红土旱地冬小麦根系生长动态观测

冬小麦根系的生长发育可概括为根系的形成、壮大和逐渐衰亡三个阶段。初生根对根乃至小麦的整体生育具有奠基作用。     

施氮量及氮磷钾比例对红土晒烟产质量的影响

为研究和探索红土晒烟适宜的施氮量和氮磷钾比例,为生产优质红土晒烟提供经济合理的科学施肥依据和指导方案,运用正交设计,在红土晒烟适宜种植区进行重复小区比较试验,研究不同施氮量和不同氮磷钾比例对红土晒烟生长发育情况、产量、产值和内在品质的影响,结果表明,不同施氮量和氮磷钾比例对红土晒烟的产量、产值、以及内在品质存在不同程度的影响,而对烟丝外观质量的影响较小,对植物学性状的影响没有规律。施氮量为75kg/hm2时产量和产值最高,增加到105kg/hm2时,产量反而略有下降,并且此时烟碱含量明显升高,平均超过3.0%。P2O5：N比提高对产量和产值的影响不大,并会使烟碱含量升高。提高K2O：N比,对红土晒烟的产量和产值没有增加作用,且烟叶含钾量也未有明显增加,但有助于降低烟碱含量。因此,红土晒烟适宜的施氮量宜控制在75kg/hm2或以下,P2O5：N宜为0.5：1,土壤磷含量较低、pH＞7的可增加到1：1;K2O：N宜为2：1,钾含量较低的土壤可增加到3：1。     

红土晒烟品种比较试验

以保山地区大面积种植的红土晒烟品种拉茄为对照,对不同种源的肯那、歪尾巴、沂水香烟、Va309等4个品种进行比较试验,通过生物学性状、农艺性状、外观质量的观察比较和对产量、产值的方差分析结果:参试品种均不及对照品种拉茄;歪尾巴、肯那综合性状表现相对较好,接近拉茄;而沂水香烟、Va309明显较差。     

羊驼AIF部分cDNA序列分析及其在不同毛色的表达定位

通过对已构建的羊驼皮肤cDNA文库进行筛选和ESTs分析,发现与其它动物AIF基因相应cDNA序列高度同源的序列,经序列分析证明命名为羊驼AIF基因序列,已经向Genbank提交。与其他动物（褐鼠、小鼠、人等）的AIF基因相应序列进行相似性比较,相似性分别为100%、91%、71.6%。运用免疫组化技术进一步研究该基因在羊驼皮肤中的表达和定位,结果显示AIF在羊驼毛囊的毛根、根鞘、毛球、毛乳头位置均呈阳性表达,且棕色皮肤比灰色皮肤表达量高,提示该基因可能和羊驼毛色形成或毛的生长相关。     

岩溶山地植被恢复中碳酸盐岩红土入渗特征及其影响因素

退耕还林还草工程实施后岩溶山地林草植被结构明显改善,研究植被恢复中碳酸盐岩红土入渗特征对岩溶生态恢复有重要意义。采用盘式入渗法在不同植被覆盖(荒草、灌草丛和乔木)下分别测定不同负压水头(-0.5,-3,-6,-15 cm)的水分入渗特征,计算不同负压下非饱和导水率、土壤孔隙分布常数、各孔隙级别对水流的贡献率,明确不同植被覆盖碳酸盐岩红土入渗特性差异。结果表明:不同水头条件下荒草、灌草丛和乔木地的土壤稳渗率均随负水头增大而递增,且碳酸盐岩红土入渗达到稳渗状态所需时间较长(约120 min),在低水头下荒草地土壤稳渗率最大(0.17 mm/min),而在高水头下乔木地最大(9.17 mm/min);荒草、灌草丛和乔木地土壤饱和导水率K_s差异极显著(P0.01),乔木地土壤饱和导水率达到最大(4.62 mm/min),而K_3、K_6、K_(15)和Gardner α差异不显著,碳酸盐岩红土饱和导水率K_s仅受土壤有机质含量和土壤电导率控制;乔木地土壤大孔隙数量及其占比显著大于灌草丛与荒草地(P0.05),碳酸盐岩红土导水性能主要受土壤大孔隙对水流的作用控制(70%)。研究结果可为西南岩溶山地生态恢复和水资源承载力分析提供数据支撑和理论依据。     

液体培养研究不同土壤中硝化活性

A red soil, a fluvo-aquic soil and a permeable paddy soil were used in a long-term investigation to study changes in nitrification with treatments: 1) soil incubation, 2) liquid incubation inoculated with soil samples, and 3) liquid incubation inoculated with ammonia-oxidizing bacteria (AOB) from the soils. There were significant differences (P < 0.001) in nitrification rates among the three soils when measured for 28 days by adding (NH4)2SO4 at the rate of 154 mg N kg-1 dry soil to fresh soil. However, the amounts of nitrifying bacteria in the three soils were not related to soil nitrification capacity. When the soil samples or the isolates of AOB enriched from the corresponding soil were incubated in liquid with pH 5.8, 7.0 and 8.0 buffers and 10 mmol L-1 ammonium nitrogen, there were no significant nitrification differences in the same soil type at each pH. The ability to oxidize ammonia through AOB from different types of soils in a homogeneous culture medium was similar, and the soil nitrification capacity could reflect the inherent properties of a soil. Altering the culture medium pH of individual soil type also showed that acidification of an alkaline fluvo-aquic soil decreased nitrification capacity, whereas alkalinization of the acidic red soil and permeable paddy soil increased their nitrification. For a better insight into factors influencing soil nitrification processes, soil properties including texture and clay composition should be considered.     

