贵州花生新品种(系)的丰产性与稳产性分析

利用非参数度量法对2003~2004年贵州省花生区域试验资料进行了丰产性与稳产性分析。结果表明:试点设置是合理的;油育94-13的丰产性和稳产性好于其它组合(品种);油育94-2013、黔花024两组合丰产性好,但稳产性较差。     

日本细毛环腹瘿蜂对斑翅果蝇的寄生效能

日本细毛环腹瘿蜂Leptopilina japonica是斑翅果蝇Drosophila suzukii的优势寄生性天敌之一, 对斑翅果蝇具有良好的生防潜力。为更好地利用日本细毛环腹瘿蜂防控斑翅果蝇, 本研究在室内观察了日本细毛环腹瘿蜂的行为活动和生长发育特征。采用室内接虫法研究了该蜂对斑翅果蝇2龄幼虫的寄生能力。分别运用Holling Ⅱ型圆盘方程、搜寻效应方程和Hassell-Varley模型拟合分析了日本细毛环腹瘿蜂的寄生功能反应、搜寻效应和自身密度干扰效应。结果表明:日本细毛环腹瘿蜂的寄生功能反应符合Holling Ⅱ模型, 其拟合方程为:Na=0.70N/(1+0.03N); 寄生效能(a/Th)为15.78; 在一定空间内, 寄生蜂的寄生量随寄主密度增加而增大, 至寄主密度达25头/罐后寄生量趋于平稳; 寄生蜂的搜寻效应随着寄主密度的增加而减弱; 当斑翅果蝇的密度分别为10、20、30头/罐时寄生蜂自身密度干扰模型分别为E10=0.487 8P-0.871 3; E20=0.442 0P-0.676 8和E30=0.346 2P-0.433 7, 在同一寄主密度下, 日本细毛环腹瘿蜂的寻找效应均随自身密度的增加而减弱。日本细毛环腹瘿蜂对斑翅果蝇2龄幼虫具有较好的寄生效能, 但寄主密度较大会导致日本细毛环腹瘿蜂的寄生效能减弱, 随着寄生蜂自身密度的增加, 其种内个体间会出现干扰作用。     

基于激光雷达扫描的料仓原料储料量测量方法

为提高仓内原料储料量测量自动化和智能化水平,设计了一种基于二维激光雷达扫描的储料量测量装置与系统。本系统采用RPLIDAR S1型二维激光雷达扫描获取不同储料量物料的原始点云数据,通过坐标变换、重叠点提取、滤波、分割等方法对原始点云进行预处理,采用贪婪投影三角化算法将预处理后的点云进行三维重建,获得仓内原料的三维模型,结合物料三维模型和物料的容重获得仓内原料的储料量,从而实现储料量的自动测量。以玉米为试验对象,测量小型储料塔内玉米储料量并对玉米不同储料量进行扫描测量,验证模型的准确性,结果显示：测量结果的平均绝对误差为8.05 kg,平均相对误差为1.52%。研究结果表明,基于二维激光雷达扫描的储料量测量方法是可行的,具有较好的稳定性和测量精度,能够满足实际生产需求。     

湖北省不同地区水稻土对几种养分的吸附能力研究

对湖北省4个不同地区典型水稻土的磷(P)、钾(K)、硫(S)、硼(B)、锌(Zn)的吸附能力进行了研究。4种水稻土对P的吸收能力大小顺序为:洪湖市油-稻两熟区近代河流冲积物母质发育的水稻土(4#土)>襄樊市麦-稻两熟区Q3母质发育的水稻土(3#土)>荆门油-稻两熟区Q3母质发育的水稻土(2#土)>蕲春县油-稻-稻三熟制区花岗片麻岩母质发育的水稻土(1#土);对K的吸收能力大小顺序为:3#>4#>1#>2#;对S的吸收能力大小顺序为:3#>2#>4#>1#;对Zn的吸收能力大小顺序为:3#>4#>2#>1#;对B的吸收能力大小顺序为:3#>4#>1#>2#。田间养分管理策略应根据不同地区土壤对养分的吸附能力大小进行相应调整。     

Effects of sediment load on the abrasion of soil aggregate and hydraulic parameters in experimental overland flow

