氟啶胺对土壤中蔗糖酶活性及呼吸作用的影响

使用农药控制作物害虫和疾病可提高农业生产力, 然而农药的使用对土壤造成的污染已成为巨大且日益严重的问题。重复、广泛使用的农药进入土壤影响土壤生物、生物代谢及其生物活性, 已成为农业生态环境重要的研究内容。为了更好地了解氟啶胺对土壤微生物活性和土壤质量等潜在环境危险, 采用实验室模拟的方法研究了氟啶胺农药残留动态, 以及氟啶胺对土壤呼吸强度、蔗糖酶活性及其动力学和热力学特征参数的影响。结果表明: 高剂量(100 mg·kg^-1)氟啶胺在土壤的降解速率常数最大, 氟啶胺在土壤中的半衰期范围为0.38~0.59 d。高剂量(50 mg·kg^-1、100 mg·kg^-1 和1 000 mg·kg^-1)氟啶胺对土壤蔗糖酶表现出不同程度的抑制作用; 低剂量(1 mg·kg^-1、5 mg·kg^-1)处理表现为抑制-激活-抑制作用, 且波动范围较大; 10 mg·kg^-1 氟啶胺对土壤蔗糖酶前期表现为抑制、后期表现为激活作用, 波动范围较大。不同浓度氟啶胺胁迫下蔗糖酶促反应的Michaelis 常数(K_m)和最大反应速率(V_max)发生改变, 但变化不大。土壤中氟啶胺浓度为1 mg·kg^-1 时蔗糖酶所需的活化能(E_a)比CK 高, 其他浓度都低于CK; 5 mg·kg^-1、10 mg·kg^-1、50 mg·kg^-1、100 mg·kg^-1 和1 000 mg·kg^-1 所需的活化焓变(ΔH)随氟啶胺的浓度降低而变小; 在相同温度下蔗糖酶的活化熵变(ΔS)表现为: 1 mg·kg^-1G)变化差异较小; 320~330 K (开氏温度)时最大速度常数(Q₁₀)最大, 而290~300 K 时Q₁₀ 较小。低剂量氟啶胺对土壤微生物呼吸作用的影响表现为随时间变化呈现抑制-激活趋势, 高低剂量表现为抑制作用。土壤微生物的呼吸活性因氟啶胺的加入而产生波动。本研究结果有助于进一步分析研究受农药污染土壤的质量和酶活之间的相关性。     

Veterinary antibiotics at environmentally relevant concentrations inhibit soil iron reduction and nitrification

Veterinary antibiotics used in food animal production, subsequently entering the agroecosystem through land application of animal manure, constitute a growing concern. Previous studies have reported inhibitory effects of antibiotics on soil microbial activities, however, treatment concentrations in these studies were often many times greater than the ranges typically found in the environment. When spiked into manure and mixed with soil at environmentally relevant concentrations in a laboratory study, sulfadimethoxine and monensin blocked soil iron reduction over periods extending from a few days to the entire 50-Day experiment. Sulfadimethoxine also had an inhibitory effect on soil nitrification periodically over the course of the study. Respiration and community-level physiological profile parameters were not inhibited by sulfadimethoxine, monensin, or chlortetracycline. We conclude that antibiotics at environmentally relevant concentrations can disrupt soil microbial processes, although the detection of such impact may be antibiotic and/or process specific.     

The extent of drying influences the flush of respiration after rewetting in non-saline and saline soils

