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依托O3FACE(Free-Air O3 Enrichment)研究平台,研究了大气臭氧(O3)浓度增加对拔节期水稻根系呼吸和生物量积累分配的影响,利用特制集气装置分析了厌氧—有氧条件对根系呼吸的影响。结果表明,O3浓度升高水稻冠层和总生物量略有降低,而根干物重和根/冠比分别显著降低14.7%和10.4%。9∶1和9.5∶0.5的纯N2∶O2配比利于根系呼吸,纯N2或空气、CO2饱和蒸馏水条件不同程度降低了根系呼吸速率;高臭氧处理、对照处理的水稻根系呼吸速率分别在CO2饱和蒸馏水、纯N2条件下最小,表明尽管不同根系测定条件影响根系呼吸速率,但影响程度也受植物生长的大气环境制约。臭氧污染处理水稻根系的呼吸速率在气态测定条件下显著高于正常大气处理23.6%~52.7%,在CO2饱和蒸馏水测定条件下未达到显著水平,臭氧污染效应明显降低。两个环境生长的水稻根系呼吸均随测定根系气态环境供氧量的增加呈凸二次函数变化,5%~10%比例的氧气供应促进了根系呼吸,较强的厌氧环境(纯N2)和有氧环境(Air)均不利于水稻根系呼吸。 相似文献
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储藏稻谷品质指标的变化及其差异性 总被引:14,自引:4,他引:10
为了探讨储藏稻谷品质的变化规律及其影响因素,该文对国内不同储藏区域、储藏年限的180个商品稻谷样品的电导率(ECR)、丙二醛含量(MDAC)、脂肪酸值(FAV)、过氧化氢酶(CAT)、过氧化物酶(POD)、多酚氧化酶(PPO)活性等品质指标进行了测定,然后,采用SPSS10.0统计软件对这些测定数据进行差异分析。结果表明:随着稻谷储藏时间的延长和陈化程度的加深,ECR、MDAC、FAV逐渐增大,而CAT、POD、PPO的活性逐渐降低,这些指标在一定程度上反映不同储藏年限间稻谷品质的差异,其中显著影响稻谷新鲜度的指标是FAV、ECR、MDAC和PPO活性,尤以FAV的差异最大;而不同储藏地域的气候条件以及稻谷类型上的差异也将对储藏稻谷品质指标的变化产生显著的影响。 相似文献
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粮食储备是保障国家粮食安全的重要物质基础,谷物中脂肪酸含量是粮食储藏过程中品质变化的敏感性指标。为了实现绿色储粮安全管理,该文采用多元线性回归(multiple linear regression,MLR)、人工神经网络(artificial neural network, ANN)、支持向量回归(support vector regression, SVR)、最小二乘支持向量回归(least square support vector regression,LSSVR)等机器学习算法模型,对东北地区稻谷储藏过程中的脂肪酸含量(以KOH计)进行预测。通过主成分分析(principal component analysis,PCA)方法筛选稻谷关键储藏参数,得到4个影响稻谷脂肪酸含量的关键因子,分别为稻谷入仓水分、入仓脂肪酸含量、储藏有效积温、检测粮温。然后,将得到的关键因子进行归一化处理,再分别输入到MLR、ANN、SVR、LSSVR模型,采用决定系数R2、平均绝对误差(MAE)、平均绝对百分比误差(MAPE)、均方根误差(RMSE)等评价指标对不同模型的预测性能进行对比,探讨稻谷脂肪酸含量预测的最优模型算法。研究结果表明,LSSVR模型的决定系数R2、MAE、MAPE、RMSE分别为0.911、0.275 mg/100 g、1.604%、0.348 mg/100 g,预测效果略优于MLR,明显优于ANN和SVR,LSSVR和MLR模型可作为稻谷储藏期间脂肪酸含量预测的方法。该研究实现了稻谷脂肪酸含量的预测,为科学储粮、安全绿色储粮提供参考。 相似文献
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草甸沼泽土壤硝化-反硝化作用和有机碳矿化对氮输入的响应 总被引:2,自引:0,他引:2
通过室内培养实验.研究了草甸沼泽土壤N2O排放和反硝化损失对氮输入的响应特征,结果表明,在培养期(23 d)内N2O平均排放速率为0.32(NO).0.87(N1).17.69(N2),28.07(N3)μgN2O-N/(kg±·h),反硝化平均损失速率为0.25(NO),0.81(NI),22.29(N2),30.28(N3)μgN2O--N/(kg±·h).两者都随氮输入量增高而升高.其中,N3处理N2O平均排放速率和反硝化平均损失速率与对照差异显著(p<0.05),N1和N2与对照差异不显著.N2O排放总量占氮输入的比例为0.03%(N1),1.04%(N2).1.76%(N3),反硝化损失总量占氮输入的比例为0.04%(N1),1.29%(N2),1.93%(N3).均表现为随氮输入量的增大而增高.N1处理下有机碳矿化速率低于对照,而N2和N3有机碳矿化速率高于对照,说明低氮输入对有机碳矿化有一定抑制作用,.高氮输入促进有机碳矿化. 相似文献
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该研究以江西稻田为研究对象,设置了不施氮对照(N0)、减氮40%(N1)、常规施氮(N2)、增氮50%(N3)等4个处理,采用静态箱-气相色谱法研究了稻田温室气体(N_2O、CH4、CO_2)的排放通量和速率,并计算了温室气体排放强度及全球增温潜势。结果表明:在晚稻栽培过程中,N_2O和CO_2的排放通量均出现3次峰值,且都表现为增施氮肥处理高于其他处理,而CH4排放通量仅出现一次峰值;N0、N1、N2的N_2O和CO_2的总排放量无显著差异(P0.05),但N3处理下的N_2O和CO_2的排放量显著高于其他处理(P0.05);与对照比,N1、N2和N3的CH4总排放量分别提高了58.70%、69.63%、96.15%,净增温潜势分别增加了22.34%、25.34%、52.92%;N3的温室气体排放强度最高,达1.12kg/kg,显著高于N1和N2。 相似文献
