长期施肥对黑土呼吸过程的影响

土壤呼吸是土壤有机C矿化分解,释放无机养分的重要生物化学过程。对公主岭地区长期有机肥(不施有机肥、施中量和高量有机肥处理)与化肥(不施化肥、施用N、NP、NPK化肥)配合施用的12个处理的黑土进行室内好气培养(196天),采用一级动力学方程模拟土壤的呼吸过程,结果表明,有机肥和化肥的施用能显著增加土壤呼吸释放的CO2 -C的累积量,提高土壤中潜在矿化的有机碳含量及其占土壤有机质的比例,促进土壤有机质中无机养分的释放,有利于提高土壤养分的有效性,改善黑土的供肥状况。有机肥与NPK化肥配合施用效果更为明显。     

Kinetic Parameters of Gross N Mineralization of Peat Soils as Related to the Composition of Soil Organic Matter

Peat land has been considered as an alternative type of land for agricultural development especially in the tropics. In the present study, the N-supplying capacity, one of the most important soil properties in terms of crop production, of peat soils was examined. Ten peat soil samples were collected from Indonesia, Malaysia, and Japan. Gross N mineralization in the soil samples was estimated using a zero-order model, and kinetic parameters of mineralization were determined using a simple type model. Soil organic matter composition was investigated using ¹³C CPMAS NMR. Mineralization potential ( N ₀), apparent activation energy ( E _a), and mineralization rate constant ( k ) ranged between 571–2,445 mg kg⁻¹, 281–8,181 J mol⁻¹, and 0.009–0.020 d⁻¹, respectively. Although none of the parameters showed a significant correlation with the soil C/N ratio, a negative correlation was observed between the k value and the ratio of the proportion of alkyl C in total C to that of O -alkyl C estimated by ¹³C CPMAS NMR. The latter suggested that the k values were higher in the peat soils relatively rich in readily decomposable organic matter including carbohydrates.     

Isotopic detection of recent photosynthate carbon flow into grassland rhizosphere fauna

In this study, we measured the incorporation of recent photosynthate-C inputs into active rhizosphere fauna (earthworms, enchytraeids, mites and collembolans) in an upland grassland soil under natural environmental conditions. This was achieved by means of a ¹³CO₂ pulse-chase experiment made during the growing season, followed by a 20-day dynamic sampling of soil fauna for ¹²C/¹³C analysis by IRMS. The effect of post-¹³C labelling defoliation (cutting) on fauna ¹²C/¹³C ratios was also examined.Results showed that earthworms made up over 93% of the extracted fauna biomass, while mites, collembolans and enchytraeids together accounted for less than 7%. All fauna groups showed evidence of tracer ¹³C in their tissues within a week of ¹³CO₂ pulse labelling in both control and cut treatments. Cutting significantly increased the amount of tracer ¹³C entering the organisms (P=0.0002). Similarly, the fauna group also had a significant effect (P=0.0001). Time did not have any effect on fauna ¹³C content between groups as differences were only significant at the last sampling occasion. The interaction time×animal group, however, had a significant effect (P=0.0054).Collembolans accounted for most of the tracer ¹³C measured within the fauna biomass, i.e. mean±standard deviation of 44.78±12.75% and 44.29±14.69% of fauna ¹³C in control and cut treatments, respectively. Mites and earthworms contained between 22.13% and 28.45%, and enchytraeids less than 6% of the tracer ¹³C. We conclude that, during the growing season, there was a rapid incorporation of recent photosynthate-C into rhizosphere mesofauna. This carbon transfer was most significantly increased by defoliation in mites and collembolans (P<0.01). These results provide evidence that soil foodweb carbon dynamics are not solely underpinned by detrital decomposition but are also affected by short-term plant rhizodeposition patterns.     

沼泽垦殖前后土壤呼吸与CH_4通量变化

湿地是陆地生态系统的重要组成部分,在碳的储存中起着重要作用。湿地垦殖后,在相同季节根层土壤温度明显高于沼泽湿地土壤,但垦殖后土壤有机碳、氮素含量明显降低,C:N比值减小,土壤呼吸通量增大,且具有季节性变化。垦殖8年的农田土壤,呼吸通量大于垦殖15年的农田土壤,弃耕后土壤有机碳含量及土壤呼吸强度有所增加,土壤呼吸通量与土壤温度呈显著正相关关系。沼泽湿地土壤为大气CH4的重要源,通量季节性变化明显,沼泽垦殖后农田土壤成为CH4的汇,不同垦殖年限土壤间CH4通量差异性不大。     

