干旱胁迫下保水剂对苗木生长及生理的影响

在盆栽条件下,对不同保水剂处理的土壤吸持水特性以及云南拟单性木兰和绒叶含笑苗的水分生理、生长状况进行试验研究。结果表明,随着保水剂用量的增加,土壤保水能力和供水能力增加,苗木在有限水分条件下生存期延长3-91 d,地径、树高、新增叶片分别增加了16.7％-461.2％,22.7％-368.2％,42.9％-372.7％;随着保水剂用量增加,土壤容重下降了6.2％-35.1％,总孔隙度和毛管孔隙度明显增加了3.6％-20.3％和5.9％-22.6％;在有限水分条件下,通过不同保水剂处理能减少水分的胁迫,净光合速率增长8.9％-461.2％,蒸腾速率增长了22.2％-518.7％,气孔导度增长了4.2％-512.5％。     

意大利瓦勒拉尼整地系统与常规开沟犁整地效益对比分析

通过意大利瓦勒拉尼整地系统（由火车型犁和海豚型犁2种犁型构成,其中火车型犁近似水平沟式整地,海豚型犁近似大鱼鳞坑式整地）与常规开沟犁整地效益的对比试验,结果显示：同期覆土层（0～20 cm）的土壤含水量以瓦勒拉尼系统2种整地方式最高,是常规开沟犁整地的1.28倍和1.11倍。火车型犁整地的土壤容重为1.05 g/cm3,常规开沟犁整地为1.08 g/cm3,火车型犁整地后的土壤容重最小。瓦勒拉尼系统的火车型犁整地后的土壤毛管最大持水量是56.12%,远高于未整地的48.44%和普通犁整地的52.12%,分别是后两者的1.16倍和1.08倍。火车型犁整地后文冠果的地径达1.00 cm,是普通犁整地后地径0.42 cm的2.38倍;树高为0.93 m,是普通犁整地后树高0.53 m的1.75倍;保存率由59.30%提高至91.43%,提高了32.13个百分点;海豚型犁整地文冠果4年保存率则提高了13.42个百分点。     

泥炭覆土搅拌时间对覆土结构及双孢蘑菇产量和质量的影响

为优化双孢蘑菇(Agaricus bisporus)覆土技术,以泥炭为覆土材料,研究泥炭覆土搅拌时间对覆土物理结构以及对双孢蘑菇产量和质量的影响。结果证实,随搅拌时间的延长,泥炭覆土充气孔隙度降低,容重增加。充气孔隙度与双孢蘑菇产量高度正相关,但是与双孢蘑菇子实体大小及商品菇率高度负相关;覆土容重与双孢蘑菇产量高度负相关,但是与双孢蘑菇子实体大小及商品菇率高度正相关。搅拌时间较短的覆土(5~20 min),双孢蘑菇总产量较高,且每潮菇产量更均匀,更有利于工厂化生产。搅拌时间较长的覆土(40~120 min),双孢蘑菇子实体较大,但是会降低双孢蘑菇的总产量以及影响每潮菇产量的均匀性。本试验条件下泥炭覆土最适搅拌时间为10 min,双孢蘑菇3潮菇总产量34.5 kg/m~2,商品菇产量27 kg/m~2。研究初步揭示覆土物理结构对双孢蘑菇产量及质量的影响,为优化覆土技术及筛选优质覆土材料提供参考。     

利用盘式吸渗仪确定土壤水力学参数研究进展

各种农业措施显著影响土壤的物理性质,特别是土壤水力学参数。随着计算机模型广泛用于土壤物质迁移的预测预报,准确确定土壤水力学参数成为一项重要的研究任务。盘式吸渗仪作为一种简便实用的仪器正被广泛用于田间土壤水力学参数的测定。国内外学者研究了稳态、瞬态和反推等方法,利用盘式吸渗仪来确定土壤近饱和导水率、吸渗率和水分特征曲线。同时该仪器可以用于田间测定土壤孔隙分布状况,以及两区模型中的参数。笔者对国内外有关盘式吸渗仪研究从相关理论和应用方面进展进行了综述,并对田间测定操作中注意的问题进行评述,指导田间试验以获得准确的测定数据。盘式吸渗仪在田间测定土壤孔隙,特别是大孔隙流方面有独特的优点,但是其并未在中国不同质地土壤上得以广泛应用。     

基于图像处理的疏透度测定及结构关系研究

为快速、准确地测定防风林林带疏透度，建立林带疏透度与林带结构因子间的关系模型，为防风林建设及调整提供合理化意见。使用图像处理技术对获取的防风林林带照片进行自动识别，通过Otsu算法自动将树木实体区域和孔隙区域分割，从而测定林带疏透度。并采用相关性分析和逐步线性回归法建立疏透度与林带结构因子间的关系模型。结果表明，采用Otsu算法测定林带疏透度的方法与图像处理软件(Photoshop)测定结果无明显差异，该方法操作简单、效率高，能够快速、准确测定防风林林带疏透度。防风林疏透度与林带行数、棵数、枝下比例、株行距、密度存在显著性相关关系，构建疏透度与林带行数、密度间的关系模型:β=-0.060 1N-0.065 8ρ+0.810 9(R²=0.961 3,P=0.000 29)。根据建立的防风林林带疏透度与林带结构因子间的关系模型，可对防风林的建设提供科学合理化的指导，使其发挥更好的防护效应。     