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为了研究储藏过程中不同温度和气调条件对稻谷品质劣化的影响,利用蛋白质组学技术探讨稻谷储藏陈化的分子机理,研究温度37℃、25℃和25℃+CO2气调下稻谷储藏90 d品质和蛋白质组的变化.结果表明,较37、25℃贮藏,25℃+CO2气调下稻谷储藏脂肪酸值升高最少,发芽率下降最少(P<0.05).稻谷储藏产生125个差异蛋白点,其中37个蛋白得到鉴定,根据蛋白质的功能可分为5类,包括代谢(45.9%),细胞结构(29.7%),抗胁迫(2.7%),功能性蛋白(5.4%)和其他蛋白(16.3%).并鉴定出4个目标蛋白,分别为蛋白酶体亚基β-1(B26、D09和F16),葡糖-1-磷酸腺苷酰基转移酶(C01和E07),ADP-葡萄糖焦磷酸化酶大亚基(B04和F04)和乙酰辅酶A(A06和C05).采用蛋白质组学技术分析稻谷储藏过程中蛋白质组变化,结果表明高温储藏促进稻谷差异蛋白表达,CO2气调储藏可降低差异蛋白表达.对差异表达蛋白功能分析表明,稻谷陈化可能与糖代谢紊乱、蛋白质分解能力降低,抗氧化酶活性降低,脂肪水解和氧化增强有关.研究结果为稻谷的合理、安全储藏提供参考. 相似文献
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综合产量和土壤N2O排放的马铃薯施氮量分析 总被引:4,自引:3,他引:1
施氮可提高作物产量,但同时也增加温室气体N_2O的土壤排放量。研究施氮量与产量和土壤N_2O排放的关系,对保障作物产量并兼顾环境效应的农业生产实践具有重要指导意义。该研究设置N0(0)、N1(67.5 kg/hm~2)、N2(125 kg/hm~2)、N3(187.5 kg/hm~2)4个施氮水平,采用静态箱-气相色谱法对土壤N_2O排放进行田间原位测定,研究施氮量对马铃薯产量、土壤N_2O排放的影响,分析综合产量与土壤N_2O排放的合理施氮量。结果表明:施氮显著增加马铃薯产量和土壤N_2O累积排放量,较不施氮(N0)处理,N1、N2和N3处理马铃薯产量增加78.5%、93.1%和95.6%;生育期N1、N2和N3处理马铃薯土壤N_2O累积排放量分别是N0处理的2.3、4.4和6.7倍。同时,随施氮量增加,N_2O排放系数、硝态氮强度和单产N_2O排放量均显著增加。在低氮处理(N0、N1)时,土壤N_2O排放通量与土壤温度、湿度显著正相关,而在高氮水平时,土壤N_2O排放通量与土壤硝态氮含量显著正相关。施氮67.5 kg/hm~2可确保研究区马铃薯产量并有效降低土壤N_2O排放。 相似文献
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稻麦轮作体系养殖肥水灌溉对产量、氨挥发和 氧化亚氮排放的影响 总被引:6,自引:0,他引:6
稻麦轮作体系进行养殖肥水灌溉可能导致氮(N)素的氨挥发(NH3)和氧化亚氮(N2O)排放增加。本文通过土柱模拟试验,定量评价了稻麦轮作体系推荐施N量(稻季225 kg/hm2,麦季150 kg/hm2)下,不同N浓度养殖肥水灌溉对水稻、小麦籽粒产量以及NH3挥发和N2O排放的影响。试验处理为:1无N检出的清水灌溉(CK),2低N浓度肥水灌溉(SI-L),3中N浓度肥水灌溉(SI-M)和4高N浓度肥水灌溉(SI-H)。稻季结果表明,NH3挥发与N2O排放量随灌溉肥水N浓度的提高而增加,其决定系数(R2)可达0.895与0.998。与清水对照相比,不同N浓度的肥水灌溉使NH3挥发增加19.7%~40.8%;SI-H处理N2O排放显著增加68.8%;不同N浓度肥水灌溉没有显著增加水稻产量。麦季结果亦表明,NH3挥发与N2O排放量随灌溉肥水N浓度的提高而增加,其决定系数(R2)可达0.939与0.980。与清水对照相比,SI-H处理使NH3挥发显著增加20.2%;SI-M与SI-H处理N2O排放分别显著增加64.9%和120.3%;SI-H处理小麦产量显著提高46.7%。利用稻田生态系统消纳养殖肥水中N时,须考虑肥水灌溉导致的NH3挥发和N2O排放所造成的环境影响,合理地进行水肥调控。 相似文献
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秸秆条带状覆盖对稻田CH_4和N_2O排放的影响 总被引:2,自引:1,他引:1
采用3种秸秆还田方式(对照、秸秆均匀混施和秸秆条带状覆盖)进行田间试验,观测稻田CH4和N2O的排放通量,以探讨秸秆条带状覆盖对稻田CH4和N2O排放的影响。结果表明:秸秆条带状覆盖的CH4排放量是对照的2.7倍,二者的N2O排放量无明显差异;秸秆条带状覆盖的稻田CH4排放量较秸秆均匀混施减少32%,其N2O排放量是后者的5.1倍;稻田排放CH4和N2O的全球增温潜势(GWP)为:秸秆均匀混施秸秆条带状覆盖对照,且差异显著;秸秆条带状覆盖的水稻产量分别较对照和秸秆均匀混施增加27%和17%。秸秆条带状覆盖是值得推荐的稻季秸秆还田方式。 相似文献
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为明确低O2高CO2贮藏环境对马铃薯块茎淀粉-糖代谢的影响,本试验以大西洋马铃薯为试验材料,研究体积分数为5%O2+2%CO2(CA1)、5%O2+4%CO2(CA2)、5%O2+6%CO2(CA3)、5%O2+8%CO2(CA4)及5%O2+10%CO2(CA5)的气体环境对马铃薯在4℃贮藏期间块茎中糖类、淀粉及淀粉-糖代谢相关酶[腺苷二磷酸葡萄糖焦磷酸化酶(AGPase)、尿苷二磷酸葡萄糖焦磷酸化酶(UGPase)、淀粉磷酸化酶(SP)及转化酶(INV)]活性的影响,并对块茎中还原糖含量的变化与淀粉-糖代谢相关因子进行相关性分析。结果表明,适宜的低O2高CO2贮藏环境可有效抑制淀粉含量、AGPase活性、UGPase活性的下降,并且能够抑制还原糖、蔗糖、果糖、葡萄糖含量及SP、INV活性的上升,CA1环境贮藏的马铃薯块茎在整个贮藏期间淀粉含量显著高于CK(P<0.05),还原糖、蔗糖、果糖及葡萄糖含量显著低于CK(P<0.05),AGPase、UGPase活性显著高于CK(P<0.05),而SP、INV活性均显著低于CK(P<0.05);相关性分析结果表明,还原糖含量与淀粉含量、AGPase活性、UGPase活性呈极显著负相关(P<0.01),与葡萄糖含量、果糖含量、SP活性及INV活性呈极显著正相关(P<0.01)。综上,马铃薯在CA1(5%O2+2%CO2)环境下贮藏可有效延缓块茎低温贮藏期间“糖化”现象的出现,AGPase、UGPase、SP、INV在贮藏过程中起到了一定的调控作用。本研究结果为加工型马铃薯的安全贮藏及明确“低温糖化”机理提供了理论依据。 相似文献