Drying and rewetting are common events in soils during summer, particularly in Mediterranean climate where soil microbes may be further challenged by salinity. Previous studies in non-saline soils have shown that rewetting induces a flush of soil respiration, but little is known about how the extent of drying affects the size of the respiration flush or how drying and rewetting affects soil respiration in saline soils. Five sandy loam soils, ranging in electrical conductivity of the saturated soil extract (ECe) from 2 to 48 dS m⁻¹ (EC2, EC9, EC19, EC33 and EC48), were kept at soil water content optimal for respiration or dried for 1, 2, 3, 4 or 5 days (referred to 1D, 2D, 3D, 4D and 5D) and maintained at the achieved water content for 4 days. Then the soils were rewet to optimal water content and incubated moist for 5 days. Water potential decreased with increasing drying time; in the 5D treatment, the water potential ranged between −15 and −30 MPa, with the lowest potentials in soil EC33. In moist and dry conditions, respiration rates per unit soil organic C (SOC) were highest in soil EC19. Respiration rates decreased with increasing time of drying; when expressed relative to constantly moist soil, the decline was similar in all soils. Rewetting of soils only induced a flush of respiration compared to constantly moist soil when the soils were dried for 3 or more days. The flush in respiration was greatest in 5D and smallest in 3D, and greater in EC2 than in the saline soils. Cumulative respiration per unit SOC was highest in soil EC19 and lowest in soil EC2 Cumulative respiration decreased with increasing time of drying, but in a given soil, the relationship between water potential during the dry phase and cumulative respiration at the end of the experiment was weaker than that between respiration rate during drying and water potential. In conclusion, rewetting induced a flush in respiration only if the water potential of the soils was previously decreased at least 3-fold compared to the constantly moist soil. Hence, only marked increases in water potential induce a flush in respiration upon rewetting. The smaller flush in respiration upon rewetting of saline soils suggests that these soils may be less prone to lose C when exposed to drying and rewetting compared to non-saline soils.     

Contribution of crop residue carbon to soil respiration at a northern Prairie site using stable isotope flux measurements

Heterotrophic respiration from agricultural soils can be differentiated as originating from microbial decomposition of recent litter inputs or crop residue carbon (CRC) and resident soil organic carbon (SOC) pools of varying age and stages of decomposition. Our objective was to determine the relative contributions of these pools to respiration in a northern agroecosystem where the non-growing season is long. A tunable diode laser trace gas analyzer was used to determine atmospheric stable C isotope ratio (δ¹³C) values and ¹²CO₂ and ¹³CO₂ fluxes over an agricultural field in the Red River Valley of southern Manitoba, Canada. Measurement campaigns were conducted in the fall of 2006 and spring of 2007 following harvest of a maize (C₄) crop from soil having SOC derived from previous C₃ crops. Stable CO₂ isotopologue gradients were measured from the center of four 200 × 200 m experimental plots, and fluxes were calculated using the aerodynamic flux gradient method. The soil in two of the experimental plots underwent intensive tillage, while the other two plots were managed using a form of reduced tillage. Approximately 70% and 20-30% of the total respiration flux originated from the maize C₄-CRC during the fall of 2006 and spring of 2007, respectively. At least 25% of the maize residue was lost to respiration during this non-growing period. No difference in the partitioning of heterotrophic respiration into that derived from CRC and SOC was detected between the intensive tillage and recently established reduced tillage treatments at the site.     

月季切花开花和衰老进程中乙烯变化类型初探

以１４个生产用月季切花品种为试材，测定了开花和衰老过程中花朵的乙烯生成量和呼吸强度变化动态。结果表明：（１）乙烯生成量在萨蔓莎、天使、默西德斯、加布里拉和雅典娜５个品种表现为蕾期较低，随外层花瓣展开逐渐增大，在盛开期达到高峰，然后降低，变化动态类似于跃变型切花和跃变型果实；唐娜小姐品种在整个开花和衰老进程中一直保持在较低水平，类似于非跃变型切花和果实的变化动态；坦尼克、黄金时代、金徽章、金牌、红衣主教、红成功、玛丽娜等品种在蕾期较低，随着开花进程逐渐增大，至盛花后期花朵露心时仍在增加，类似于末期上升型果实的变化特点。（２）上述３个类型月季品种的呼吸强度在瓶插期间的变化趋势一致，即花蕾期相对较低，花朵充分展开前迅速升高并出现高峰，然后降低，呈现典型的呼吸跃变类型，同时，萨蔓莎和天使呼吸跃变高峰的出现都比类似乙烯跃变高峰的出现提前１～２天。说明月季切花乙烯生成量与呼吸强度的变化动态有很大不同     

The effect of sucrose on the flower bud opening of ‘Madelon’ cut roses

Complete flower bud opening is characterised by an increase in the petal area, and by enhanced dry and fresh weights of the petals. The import of dry matter into the petals is used for osmotic, biosynthetic and respiratory demands. However, flowers of ‘Madelon’ cut roses frequently fail to open completely under postharvest conditions. An aqueous solution containing 45 mM sucrose induces proper flower bud opening, even when the cut roses have been exposed initially to a sucrose-free solution for 48 h. This points to a requirement for a supply of organic matter from source tissue to the flower as main sink. This conclusion is confirmed by the observation that complete flower bud opening can also be achieved without any addition of sucrose by a reduction in the number of participating petals. Replacing two-thirds part of the 45 mM sucrose by an isomolalic amount of KNO₃ does not affect the flower opening process, implying that a considerable amount of the added sucrose is claimed for osmoregulation. The role of added sucrose and the contribution of the endogenous storage pool in the process of flower bud opening is discussed.     