The breakdown of soil aggregates under rainfall and their abrasion in overland flow are important processes in water erosion due to the production of more fine and transportable particles and, the subsequent significant effect on the erosion intensity. Currently, little is known about the effects of sediment load on the soil aggregate abrasion and the relationship of this abrasion with some related hydraulic parameters. Here, the potential effects of sediment load on soil aggregate abrasion and hydraulic parameters in overland flow were investigated through a series of experiments in a 3.8-m-long hydraulic flume at the slope gradients of 8.7 and 26.8%, unit flow discharges from 2×10~(–3) to 6×10~(–3) m~2 s~(-1), and the sediment concentration from 0 to 110 kg m~(–3). All the aggregates from Ultisols developed Quaternary red clay, Central China. The results indicated that discharge had the most significant(P0.01) effect on the aggregates abrasion with the contributions of 58.76 and 60.34%, followed by sediment feed rate, with contributions of 39.66 and 34.12% at the slope gradients of 8.7 and 26.8%, respectively. The abrasion degree of aggregates was found to increase as a power function of the sediment concentration. Meanwhile, the flow depth, friction factor, and shear stress increased as a power function along with the increase of sediment concentration at different slope gradients and discharges. Reynolds number was obviously affected by sediment concentration and it decreased as sediment concentration increased. The ratio of the residual weight to the initial weight of soil aggregates(Wr/Wi) was found to increase as the linear function with an increasing flow depth(P=0.008) or Reynolds number(P=0.002) in the sediment-laden flow. The Wr/Wi values followed a power function decrease with increasing friction factor or shear stress in the sediment-laden flow, indicating that friction factor is the best hydraulic parameter for prediction of soil aggregate abrasion under different sediment load conditions. The information regarding the soil aggregate abrasion under various sediment load conditions can facilitate soil process-based erosion modeling.     

基于InVEST模型的祁连山国家级自然保护区土壤保持现状与功能

运用InVEST模型,对甘肃祁连山自然保护区土壤保持现状与功能进行了定量评估,分析了不同土地利用、海拔高度、坡度以及土壤类型下的保土状况。结果表明:2015年甘肃祁连山自然保护区土壤侵蚀量与土壤保持量分别为1. 67×10^8t、4.21×10^8t。从侵蚀面积来看,保护区以微度和轻度侵蚀为主,占总面积的63.95%;虽草地的土壤保持能力弱于其他自然植被类型,但草地是土壤保持总量最高的土地利用类型;不同海拔梯度下的土壤保持总量随海拔增加呈现先增后减的趋势,保护区内海拔2 500~3 500 m的土壤保持功能最好;栗钙土的土壤保持量最高,黑毡土在草原土壤类型中土壤保持强度较低;坡度为15°~25°的区域土壤保持量最大,占土壤保持总量的31.93%;甘肃祁连山保护区生态系统减少泥沙淤积和减少土地废弃的价值分别为5. 76×10^8元和1. 44×10^8元,保护区内林草地保肥价值为9. 03×10^10元。     

玉米叶片表皮蜡质相关性状的全基因组关联分析

为发掘玉米叶片表皮蜡质合成与调控相关基因,以218份由温带、亚热带和热带自交系组成的关联群体为材料,在原阳对其3个生物学重复叶片表皮挂水能力进行调查,利用1.25 M覆盖玉米全基因组的SNPs进行Q、K和Q+K这3种模型下的全基因组关联分析。结果表明,Q模型较K模型和Q+K模型能更好地评价叶片表皮的挂水能力。Q模型下,共检测到88个覆盖玉米9条染色体的显著SNPs（P ≤ 2.04E-6）,88个SNPs分布于47个QTLs内,单个QTL可解释13.6%~45.6%的叶片挂水能力表型变异,47个QTL内共有97个候选基因,其中,77个具有功能注释。位于第2染色体上的转录因子NAC77（GRMZM2G018436）和第3条染色体上的亚油酸酯氧合酶（GRMZM2G156861）编码基因,是叶片表皮蜡质性状的重要候选基因。     