淹水土壤有机酸积累与秸秆碳氮比及氮供应的关系

有机酸积累和毒害是稻田秸杆还田中受到广泛关注的问题。本文以水稻与小麦秸杆为材料，采用淹水培养研究了甲酸、乙酸、丙酸及丁酸在士壤中的积累及其与秸秆碳氮比、氮肥添加量的关系。结果表明，在不施用氮肥的情况下。随秸秆用量的增加，秸秆处理的有机酸积累均显著增多。与稻秸处理相比，麦秸处理的有机酸（尤其足丙酸）积累量显著较高，土壤溶液中NH4^＋浓度显著较低。加入尿素明显减少有机酸积累，促进CH4排放，但对CO2的排放无显著影响；氮素的影响在麦秸处理中表现的尤为明显。上述结果说明麦秸的高碳氮比增加了无机氮的生物固定，抑制有机酸向CH4转化，从而导致麦秸处理有机酸积累量高于稻秸处理。施用氮肥是减少麦秸还田后有机酸积累的有效措施之一，但此措施将可能促进CH4的排放。     

农田管理措施对滨海盐渍化土壤碳平衡的影响

为研究不同农田管理措施对滨海盐渍土壤碳平衡的影响,通过玉米-小麦轮作试验,研究农田土壤碳收支情况。试验共设6个处理:(1)常规对照(CK),(2)有机肥常量(OF),(3)氮肥增施(NF),(4)秸秆还田(S),(5)有机肥加秸秆(OF+S),(6)免耕(NT)。结果表明,秸秆还田和施用有机肥提高了土壤呼吸的强度,而NT处理的CO_2平均释放量最低,不同处理下土壤呼吸表现为OF+S处理S处理OM处理NF处理CKNT处理。各处理土壤有机碳量随着作物种植年份的增加而逐渐升高,其中OF与NT处理增加最多,而NF处理并没有显著提高土壤的有机碳量。在两季作物收获后,各处理的碳输入均高于碳输出,表现为碳净输入,呈现较强的碳汇特征。S处理和OF处理的碳净输入均显著高于CK,可有效减缓土壤CO_2排放,增加其有机碳的输入。     

不同覆盖方式对植烟土壤温度和水分及烤烟品质的影响

不同覆盖方式的比较试验结果表明,秸秆与地膜双覆盖能够协调烤烟生长全过程的土壤温度,并且地温日变化幅度小,蓄水保墒作用显著。秸秆单覆盖对土壤性状改良与秸秆和地膜双覆盖相似,烟叶内在化学成分较协调,品质较高,但由于在烤烟生长前期不能提高土壤温度,使得烟叶生长速度较慢,产量下降;地膜单覆盖对土壤性状改良不及秸秆单覆盖和秸秆与地膜双覆盖,秸秆和地膜双覆盖使0~20cm土层含水量平均比露地栽培提高16.82%,比秸秆单覆盖提高6.45%,比地膜单覆盖提高5.43%,而且烟叶成分较协调,产量与产值也较高。     

纽荷尔脐橙成年态节间茎段遗传转化研究

建立柑橘成年态节间茎段的离体再生和遗传转化系统是实现柑橘转基因育种实用化的前提基础。本试验以纽荷尔脐橙成年态节间茎段为试材,初步建立了脐橙成年态节间茎段的离体再生和遗传转化系统。结果表明采用改良的预处理灭菌法对成年态茎段进行消毒处理,污染率明显降低。节间茎段在MS＋3mg／L6-BA的培养基上,不定芽再生率较高。采用根癌农杆菌介导法将外源抗真菌病基因chit42导入其中,抗性芽通过二次嫁接后获得再生植株,PCR检测4株抗性植株中有2株扩增出该特异性条带,RT-PCR分析进一步确认外源基因chit42能够在转基因植株的基因组中表达。     

玉米种质C8605-2在品种改良中的应用

C8605-2是国内优良的玉米骨干自交系之一,它在新品种选育和种质改良创新中都得到了广泛的应用。加强其研究和利用,对丰富和发展种质资源、培育优良品种必将会起到极大的促进作用。     

成熟期库尔勒香梨理化指标变化规律及相关性研究

为了研究库尔勒香梨成熟过程中理化指标的变化规律,探求成熟期库尔勒香梨主要理化指标间的相关性,以成熟期库尔勒香梨为研究对象,研究库尔勒香梨果实硬度、叶绿素含量、SSC(可溶性固形物含量)和维生素C含量的变化规律;采用相关分析和回归分析的方法,应用Spss软件和Excel软件对指标均值以及各指标间相关性进行了分析,并对试验结果进行了实验验证。研究结果表明:在成熟期内,库尔勒香梨果实理化参数变化范围分别为:硬度4.23~7.99 kg/cm2、叶绿素3.17~6.54 mg/100 g、SSC11.54%~15.41%、维生素C 1.9~4.2 mg/1 0 0 g;随着成熟的深入,果实硬度逐渐降低、叶绿素含量逐渐减少、SSC逐渐增加、维生素C含量逐渐增加;各指标均值在0.01水平上显著相关。回归分析过程中选取最优的拟合方式,并建立相应的数学模型,果实硬度和SSC与叶绿素含量和维生素C含量间决定系数均大于0.95,验证试验预测值与测量值误差小于3.2 1%,在库尔勒香梨成熟过程中可应用果实硬度和SSC对叶绿素和维生素C含量进行预测。研究结果能够为库尔勒香梨成熟度评价和分级提供参考。