湖北省土壤各级颗粒的磁化率

本试验对湖北省六种土壤五个粒级(>1,1-0.5,0.5-0.25,0.25-0.15.0.15-0.1mm)的磁化率进行了测定。结果表明:红壤、棕红壤、潮土和黄棕壤表土层磁化率大于母质层磁化率,而紫色土和黄褐土表土层磁化率小于下部土层的磁化率。棕红壤表土层磁化率小于淀积层磁化率。红壤、棕红壤、黄棕壤和黄褐土母质层磁化率随颗粒变细而明显增加,但这一现象在潮土、紫色土的母质层确不明显。0.25-0.15mm粒级是黄棕壤、红壤、棕红壤、潮土、紫色土磁化率随颗料大小变化的一个转折点。     

畜禽后裔测定组的最佳值

本文在考虑后裔测定总费用受限或者遗传进展一定时,探讨了几种情况下的公畜(禽)后裔组的最佳值。应用本文所给公式,即可求得实际测定中能使遗传进展最大或使经济费用最小时后裔组的最佳值。     

植物叶发育分子遗传机制的研究进展

植物的叶发育是由复杂的调控网络相互作用而进行调控的。植物叶发育的基本过程可以分为叶原基的起始发育、叶片极性的建立、叶片大小以及叶形的调控,本文主要从以上4个过程对叶发育分子遗传机制进行了阐述。     

D形截面螺旋输送机输送颗粒物料的实验研究

在可控转速的情况下运输粉末或者颗粒等松散物料时,因其机构简单,螺旋输送机被广泛应用于林业、农业等多种背景下的短距离提升或水平运输物料。为此,采用实验方法,针对改进后的D形截面筒的输送机进行输送颗粒物料的研究,结果表明:输送的质量流速率随着输送转速的增加而增加,随输送角度的增大而降低。另外,螺距和颗粒物料的粒径也对质量流速率有影响:大螺距的输送质量流速率较大,且随着输送倾斜角度的增大,螺距对质量流速率的影响减小;大颗粒的质量流速率大于小颗粒,且随着输送倾斜角度增加差距增大。     

基于自压滴灌工程过滤装置尺寸的确定及应用

由于新疆牧业灌区无电供应,水源无法过滤,实现滴灌工程难,目前采用地面灌溉。地形坡度大、灌水量多、大量水土流失。灌区下游排水不畅,洼地沼泽化面积剧增,地下水位上升导致土壤盐碱化,弃田面积逐渐扩大、种植面积萎缩。为了解决上述问题,充分利用地形落差,研制了自压滴灌工程过滤装置。同时渠道进水流量、调水池的调节流量、集水桶流量及系统流量之间建立了平衡关系。用实例说明不同地形落差与自压滴灌工程系统流量及过滤装置尺寸的计算过程。解决了自压滴灌工程水源的过滤、排沙、冲沙及自行冲洗等问题。为无电牧业灌区实现节水灌溉技术提供依据。     

办公建筑中空调形式对室内外PM2.5浓度相关性的影响

室外PM2.5可通过新风及围护结构缝隙渗透至室内,室外PM2.5较高时尤为明显,结果导致室内空气中的PM2.5浓度上升。为了研究空调形式对室内外PM2.5浓度相关性的影响,在2015年夏季对重庆某办公建筑中采用不同空调形式的室内外PM2.5浓度进行了实测。实测结果发现：集中式空调、分体式空调和非空调房间室内外PM2.5浓度比变化范围分别为0.59～0.76、0.47～0.76、0.71～0.91。室内外PM2.5浓度相关性系数的排序为：集中式空调环境（0.94）> 非空调环境（0.92）> 分体式空调环境（0.77）,研究结果表明,办公建筑的空调形式,对室内外PM2.5浓度的相关性有影响。     

Effect of soil pore size distribution on plant-available water and least limiting water range as soil physical quality indicators