干湿循环下云南非饱和红土土—水特性研究

以云南红土为研究对象,以脱湿、吸湿引起的干湿循环作为控制条件,考虑初始干密度(1.20,1.25,1.30g/cm3)、初始含水率(30.0%,33.0%,36.0%)、预固结压力(0,50,100,200kPa)、过筛粒径(0.5,1.0,2.0mm)等影响因素,通过压力板仪法,研究干湿循环下云南非饱和红土的土—水作用特性。结果表明:干湿循环过程中,不同影响因素下红土的基质吸力随含水率的增大而减小,其土—水特征曲线呈直线型或倒J形,其脱湿变化过程可以分为快速脱湿、缓慢脱湿、稳定脱湿3个阶段,对应的吸湿变化过程也可以分为快速吸湿、缓慢吸湿、稳定吸湿3个阶段。相同基质吸力下,随初始干密度、初始含水率、预固结压力的增大,红土的含水率增大;随粒径的增大,红土的含水率减小。初始干密度、预固结压力、粒径(0.5mm除外)影响下的红土的土—水特征曲线可采用幂函数关系进行拟合,不同初始含水率、粒径0.5mm时的土—水特征曲线可采用线性函数关系进行拟合。红土脱湿过程的含水率高于吸湿过程的含水率,脱湿—吸湿过程中的土—水特征曲线存在滞后现象,其实质在于干湿循环作用下红土具有孔隙效应、瓶颈效应、角度效应的综合结果。     

红壤中水热耦合转化的实验和数值模拟研究

Coupled transfer of soil water and heat in closed columns of homogeneous red soil was studied under laboratory conditions.A coupled model was constructed using soil physical theory,empirical equations and experimental data to predict the coupled transfer.The results show that transport of soil water was affected by temperaature gradient,and the largest net water transport was found in the soil column with initial water content of 0.148m^3m^-3,At the same time,temperature changes with the transport of soil water was in a nonlinear shape as heat parameters wre function of water content,and the changes of temperature were positively correlated with the net amount of water transported.Numerical modelling results show that the predicted values of temperature distribution were close to the observed values,while the predicted values of water content exhibited limited deviation at both ends of the soil column due to the slight temperature changes at both ends .It WAS indicated that the model proposed here was applicable.     

沙棘生态功能应用

沙棘是优良的多用途树种,也是典型的克隆植物。其侧根(萌蘖根)在水平延伸过程中能产生大量的根蘖苗,具有极强的克隆繁殖和空间拓展能力,可依靠克隆生长赋予的生理整合作用及觅养行为等特性,提高资源的利用效率以及自身的繁殖生存;并能通过林窗更新、平茬以及林缘扩散等途径维持种群的稳定性和持久性。因此,被广泛应用于水土保持、防风固沙、治理砒砂岩以及防止红土泻溜等方面。本文就其生态功能进行概述。     

Aggregate Stability and Its Relationship with Some ChemicalProperties of Red Soils in Subtropical China

The stability of aggregates in the surface soil is crucial to soil erosion and runoff generation. Thus, to understand the stability and the breakdown mechanisms of soil aggregates as well as the relationship between aggregate stability and selected soil chemical properties, such as different forms of Fe and A1 oxides, organic matter, CEC and clay content, the aggregates of slightly and severely eroded red soils derived from Quaternary red clay in subtropical China were analyzed using the routine wet sieving and the Le Bissonnais methods. The results indicated that the aggregates of the severely eroded soils were more stable than those of the slightly eroded soils. Different aggregate breakdown mechanisms resulted in different particle size distribution. The slaking from entrapped air in aggregates severely destroyed the soil aggregates,especially in the slightly eroded soils. Meanwhile, mechanical breakdown and microcracking had little effect on the aggregates compared to slaking. The fragments resulting from slaking were mainly microaggregates that increased in size with increasing clay content. The main fragment size of the slightly eroded soils was 1.0-0.2 mm, while for the severely eroded soils it was 5.0-2.0 mm and 1.0-0.5 mm. Overall, more than 20% of the fragments were smaller than 0.2 mm.In addition, aggregate stability was positively and often significantly correlated with Fed, Ald, Feo and clay content, but significantly and negatively correlated to SOC.