heavy metals (Cu and Zn) added to soil with sewage sludge in both acidic and limed soil.     

Performance of Slag-Based Gypsum on Maize Yield and Available Soil Nutrients over Commercial Gypsum under Acidic and Neutral Soil

ABSTRACT

Effect of slag-based gypsum (SBG) and commercial gypsum (CG) on maize was investigated in acidic and neutral soils. A randomized complete block design (RCBD) with seven treatments consisting of three levels (150, 450, and 750 kg ha^?1) of SBG and CG with recommended dose of fertilizer (RDF) and one control was maintained. Application of SBG @750 kg ha^?1 recorded significantly higher (8.61 and 8.69 t ha^?1, respectively) cob yield of maize compared to CG and control treatments in both soil condition. Increased levels of SBG application increased soil pH and EC in both the soils, but decreased with the application of CG. Application of 750 kg SBG ha^?1 recorded significantly higher soil available nutrients like phosphorus in acidic soil and potassium in neutral soil. Higher exchangeable calcium and magnesium in acidic soil and exchangeable calcium in neutral soil were recorded with the application of CG @750 kg ha^?1. Available sulfur was significantly higher with CG @750 kg ha^?1 applied treatment in both soils. CaCl₂Si content in acidic soil varied significantly and recorded higher with application of SBG, while CaCl₂Si content in neutral soil and AASi in both soils had no significant effect by application of SBG. Significantly higher DTPA extractable micronutrients in acidic and neutral soil were noticed in SBG @750 kg ha^?1 applied treatment. However, application of SBG had no significant effect on iron and copper content in neutral soil. Higher uptake of nutrients was recorded with 750 kg SBG ha^?1 compared CG applied and other treatments.     

不同土壤水分供应下锌对玉米叶片超微结构的影响

选择 土为供试土壤, 进行盆栽玉米试验, 设定0和5.0 mg·kg^-1两个锌处理, 按土壤饱和持水量的40%~45%和70%~75%在玉米的4叶1心期实施干旱和正常水分处理。生长50 d后, 测定不同土壤水分与锌供应状况下植株生物量和锌含量, 利用透射电子显微镜观察完全伸展新叶的超微结构变化, 以期揭示不同土壤水分供应下, 植物对施锌的响应机理。结果表明: 土壤水分供应充足条件下, 与不施锌相比, 施锌玉米地上部生物量和总干重分别增加78%和52%, 根系和地上部锌含量和锌吸收量增加较多; 而干旱条件下, 施锌对玉米生物量无显著影响。干旱条件下缺锌玉米叶片维管束鞘细胞中叶绿体结构基本保持完好, 淀粉粒和基质片层清晰可见, 但叶肉细胞中叶绿体膜受损, 基质片层结构出现皱缩, 基粒片层减少; 施锌玉米叶片维管束鞘细胞中叶绿体结构保持完好, 叶绿体周围的线粒体数目较多, 叶肉细胞中叶绿体中脂肪颗粒增多, 叶片维管束鞘细胞与叶肉细胞之间可见清晰的胞间连丝。土壤水分充足处理下, 缺锌叶片细胞膜出现皱缩, 维管束鞘细胞叶绿体淀粉粒增多, 片层结构受损, 严重时维管束鞘细胞中内溶物消失, 残存的叶绿体中仅有淀粉粒和少许片层; 叶肉细胞中叶绿体可见淀粉粒, 但片层结构少, 有些出现断裂、收缩。土壤水分充足条件下, 施锌玉米维管束鞘核叶肉细胞结构清晰, 叶绿体结构完整。结论认为: 锌对干旱胁迫下玉米叶片细胞结构的破坏有一定的缓解作用; 但土壤水分正常供应下, 缺锌导致细胞结构受损程度比干旱情况下更严重。     

营养型土壤改良剂对酸性土壤中钾的调节及玉米吸钾量的影响

营养型土壤改良剂(以下简称改良剂)施入三种不同肥力水平的土壤进行恒温培养试验和盆栽试验,测定土壤有效钾的含量、盆栽试验玉米的生物量和钾吸收量。结果表明:对于有效钾含量高的土壤,改良剂能促进钾的缓效化,有利于土壤钾的保蓄,防止土壤钾的淋失;对于有效钾含量较低的土壤,改良剂可以活化土壤中的钾,提高土壤钾的有效性;不同肥力水平的土壤,改良剂都能促进玉米对钾的吸收,有利于提高钾肥的吸收利用效率。     