小冠开心形和细型主干形‘玉露香’梨光能截获与光合作用差异

小冠开心形和细型主干形是黄土高原梨树生产中的主要树形模式。为阐述这两种树形对冠层光能截获和叶片光合功能的影响,以山西芮城县4年生的‘玉露香’梨为试材,2017年和2018年连续两年测定了冠层截获的光合有效辐射PAR、叶片光合的光响应特性、荧光淬灭动力学特性以及光午休期间叶片的热耗散特性和光呼吸。结果表明：小冠开心形冠层不同方位和不同时刻截获的PAR均高于细型主干形,平均提高47.6%;与细型主干形相比,小冠开心形叶片光响应的最大净光合速率Pnmax,p与光饱和点LSP显著升高;光合碳同化过程的3个限制因子中,磷酸丙糖利用速率Vtpu对冠层光环境变化最敏感。正午强光胁迫下,小冠开心形叶片光呼吸速率Pr与总光合速率Pg的比例（Pr/Pg）比细型主干形叶片提高58.5%,NPQ中可恢复组分r(qE)提高了8.9%,而不可恢复组分r(qI)降低了75.0%。两种树形相比,小冠开心形梨树冠层可截获更多的光能,叶片的光合能力更强,强光胁迫时能够通过更高效的热耗散和光呼吸进行自我保护,可作为黄土高原产区梨树适宜树形。     

Evidence of sedimentation inequality along riparian areas colonised by Impatiens glandulifera (Himalayan balsam)

Soil loss from riparian areas supporting the annual invasive weed, Impatiens glandulifera (Himalayan balsam), was measured and compared with equivalent values recorded at nearby, topographically similar areas supporting perennial vegetation over a cumulative seven-year period, along sections of two separate river systems; one in Switzerland, and one in the UK. Soil loss from colonised locations was significantly greater than from reference locations in four of the seven measurement periods. Despite contrasting results, standard deviations, based on soil losses and gains, were predominantly higher for colonised areas at both rivers over most monitoring periods. These findings indicated that areas colonised by Himalayan balsam experience higher sediment flux in comparison with areas free of invasion. Here, we test those original interpretations by reinterrogating the datasets using a more robust analysis of inequality. Nine datasets were tested, five of which (i.e. 56%) showed that sediment flux was significantly greater at Himalayan balsam-invaded areas than at reference areas. Three datasets showed no difference in sediment flux between invaded and reference areas (33%), and one (11%) showed higher sediment flux at reference areas. Most results uphold our original interpretations and support our hypothesis that hydrochory probably dictates where colonisation initially occurs, by depositing Himalayan balsam seeds in slack or depressional areas along river margins. Once Himalayan balsam becomes established and sufficient perennial vegetation is displaced, seasonal die-off and depleted vegetation cover may increase the risk that some areas will experience significantly higher sediment flux.     

塔里木河上游棉区不同类型盐土阳离子交换量分布特征及影响因素

【目的】研究塔里木河上游棉区不同类型盐土CEC的分布状况及影响因素。 了解不同类型盐土土壤特性及肥力状况,为新疆南疆干旱区盐土改良利用提供理论依据。【方法】以阿拉尔绿洲草甸盐土(MeS)、沼泽盐土(MaS)、残余盐土(ReS)、洪积盐土(PrS)、棕漠林盐土(DeS)5种典型盐土为对象,研究该流域不同类型盐土阳离子交换量(CEC)的剖面分布规律,分析盐土CEC的影响因素,并利用灰色关联法对盐土CEC与土壤理化性质之间的关系进行了量化。【结果】该区盐土CEC在2.02～25.54 cmol/kg,平均值为12.39 cmol/kg,CEC随剖面深度的变化规律各类型盐土有所不同,不同类型盐土CEC大小依次为MeS> ReS > DeS > PrS > MaS。粘粒是干旱区盐土CEC的主要来源;pH、CaCO₃、盐基总量(TEB)和碱化度(BSP)与盐土CEC呈极显著正相关,是盐土CEC的主要影响因素,其中CaCO₃对盐土CEC的贡献不容忽视;盐土有机质(SOM)含量极低,对盐土CEC未表现出显著性影响;交换性钙饱和度(CaSP)、交换性镁饱和度(MgSP)及交换性钾饱和度(KSP)对盐土CEC有显著的抑制作用。【结论】塔里木河上游棉区不同类型盐土CEC有显著差异,不同类型盐土保肥、供肥及缓冲性能不同。pH、CaCO₃、TEB和ESP是CEC主要贡献因子,SOM对盐土CEC无显著的影响。