Soil pore size distribution(SPSD) is one of the most important soil physical properties. This research investigated the relationships of location and shape parameters of the SPSD curves with plant-available water(PAW) and least limiting water range(LLWR) of the light-textured soils at the Torogh Agricultural Research Station in north-eastern Iran. Soil moisture release curve(SMRC), PAW and LLWR in matric heads of 100 and 330 h Pa for the field capacity and location and shape parameters of the SPSD curves of 30 soils with different texture and organic carbon contents were determined, and the variable relationships were statistically analyzed. The results showed that the median equivalent pore diameter(de), mean de, standard deviation(SD*), and skewness of the SPSD curves were significantly correlated with PAW(PAW330) and LLWR(LLWR330) measured in a matric head of 330 h Pa. Decrease in deand increase in the diversity of soil pore size(SD*) increased PAW330 and LLWR330. The SD* values of all the soil samples were lower than the optimal ranges suggested in literature. Neither PAW nor LLWR values were significantly different in the soils with the optimal modal deand those with non-optimal modal de. Optimal values of median and mean equivalent pore diameters and kurtosis of SPSD curves led to a significant improvement of PAW330 and LLWR330 as soil physical quality indicators. It was recommended to revise the optimal ranges for SD* and modal defor future studies.     

Intensive organic vegetable production increases soil organic carbon but with a lower carbon conversion efficiency than integrated management

Intensive vegetable production in greenhouses has rapidly expanded in China since the 1990s and increased to 1.3 million ha of farmland by 2016, which is the highest in the world. We conducted an 11‐year greenhouse vegetable production experiment from 2002 to 2013 to observe soil organic carbon (SOC) dynamics under three management systems, i.e., conventional (CON), integrated (ING), and intensive organic (ORG) farming. Soil samples (0–20 and 20–40 cm depth) were collected in 2002 and 2013 and separated into four particle‐size fractions, i.e., coarse sand (> 250 µm), fine sand (250–53 µm), silt (53–2 µm), and clay (< 2 µm). The SOC contents and δ¹³C values of the whole soil and the four particle‐size fractions were analyzed. After 11 years of vegetable farming, ORG and ING significantly increased SOC stocks (0–20 cm) by 4008 ± 36.6 and 2880 ± 365 kg C ha^?1 y^?1, respectively, 8.1‐ and 5.8‐times that of CON (494 ± 42.6 kg C ha^?1 y^?1). The SOC stock increase in ORG at 20–40 cm depth was 245 ± 66.4 kg C ha^?1 y^?1, significantly higher than in ING (66 ± 13.4 kg C ha^?1 y^?1) and CON (109 ± 44.8 kg C ha^?1 y^?1). Analyses of ¹³C revealed a significant increase in newly produced SOC in both soil layers in ORG. However, the carbon conversion efficiency (CE: increased organic carbon in soil divided by organic carbon input) was lower in ORG (14.4%–21.7%) than in ING (18.2%–27.4%). Among the four particle‐sizes in the 0–20 cm layer, the silt fraction exhibited the largest proportion of increase in SOC content (57.8% and 55.4% of the SOC increase in ORG and ING, respectively). A similar trend was detected in the 20–40 cm soil layer. Over all, intensive organic (ORG) vegetable production increases soil organic carbon but with a lower carbon conversion efficiency than integrated (ING) management.     

土壤颗粒分布体积分形维数与数量分形维数之间的关系

土壤的体积颗粒分布(PSD)可用于同时确定数量分形维数(DN)和体积分形维数(DV)。以往的试验和理论研究均未直接比较DV和DN的关系。为建立DV和DN的关系并分析其参数的敏感程度,在中国各地取了12种不同质地土壤,利用激光粒度仪进行了测定。提出了含3个参数Rupper(颗粒半径的上限),Ri(第i个半径)和Rlower(半径下限)的DV-DN理论关系,该关系可说明为什么DN可能大于3。在未调整的幂定律范围内(PLR),DV的幂定律半径为38.6～85.8μm,DN的幂定律半径为53.2～358μm,估算的DV值(2.18～2.69)比DN值(2.38～3.19)小。调整后的PLR比未调整的窄。在调整的PLRs范围内,估算的DV值变化范围为2.11～2.56,而DN变化范围为2.28～3.02。调整和未调整PLRs得出的DV和DN的差异说明,Rupper,Rlower,Ri和Rlower/Rupper均可能影响DV与DN关系,有必要进行参数的敏感性分析。进行敏感性分析可基于敏感系数(C)来鉴别DV-DN关系中各参数改变所引起的DV和DN相对变化,从而找出对该关系影响最大的参数。就不同情况下计算的C值而言,Rupper是影响DN值的最重要参数,小的Rupper值可能导致估算DN的准确度降低。PLR范围越大,DN的估算越准确。根据DV估算DN的相对误差的绝对值在12%范围内,说明得出的DV-DN理论关系是正确的。