Profile Characteristics and Potential Environmental Effect of Accumulated Phosphorus in Soils ofVegetable Fields in Beijing

Profile characteristics of accumulated P in 10 representative soils of vegetable fields in suburban districts of Beijing were investigated. Bioavailability of the accumulated P and its potential effect on the environment were studied in a greenhouse pot experiment and a soil column experiment. The results showed that the concentration of Olsen-P in the 0～20 cm soil samples of the vegetable fields ranged from 22.1 to 358.0 mg kg-1, which was 2 to 10 times higher than that of the crop fields in the suburbs of Beijing. Most of the excessive phosphorus was accumulated in the topsoils. The longer the soils cultivated with vegetables, the higher the soil total P, Olsen-P and organic matter concentration. Accumulated P in the soils from vegetable fields had higher bioavailability. Application of phosphorus fertilizer could not increase the dry weights of cucumbers, Chinese cabbage, and rape seedlings continuously planted. The soil column study showed high P concentration (＞ 0.6 mg L-1) in the leachates from the columns of the vegetable field soils with high accumulated P, which has a potential effect on the groundwater and natural water quality.     

施用石灰与钙蒙脱石对酸性土壤硝化动力学过程的影响

土壤酸化是粘土矿物缓慢风化的自然过程,但近年来随着人类高强度的农业利用,土壤酸化现象逐渐加剧,而铵态氮肥的硝化作用是土壤酸化的主要贡献者之一。传统的施用石灰改良酸性土壤,常常会有反酸现象,并可能导致土壤板结。蒙脱石是碱性或中性土壤的主要粘土矿物组分,而在土壤酸化的过程中,蒙脱石被进一步风化掉。本文通过室内模拟实验,采用硝化动力学拟合及对净硝化速率的计算,分别研究了蒙脱石(Ca-M)和石灰(Ca-OH)对酸性黄壤硝化作用的影响。结果表明:酸性黄壤添加石灰或蒙脱石后,土壤均发生了显著的硝化作用,且硝化过程符合一级动力学模型N_(NO3)=N_0+N_p(1-exp(-k_1t))(P0.001)。Ca-OH处理土壤样品的净硝化速率(3.429 mg·kg~(-1)·d~(-1))显著大于Ca-M处理(2.381 mg·kg~(-1)·d~(-1));Ca-OH处理土壤样品的潜在硝化速率(V_p)和平均硝化速率(V_a)在pH值5.7和6.2时分别为6.42、8.58 mg N·kg~(-1)·d~(-1)和2.71、3.87 mg N·kg~(-1)·d~(-1),均显著大于钙基蒙脱石处理(pH值5.7和6.2时分别为3.40、4.56 mg N·kg~(-1)·d~(-1)和2.36、3.04 mg N·kg~(-1)·day~(-1))。结果表明采用石灰改良酸性土壤发生复酸化现象的可能性及程度大于钙基蒙脱石,本研究为酸性土壤改良提供了新的参考。     

Salt tolerance of grain crops in relation to ionic balance ability to absorb microelements

A greenhouse experiment was conducted to investigate the effect of exchangeable Na on the growth and absorption of metal elements in barley, rye, and maize. The plants were cultivated in soils whose exchangeable sodium percentages (ESP) were 6.6 (saline soil: Saline), 17.4 (saline-sodic soil: Sodic 1), and 39.6 (sodic soil: Sodic 2), which were prepared from Tottori sand dune soil (Control). The dry weight (DW) and concentrations of metal elements Ca, Mg, Mn, Zn, and Cu) in shoots were analyzed. The shoot DW was smaller with higher ESP, but in barley the difference between all the treatments was no longer observed with time. In Sodic soils, the growth of barley was vigorous, whereas rye growth was poor, and maize plants died by 5 weeks after planting. The Na concentration in shoots of all the species was higher with higher ESP. The K concentration in shoots was low at the early growth stage, but in barley it was higher in the Saline and both Sodic soils than in the Control at the subsequent stages. The concentrations of Ca and Mg in shoots of barley and maize in the Saline and both Sodic soils were higher than those in the Control, but in rye the concentrations were lowest in Sodic 2. The concentrations of Mn, Zn, and Cu in barley shoots in the Saline and bothSodic soils tended to be higher than those in the Control, whereas in rye they were lower than in the Control in both Sodic soils. Barley showed a higher ability to absorb low available microelements than rye and maize. These results indicate that barley is tolerant to sodicity as well as salinity, maize is tolerant to salinity, but is very sensitive to sodicity, and rye is moderately sensitive to both stresses. We suggest that the tolerance of grain crops to ESP involves a tolerance to a high Na concentration in shoots, the ability to keep suitable concentrations of essential cations in the presence of a high concentration of Na in shoots and the ability to absorb low available microelements.     

