Soil aggregate formation and stability induced by starch and cellulose

Soil aggregate (SA) can be formed and stabilized when soil organic matter (SOM) is decomposed in the soil. However, the relationships between the SA dynamics and SOM with different decomposition rates have not been clarified. Therefore, this study examined the effects of the addition of polysaccharides to soil on SA formation and stability. A Japanese tropical soil was incubated for 99 d at 30 °C in a dark environment following the addition of 0.5% (w/w) starch or cellulose. The decomposition rates of the amendments, and SA formation and stability were evaluated by measuring soil respiration rates, and distribution fractions of soil aggregate sizes and mean weight diameter (MWD) of SA, respectively. The cumulative soil respirations with all treatments rapidly increased until Day 12 of the incubation. The initial slope of the cumulative soil respiration in the soil with starch was significantly higher than that in the soil with cellulose. In either soil with starch or cellulose, the fractions of macro-aggregates (>1000 μm in diameter) significantly increased, respectively, compared with control soil. However, the fractions of meso-aggregates (250–1000 μm) and nano-aggregate (<20 μm) in the soil with starch significantly decreased, while those fractions in the soil with cellulose fluctuated until Day 6. The MWDs reached the maximum on Day 6, indicating the SA formation in the soils with starch or cellulose. The increasing rate of the SA formation in the starch-amended soil was greatly higher than that in the cellulose-amended soil. After Day 6, the MWDs in the soils with either polysaccharide decreased with similar trends with no significant differences between treatments, indicating similar stability of the SA in both treatments. This study showed that the different decomposability of the organic amendments might influence the SA formation differently, but not the SA stability.     

紫花苜蓿根腐新病原-厚垣镰孢菌生物学特性研究

针对紫花苜蓿根腐致病菌厚垣镰孢菌(Fusarium chlamydosporum)在不同温度、光照、p H和多种碳氮源条件下的生物学特性,采用菌饼法进行了测定,并对不同碳氮源下菌落产色素情况进行了连续观察。结果表明:该病原菌在5~40℃均可生长,最适温度为25℃;当p H 4.0~12.0时均能生长,最适宜p H为7.0;全黑暗条件有利于菌丝生长,菌丝生长最适碳源、氮源分别为山梨醇和蛋白胨,碳源氯醛糖及除蛋白胨以外8种氮源均不利于菌丝的生长。含不同碳氮源培养基可诱导菌丝产生不同色素,且颜色变化差异大,在不同的生长阶段,色素颜色也会发生变化。     

应用压力早期恢复资料确定低渗地层压力

低渗透油藏的压力恢复曲线,不能用Horner外推压力求取地层压力。基于Horner方程的等轴双曲线形式,提出了应用压力早期恢复资料确定低渗地层压力的新方法。通过油井实际资料计算验证,用该方法计算的地层压力准确可靠,较好地解决了低渗透油藏求地层压力的问题。     

覆盖方式对旱地小麦花后旗叶抗氧化生理及粒重形成的影响

于2017—2018年和2018—2019年,在西北中部旱作雨养农业区以冬小麦‘康庄974’为试验材料,设秸秆带状覆盖(SM)、地膜覆盖(PM)和无覆盖对照(CK)共3个栽培处理,分析不同覆盖方式对小麦灌浆期土壤水分和温度及抗氧化能力的影响,探讨花后干物质积累量和粒重形成的关系。结果表明,随生育期推进,花后旗叶相对含水量(RWC)逐渐降低,丙二醛(MDA)含量逐渐升高,且PM较SM降、升幅度明显。与CK相比,覆盖显著提高花后旗叶抗氧化酶活性,增加渗透调节物质含量;开花时间越长,SM抗氧化酶活性升高的幅度越大,而PM主要提高花后7 d旗叶抗氧化能力。SM和PM的粒重分别较CK增加14.3%和19.1%(P<0.05)。相关分析表明,土壤水分(SW)是影响旗叶生理活性的关键因子,提高SW,有利于增加RWC(r=0.84^**),从而提高旗叶抗氧化能力,其中RWC和抗坏血酸酶(ASA)活性呈极显著正相关关系(r=0.82^**);ASA活性和脯氨酸(Pro)含量呈极显著正相关关系(r=0.94^**),和MDA含量呈极显著负相...     

根系生长与土壤物理性状之间的关系

根系生长在土壤之中,土壤物理条件的改变会对根系生长产生直接或间接的影响.为此,通过分析土壤主要物理条件,对土壤物理环境与作物生长之间的关系进行了评述,并对目前研究中存在的不足及今后需深入的研究领域提出了建议.     

农业机械系统配备量优化研究

农业机械系统选型配套是研究机械化的重要基础性工作,同时也是确保优质和高效完成各项作业的重要条件。为此,对目前农业机械配备方法进行了研究与分析,提出采用流水作业下的农业机械线性规划配备模型来进行配备量研究,对农业机械化取得良好经济效益有很好的推进作用。     

兴安落叶松容器苗化学剪根效果与根生长潜力测定的研究

采用内壁涂有不同浓度碳酸铜的容器培育出兴安落叶松(Larix gmelini(Rupr.)Rupr.)苗木,苗木侧根受碳酸铜的抑制,减小了根系变形的程度。通过对处理苗木根生长潜力的测定表明:碳酸铜浓度为100～150g/L时改变了兴安落叶松容器苗新根的分布状态,根系中、上层的新根数量明显增加,这样的苗木根系更接近自然发育的苗木根系,从而克服了一般容器苗根系易变形的缺点。     

生长素在烤烟库源关系改变时对烟株根系钾的影响

采用土培试验方法，研究内外源生长素在不同生长阶段缺钾或供钾条件下对烟株根系钾的影响。结果表明：缺钾胁迫下，外源生长素在不同地烟株根系积累钾有很大的促进作用，内源生长素在腰叶成熟前对烟株根系积累钾的能力有一定的稳定作用。供钾条件下，内外源生长素在不同生长阶段对烟株根系积累钾均有很大的促进作用，其促进作用比缺钾胁迫时大。且无论缺钾与否，外源生长素对烟株根系积累钾的促进作用大于内源生长素的作用。     

嫩江沙地几种植物根系垂直分布的研究

采用全部分层挖取法研究了银中杨(Populus alba×Populus berolinensis)、沙棘(Seabuckthorn)、沙枣(Elaeag-nus angustifolia)和山杏(Prunus arm eniaca)4个树种的根系分布情况。结果表明:各树种之间根系的垂直分布差异显著,银中杨根系在0～120 cm土层中均有分布,林龄越大分布越深,但主要集中在0～40 cm的土层中,而且以直径小于7 mm的根系为主;沙棘根系分布较浅,在0～30 cm土层中,分布相对均匀;沙枣根系分布最深仅达20 cm;山杏的根系分布虽可达130 cm,但主要还是集中在10～50 cm土层中。根系总量分布由大到小依次是银中杨、沙棘、沙枣、山杏。