离散元模拟导种管高度对排种性能的影响

排种系统是免耕播种机的重要组成部分,其性能直接影响到免耕播种机整体工作质量。导种管为排种系统最后一个环节,主要作用是将排种器排出的种子导入开沟器并使种子能够顺利落入种沟内,其投种位置和速度对排种系统的排种均匀性有较大影响。本文用离散元软件,对导种管施加直线运动和正弦振动,模拟玉米种子由颗粒工厂生成后,经过导种管下落到土地的过程。同时,经离散元后处理模块得到玉米种子在土地上的分布图、种子的运动轨迹及种子在导种管内运动的最小速度和种子离开导种管时的速度;并用origin软件得到种子在导种管内运动的最小速度与导种管高度的拟合曲线、种子离开导种管时的速度与导种管高度的拟合曲线。模拟结果表明:当免耕播种机作业速度为1.389m/s时,最佳导种管高度应为500mm。     

不同灌水定额下核桃树吸水根系分布研究

以8a生核桃树为研究对象,采用分层分段挖掘法研究核桃树根系的空间分布,探讨滴灌条件下不同灌水定额处理组对核桃根系的作用效应,分析土层深度与水平距离变化对根长密度的影响,并建立根系密度分布函数。研究结果表明:在核桃成熟期,根长密度的一维垂直分布中,吸水根系集中分布于0~60cm,水平方向,根系集中分布于0~90cm。在垂直二维吸水根长密度分布中,C1处理主要分布在垂向0~80cm、水平0~90cm的范围内,C2处理主要分布在垂向0~60cm、水平0~90cm的范围内,C3处理主要分布在垂向0~100cm、水平0~90cm的范围内,其中尤以C3处理的根长密度分布居多。对比二元二次回归模型,利用二元多次方程拟合根长密度、水平距离与土层深度之间的关系,其函数相关度较好,可以应用于灌水施肥策略调整。     

用于砂土层连续采样的柔性软袋式钻取采样技术研究

砂土是地球表面常见的一种覆盖物,由于风力和水力的搬运作用导致传统浅层采样器所采集的样芯信息量不足,并且由于砂土颗粒之间的内聚力小流动性大,传统环刀压入方法无法采集到长度大于20cm并且具备连续层序信息的样品。为此提出一种柔性软袋式取芯技术,采用内置柔性袋取芯机构的外螺旋钻具对砂土进行钻取采样,以提高采样的样芯长度并保持层序信息。分析了取芯钻具与砂土相互接触的机理以及对采样样芯的扰动情况,通过仿真模拟的比对揭示了传统环刀压入法对样芯扰动的原因。搭建了试验台并针对传统环刀压入法与柔性软袋式取芯方法的采样率进行了对比试验,结果显示后者取芯率随转速增加下降10.4%,前者随压力增加提高16.4%,使用柔性软袋方法取芯率均值从13.08%提高到84.08%,并能保持连续的样芯层序信息。     

汇水面积阈值对土壤侵蚀定量评价的影响

土壤侵蚀预报模型是定量评价水土流失和评估水土保持措施效益的重要手段。通用土壤流失方程(Universal Soil Loss Equation,USLE)和中国土壤流失方程(Chinese Soil Loss Equation,CSLE)被广泛应用于土壤侵蚀定量评价。这些模型中坡长的计算受汇水面积阈值的影响较大。为揭示汇水面积阈值对土壤侵蚀定量评价的影响,选取北方土石山区、西北黄土高原区、东北黑土区、南方红壤丘陵区、西南紫色土区、西南山地区和西南岩溶区210个流域面积在0.2~3.0km~2的小流域,以1∶10 000地形图10m分辨率DEM为数据源,分别计算了1 000,1 500,2 000,2 500,3 000,5 000,7 000,9 000,11 000,13 000,15 000m~2共11个汇水面积阈值下各小流域不同坡长、土壤侵蚀强度级别以及土壤侵蚀的面积比例,分析了它们对汇水面积阈值变化的敏感性。结果表明:平均坡长、土壤侵蚀面积和轻度以上各级别的侵蚀强度面积比例都随汇水面积阈值的增加先增加而后趋于稳定。微度侵蚀面积比例随汇水面积阈值的增加逐渐减小并趋于稳定。当汇水面积阈值由1 000m~2增加到15 000m~2时,北方土石山区、西北黄土高原区、东北黑土区、南方红壤丘陵区、西南紫色土区、西南山地区和西南岩溶区的平均坡长分别增至阈值为1 000m~2时的1.53,4.16,1.95,1.90,1.69,1.57,1.47倍;土壤侵蚀面积比例分别增至阈值为1 000m~2时的1.20,1.85,1.43,1.37,1.77,1.44,1.30倍。汇水面积阈值对各分区的影响程度存在差异。从平均坡长和土壤侵蚀面积来看,东北黑土区受汇水面积阈值的影响最大。研究结果不仅为精确评价土壤侵蚀提供了数据支撑,而且对水土保持综合防治措施的评价和优化具有指导意义。     

Interaction Between Plant Roots and Soil Water Flow in Response to Preferential Flow Paths in Northern China

Preferential flow is expected to provide preferential channels for plant root growth and variations in soil water flow, but few studies were conducted to imply the impacts of these changes, particularly for preferential flow in stony soils. This study aimed to characterize soil water flow and plant root distribution in response to preferential flow paths and quantitatively describe the relation between plant root distribution and soil water flow. Field dye‐tracing experiments centered on experimental plants were conducted to determine the root length density and soil water flow process. Laboratory analyses were performed to characterize changes in the relative concentration of the accumulated effluent and the degree of interaction between plant roots and soil water flow. The amount of fine plant roots with preferential flow paths decreased with increasing soil depth for all experimental plots. The largest plant roots were recorded in the upper soil layers to a depth of 20 cm. The relative concentration of the accumulated effluent increased with time and decreased with soil depth under saturated soil conditions, whereas a distinct early turning point for the relative concentration of the accumulated effluent was observed in the 0–20‐cm soil columns, and the relative concentration of the accumulated effluent initially decreased and then increased with time under unsaturated soil conditions. This study provides quantitative information with which to characterize the interaction between plant roots and soil water flow in response to preferential flow paths in soil–plant–water systems. Copyright © 2016 John Wiley & Sons, Ltd.     