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【目的】分析施肥方式及添加脲酶/硝化抑制剂对稻田NH3挥发和N2O排放的影响,基于稻田NH3和N2O减排的效果评价优化施肥措施的可行性。【方法】在太湖地区开展为期两年的稻季田间小区试验,供试脲酶抑制剂为N-丁基硫代磷酰三胺(NBPT),硝化抑制剂为对羟基苯丙酸甲酯(MHPP),用量为施氮量的1%。设置6个处理:1)不施氮肥对照(CK);2)表施尿素N 300 kg/hm2 (当地常规施肥,CN);3)表施尿素N 225 kg/hm2(RNB);4)尿素N 225 kg/hm2,50%表施,50%深施(RND);5)表施尿素N 225 kg/hm2+NBPT+MHPP(RNB+DI);6)尿素N 225 kg/hm2+NBPT+MHPP,50%表施,50%深施(RND+DI)。每次施肥后两周内,用密闭式抽气法监测稻田NH3挥发,在水稻生育期内用静态箱—气相色谱法监测稻田N... 相似文献
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Anaerobic flasks with two different soils contained microorganisms which effectively reduced NO3− to N2 in the absence of C2H2 and in the presence or absence of CO2. In the presence of C2H2, the microorganisms reduced NO3− to N2O and the further reduction of N2O to N2 was temporarily inhibited. This was shown for two partial pressures of C2H2 (0.1 kPa and 1.0 kPa). However. after a maximum of 168 h, microorganisms were able to reduce N2O to N2 in the presence of C2H2. This was shown in the presence of CO2 for both partial pressures of C2H2 and in the absence of CO2 for 1.0 kPa C2H2. The absence of CO2 delayed the complete reduction of N2O. Microorganisms which had reduced N2O in the presence of C2H2 retained this ability for at least 3 days after the original atmosphere containing C2H2 had been removed. 相似文献
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Methane and nitrous oxide fluxes in an acid Oxisol in western Puerto Rico: effects of tillage, liming and fertilization 总被引:7,自引:0,他引:7
Changes in land use and management of tropical systems are considered to be major factors in the recent upsurge in increases in atmospheric nitrous oxide (N2O) and methane (CH4). Studies were initiated in western Puerto Rico grasslands to determine the effect of plowing, or liming and fertilizing an acid Oxisol on the soil–atmosphere exchanges of N2O and CH4. Weekly field flux measurements and field manipulation and laboratory studies were conducted over 22 months during 1993–1995. We found that N2O emissions from an Oxisol acidified to pH 4 were generally lower than from pH 6 Oxisol soils that were used as reference controls. Plowing the grasslands did not change mean N2O emission rates from either pH soil. Liming the acidified Oxisol to pH 6 tended to increase N2O emissions to the rates from the undisturbed grassland. Fertilizing the acidified grassland increased N2O emissions but much less than when these soils were both limed and fertilized. Short-term field studies employing nitrification inhibitors in which we measured nitric oxide (NO) and N2O emissions, demonstrated that nitrification rates generally control N2O