积雪特性参数分析及雪深模型建立

通过2015~2016年冬季积雪观测试验,测量自然条件下雪深、雪层温度、雪层密度、雪层液态含水率等积雪特性参数,分析积雪特性参数影响因子和发育变化规律,构建径向基神经网络雪深模型。结果表明,空气、地表温度及水汽压是影响雪参数发育三大主要气象因子。在时长为124 d覆雪期中,雪深最大平均融雪速率达3.20 mm·d-1,出现在融雪后期。雪层密度随雪深增加波浪式上升,其中稳定期全层密度0.1~0.4 g·cm-3;雪层液态含水率0.5%~3.5%,分层液态含水率中层较大,积雪表层和底部波动较小;全层积雪孔隙率平均值为72.3%,积底层孔隙率廓线下降最快,极差最大。经两次优化后,雪深模型最大绝对误差为0.614 1 cm,最大相对误差为5.85%,模拟精度控制在6 mm以内。     

浅谈孔隙率对沥青路面的影响

沥青混合料的孔隙率是一个重要的设计参数，其对于沥青路面的强度和使用性能有着重要的影响。在施工时，由于施工条件和设备的影响，不可能达到设计的孔隙率，于是一般要求用压实度作为施工时的一个控制指标，将沥青路面施工后的孔隙率控制在一个可接受的范围。在路面使用的初期，必然会有一段时间处于未完全压实工作状态，这种工作状态下，沥青路面能够提供的是未完全稳定的早期强度。在设计时，需要对比多个级配的混合料，确定合理的早期强度。     

Roles of Root Aerenchyma Development and Its Associated QTL in Dry Matter Production under Transient Moisture Stress in Rice

Abstract

Enhanced aerenchyma development in rice under transient drought-to-waterlogged (TD-W) stress promotes root system development by promoting lateral root production. This study analyzed the quantitative trait loci (QTLs) associated with the plasticity in aerenchyma development under TD-W stress. A mapping population of 60 F₂ genotypes of chromosome segment substituted lines (CSSL) derived from CSSL47 and Nipponbare crosses were grown in rootboxes and evaluated for shoot and root growth, and aerenchyma development (expressed as root porosity). The TD-W stress was imposed starting with water saturated soil condition at sowing and then to progressive drought from 0 to 21 days after sowing (DAS) prior to exposure to sudden waterlogging for another 17 days (21 to 38 DAS). We performed simple and composite interval mapping to identify QTLs for aerenchyma development. QTL associated with aerenchyma development was mapped on the short-arm of chromosome 12 and designated as qAER-12. The effect of qAER-12 on the plasticity in aerenchyma development under TD-W was significantly associated with the increase in lateral root elongation and branching. This resulted in greater root system development as expressed in total root length and consequently contributed to higher dry matter production. This qAER-12 is probably the first reported QTL associated with aerenchyma development in rice under TD-W and is a useful trait for the improvement of the adaptive capability under fluctuating soil moisture conditions.     

Hydraulic conductivity and porosity under conventional and no-tillage and the effect of three species of cover crop in northern France

We studied soil hydraulic conductivity (K) and porosity in five combinations of soil tillage and cover crop management systems. Treatments were winter wheat (Triticum aestivum L.) grown on a conventionally tilled soil (CT), on a no‐till soil (NT), and on an NT with three different cover crops: red fescue (Festuca rubra L.; Fr), bird's‐foot‐trefoil (Lotus corniculatus L.; Lc) and alfalfa (Medicago sativa L.; Ms). Measurements were made on a loamy soil in Grignon, France, in November 2004, May 2005 and October 2005. K and mean size of hydraulically active pores were measured in situ at three water potentials (?0.6, ?0.2 and ?0.05 kPa) at the soil surface and at 10 cm depth. In November 2004 and May 2005, pore space was described using 2D image analysis of pores on undisturbed soil samples in the 0–10 cm layer and in the 10–20 cm layer. The major differences were caused by soil tillage that created two heterogeneous soil layers and increased K in the 0–10 cm layer relative to NT. The effects of cover crop on K and porosity were not affected by the root type: there were no major differences between the grass cover crop (fibrous‐root type) and the leguminous ones (tap‐root type). However, we recorded larger functional pores and more tubules in the no‐till treatments with a cover crop, compared with the no‐till treatment without cover crop; this was probably the result of root activity. Although these changes generally did not result in larger values of K, they participated in the maintenance of soil structure and K over time.