PEG预处理提高玉米种子活力和萌发代谢的效应

本文研究了ＰＥＧ预处理对玉米种子活力及萌发代谢性酶活力的影响。结果表明，ＰＥＧ处理可以提高玉米种子活力及幼苗抗高温的能力，增强萌发玉米种子的呼吸作用，明显提高萌发期间淀粉酶、脂肪酶、转氨酶的活力。     

铝胁迫下大豆根系分泌物对根际土壤的影响

以2个大豆品种（浙春2号和浙春3号）为材料，设置了4个铝浓度，分别在铝处理7d和14d时，测定大豆根系分泌物中的氨基酸、有机酸及可溶性糖，同时对大豆根际土壤的pH值、土壤酶和土壤呼吸速率进行分析。实验结果显示，虽然根系分泌物对根际土壤具有一定的酸化作用，但是随着铝浓度的升高，根系分泌物有使根际土壤酸碱度趋向平衡的效应。低铝浓度下，大豆根系分泌较多的可溶性糖和氨基酸，促使根际土壤酶活性的增强和土壤呼吸速率的提高，同时还可分泌较多的柠檬酸，与大豆的耐铝性相关。高铝浓度抑制主要根系分泌物的分泌，降低土壤酶活性和土壤呼吸速率；但高铝胁迫增加可溶性糖分泌量。实验结果表明，浙春2号大豆比浙春3号大豆耐铝；随着铝处理时间的延长，铝毒害作用明显。     

What artificial urine composition is adequate for simulating soil N2O fluxes and mineral N dynamics?

Artificial urine, an aqueous solution of various nitrogenous compounds and salts, is routinely used in soil incubation studies on nitrous oxide (N₂O) emissions and related nitrogen (N) and pH dynamics. There is, however, no consensus on artificial urine composition, and a wide variety of compositions are used. The aim of this study was to test which artificial urine composition is adequate for simulating N₂O fluxes, respiration, soil mineral N and pH dynamics of real cattle urine in both short- and long-term incubation studies. Urine solutions of differing compositions were applied to a sandy soil and incubated for 65 days, and results of measurements on N₂O fluxes and soil mineral N were analyzed over the first 5 days as well as over the whole incubation period. Results from two real cattle urines with known nitrogenous composition (R1 and R2) were compared with three artificial urine types: (i) urea+glycine (AG), (ii) urea+hippuric acid (AH) and (iii) an artificial urine identical to the nitrogenous composition of real urine R1 (AR). During the first 5 days, only cumulative N₂O emissions for AG deviated significantly (P=0.02) from the N₂O emissions for real urines, with 0.4% of applied N emitted compared with 0.0% and 0.1% for R1 and R2, respectively. Respiration from R1 was significantly (P<0.001) higher than from R2 and all artificial urines. Over the whole incubation period, no significant differences could be detected for N₂O emissions or respiration with urine type. From all artificial urine types, AH yielded N₂O emissions closest to those from real urine. AG deviated most from real urine, both in short- and long-term incubations. Over the whole period, soil NH₄⁺ was higher for all artificial urines (P<0.001) and pH-KCl was lower for AG and AR (P=0.004) than for the real urines. AH was not significantly different from real urine R2 with respect to all measured properties except soil NH₄⁺. We conclude that only AG did not adequately simulate N₂O emissions, and that glycine is therefore not an appropriate substitution for hippuric acid in artificial urine. For future studies using artificial urine we recommend therefore a mixture containing at least urea and hippuric acid as sources of N. As no artificial urine composition resembled real urine with respect to all measured variables, even when nitrogenous composition was identical (AR), we recommend the use of real urines whenever possible.     

花生光合生产与干物质积累的动态模拟

在综合前人研究成果的基础上,兼顾模型的机理性与实用性平衡,构建了花生光合生产与干物质积累的模拟模型。模型采用高斯积分法有效地计算了冠层每日的总光合量,且充分考虑了环境因子中温度和CO2对光合作用的影响。利用试验资料对模型核实的结果显示,模型可以较好地预测不同生长条件下的生物量积累动态,具有较强的机理性和实用性。