emissions; thus these were lower in unlimed soil. It is likely that NO was produced through the chemical decomposition of nitrite, which in turn, was a product of biological nitrification. Soil consumption of atmospheric CH4 in the acidified Oxisol was about one-fourth of that in the pH 6 reference soil. Liming did not restore CH4 consumption in the acid soil to rates comparable to those in the reference Oxisol. We conducted a laboratory induction study to determine if incubation of these limed or unlimed acidified soils with high concentrations of CH4 could induce methanotrophic activity. Comparable uptake rates to the control soils were not induced by these incubations. These studies illustrate that management of soil can considerably affect the soil–atmosphere exchange of such trace gases as N2O and CH4 which can affect global atmospheric properties. 相似文献
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长期不同施肥下褐土养分及酶活性的生态化学计量特征 总被引:1,自引:0,他引:1
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基于川麦冬活性成分高和重金属含量低的有机无机肥最佳配施方案 总被引:1,自引:1,他引:0
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Effects of disturbance and glucose addition on nitrous oxide and carbon dioxide emissions from a paddy soil 总被引:1,自引:0,他引:1
The effects of disturbance and glucose addition on N2O and CO2 emissions from a paddy soil at 45% WFPS (water-filled pore space) and at 25 °C were determined. During a 45-day incubation, disturbances with and without glucose addition were imposed 0, 1, 3, and 5 times. The total amount of glucose added to soil with 1, 3, and 5 disturbances was equal (0.6% of oven-dry soil basis). Strong nitrification occurred in the paddy soil during the incubation. Disturbance alone did not influence N2O and CO2 emissions significantly, but disturbance with glucose addition did (P < 0.01). A flush of N2O as well as CO2 was always observed following disturbance with glucose addition. The discrepancy in N2O emission between disturbance alone and disturbance with glucose addition was ascribed to the different magnitude of denitrification and/or heterotrophic nitrification. Greater cumulative emission of N2O was observed in the treatment of three disturbance times with glucose addition (4.3 mg N kg−1 soil), compared with five disturbances with glucose addition (2.5 mg N kg−1 soil) and one disturbance with glucose addition (2.5 mg N kg−1 soil). Cumulative CO2 emission was significant larger in one and three disturbances with glucose addition than that five disturbance with glucose addition. Supplies of available organic C appear to be a critical factor controlling denitrification and/or heterotrophic nitrification processes and N2O emission under relatively low moisture conditions, i.e. 45% WFPS. 相似文献