粉垄耕作对小麦玉米产量及耕层土壤养分的影响

通过在河南省温县(2013~2014年)和西华县(2014~2015年)小麦、玉米2季作物的试验,研究粉垄耕作对作物产量、土壤养分(碱解氮、有效磷、速效钾、有机质)含量的影响,并分析耕作措施与作物生产、养分吸收的关系,为作物高产和施肥管理提借鉴。小麦播种季,设旋耕(12~16 cm,CK),粉垄耕作(FL1:20~30 cm,FL2:30~40 cm)3个处理,夏玉米在小麦收获后贴茬播种,其它一切农事操作均保持一致。结果表明,FL1、FL2处理小麦当季平均增产幅度分别为18.5%、23.5%,FL2FL1;玉米季,FL1、FL2处理的平均增产幅度分别为10.4%、5.8%。土壤养分方面,与CK相比,FL1、FL2处理能够增加小麦成熟期潮土土壤速效钾含量,平均增加74.49 mg kg~(-1),显著降低土壤碱解氮、有效磷、有机质含量,降低玉米季土壤耕层速效养分含量。FL1、FL2处理显著增加砂姜黑土土壤有效磷含量,平均高2.2 mg kg~(-1),降低土壤碱解氮、速效钾含量,分别平均降低7.54 mg kg~(-1)、13.38 mg kg~(-1)。小麦季,FL1、FL2处理的氮、磷、钾肥偏生产力均显著高于CK,比CK高出5~19个单位;玉米季,偏生产力比CK高出3~15个单位。说明在养分投入、农事操作等保持一致的条件下,粉垄耕作(FL1,FL2)能够增加小麦、玉米两季作物产量,促进作物对养分的吸收,特别是氮的吸收。此外,适当增加耕作层的厚度更有助于当季小麦产量的提高。     

砂质土壤积累的铜和锌的可提取性与移动性研究

An investigation was conducted to study problems of determining a reasonable percentage for ecological water-use in the Haihe River Basin of China. Three key aspects for the ecological water requirement （EWR） were analyzed, involving i） the EWR for river system, ii） the EWR for wetlands and lakes, and iii） the EWR for discharge into the sea to maintain the estuary ecological balance of the Haihe River. The Montana method and related water level-flow relationships, and the statistic approach based on hydrological records were applied to estimate different components of EWR. The results showed that the total ecological water demand in the region, was about 3.47-14.56 billion m^3. Considering flow regime change and uncertainty, the ecological water demand could be estimated by the hydrological frequency approach. Preliminary analysis showed that for different annual runoff under the frequencies of 20%, 50%, 75% and 95%, the ecological water demand approached 12%-50%, 18%-74%, 24%-103%, 35%-148% and 16%-66%, respectively. By further analysis to balance ecological water-use and socioeconomic water-use, the rational percentage of ecological water-use was estimated as 35%-74%, that provides useful information to judge whether the allocation of water resources is reasonable, and was proved to be satisfactory by comparing with the practical condition.     

缓释复合肥对不同土壤红三叶产量和品质效应的研究

采用盆栽试验研究了缓释复合肥对强酸性土、酸性土、中性土上红三叶产量和品质的效应。结果表明,与等养分普通复合肥相比,不同土壤施用缓释复合肥可显著提高红三叶产量,增产率以强酸性土（55.8%）〉中性土（39.9%）〉酸性土（7.4%）;不同缓释复合肥在不同土壤上的肥效有差异,强酸性土和酸性土上施用低磷钾的缓释复合肥产量高,中性土则以施高磷钾缓释复合肥者产量高。缓释复合肥能改善3种土壤第一茬、第二茬红三叶饲用品质和矿质品质,其中粗蛋白提高4.0%-23.1%,粗脂肪提高2.5%-38.6%,粗灰分提高1.4%-23.6%,粗纤维降低2.5%-23.3%,磷提高4.9%-18.6%,钙提高1.8%-13.7%。红三叶异黄酮含量受土壤影响较大,强酸性土和酸性土上缓释复合肥处理的异黄酮含量低于等养分普通复合肥,而中性土施用缓释复合肥提高了红三叶异黄酮含量。