Repeated annual drought has minor long‐term influence on δ13C and alkane composition of plant and soil in model grassland and heathland ecosystems

As a result of global climate change the incidence of drought conditions in Europe is predicted to increase in the future, which also influences plant resistance. Lipids are important plant constituents that protect plants against drought stress and contribute to the intermediate stable carbon (C) pool in soil. However, the extent to which drought influences lipid cycling in the plant–soil system is unknown and, therefore, it remains questionable how the ecosystem recovers after drought. We focused on plant and soil samples from two different plant communities (temperate grassland and heathland) that had been exposed to 5 years of 4.5–6.0 weeks repeated annual drought. They were sampled one year after the last drought to check the recovery of the plant–soil system. Samples were analyzed for their bulk C, stable C and nitrogen (N) isotope (δ¹³C, δ¹⁵N) and lipid composition. Contrary to our expectation, no strong influence of five years of repeated annual drought was observed for above‐ground biomass, roots and soils in the model ecosystems with respect to elemental (C and N concentrations, C : N ratio) bulk isotope (δ¹³C, δ¹⁵N) composition and the total extractable lipid concentration. Thus, plants did not sustain a significant change in their C and lipid concentration as well as their composition after five years of repeated annual drought. This might be related to the comparatively short drought period related to the overall growth season and provides evidence for recovery of the C and lipid dynamics in temperate grassland and heathland model ecosystems exposed to annual drought.     

坡长对径流及侵蚀的影响

张家口市水保试验站坡长小区五年观测资料表明,降雨强度影响径流量、侵蚀量随坡长的变化。降雨强度较小时,径流量不能用坡长与降雨强度的乘积代替,侵蚀量随坡长增加较慢。降雨强度较大时,径流量可用坡长与降雨强度的乘积代替,侵蚀量方程中坡长指数较大。     

Genetic diversity of sulfonylurea-resistant and -susceptible Monochoria vaginalis populations in Japan

Monochoria vaginalis is one of the most serious weeds of rice fields in Asia. The species is predominantly selfing. To reveal the potential for multiple mutational events, outcrossing and gene flow in the sulfonylurea‐resistant (SU‐R) M. vaginalis populations, we investigated (i) if each SU‐R population was a single SU‐R biotype or a mixture of several SU‐R biotypes using restriction analysis or direct sequencing of acetolacatate synthase (ALS) genes and (ii) genetic diversity of SU‐R and ‐susceptible (S) populations using amplified fragment length polymorphism (AFLP) analysis. Nineteen or 20 individuals were sampled from four SU‐R and five SU‐S populations respectively. Amino acid substitutions conferring resistance in the SU‐R populations were Pro₁₉₇Ser in the ALS1 or ALS3, or Asp₃₇₆Glu in the ALS1 and each SU‐R population was composed of a single SU‐R biotype. In cluster analysis each SU‐R individual formed a cluster, whereas the individuals from a SU‐S population belonged to different clusters. Some SU‐R populations showed polymorphic AFLP loci. The results indicated that these SU‐R biotypes emerged from a single mutational event and any gene flow of SU‐R genes from adjacent populations did not occur. A low level of outcrossing and recombinations of SU‐R genes occurred within some SU‐R populations of M. vaginalis.     

基于毛细管网的日光温室主动式集放热系统研究

为了对比日光温室传统保温蓄热后墙与基于毛细管网的主动式集放热系统（AHSCTM）的集放热性能,对AHSCTM的集放热性能进行了测试,构建了AHSCTM水温模型,利用一维差分法对相同环境条件下的外保温复合墙（370mm黏土砖和100mm聚苯乙烯板复合而成）日间储热量和夜间放热量进行了模拟。结果表明,AHSCTM的日间储热量和夜间放热量分别为相同条件下外保温复合墙的84.4%~111.3%和74.8%~100.7%,AHSCTM的COP（Coefficient of performance）为1.1~2.4。在夜间运行期间,AHSCTM放热量是相同时间段内外保温复合墙的98.2%~172.5%。因此,与外保温复合墙相比,AHSCTM有利于提高室内最低气温。改进AHSCTM的日间储热量和夜间放热量得到大幅提升,分别较外保温复合墙高67.6%~112.1%和69.0%~128.3%,COP可达2.8~7.0。改进AHSCTM的储放热性能优于外保温复合墙,说明利用改进AHSCTM配合保温墙体替代传统保温蓄热后墙是可行的。     

木棉雄蕊特征与其繁殖策略的关系分析

采用野外观察和实验室检测方法,对云南省个旧市冷墩村的木棉花部结构、雄蕊特征、花粉活性进行研究。结果表明,自然种群中花部形态特征具有一定变异性,3层雄蕊变异系数大小关系显著。在湿度为60%、温度为35℃时花粉活性最强。研究发现,木棉雄蕊长短变化可能有利于不同传粉生物传粉效率提高和增强适应性;木棉高层雄蕊花药个体大、花粉数量多、活性高,适应干热河谷传粉繁殖条件;温度较低时,底层花药花粉活力相对较高,可为逆境环境下木棉高层花药受损后提供后备花粉源。文章就木棉花部形态与繁殖关系、木棉形态及花粉活力对繁殖的影响进行讨论。