不同含水率对谷子籽粒压缩力学性质与摩擦特性的影响

为了探明不同含水率谷子籽粒的物理机械性质,减少谷子籽粒在播种、碾米加工及储运等过程中受到压缩载荷及摩擦而产生的机械损伤,该文针对不同含水率的谷子籽粒进行压缩力学性质与摩擦特性试验。研究了谷子籽粒的挤压破碎过程,获得不同含水率谷子籽粒的力-位移（变形）曲线,破坏力、变形量及破坏能。随着含水率升高,破坏力减小,变形量和破坏能呈现先降低后升高的变化规律。同时采用赫兹接触理论,得到谷子籽粒单向表观弹性模量和许用挤压应力,结果表明二者都随含水率升高线性降低。分别测定了谷子籽粒与钢板和铝板间的滑动摩擦系数,随含水率升高,谷子与该2种材料的摩擦系数均增大,且与铝板的摩擦系数要高于钢板。根据试验结果,分别拟合得到了压缩和摩擦力学性能指标与谷子含水率的关系方程,为谷子播种、仓储、加工等装备设计及参数优化提供了基础依据。     

土壤水分及环境因子对刺楸叶片气体交换的影响

通过测定不同土壤水分条件下,3a生盆栽刺楸苗木的气体交换参数及其周围环境因子,探讨土壤水分及微气候因子对光合速率、蒸腾速率、气孔导度等气体交换参数的影响规律。结果表明:随着水分胁迫的加剧,刺楸叶片蒸腾速率、净光合速率和气孔导度总体上表现出减小的趋势,且随着胁迫的加剧,下降的幅度越大,蒸腾速率、净光合速率和气孔导度在重度、中度、轻度胁迫下日均值分别比对照下降6 6 % ,2 5 %和16 % ,81% ,30 %及5 1% ,70 % ,17%和14 %。随着土壤水分的减少,净光合速率下降逐渐由气孔限制转变为非气孔限制,水分利用效率并未完全表现出下降的趋势,日平均值表现为对照>中度>轻度>重度。逐步回归分析表明,刺楸苗木叶片水气交换参数,不仅受土壤水分的影响,同时也受外界环境因子的综合影响,且影响程度差异较大,回归方程相关系数较好     

玉米抗旱性鉴定指标的研究

研究指出抗旱系数及脯氨酸含量、叶水势、丙二醛含量、相对电导率、蒸腾速率、叶面积和叶形态变化等指标均可作为玉米抗旱性鉴定指标的良好参数 ,并以抗旱系数为主要参数计算了各生理生化指标的相关系数 ,用以衡量这些指标在玉米抗旱性鉴定及综合评价的重要性。     

供磷水平对不同磷效率玉米氮、钾素吸收和分配的影响

在砂培条件下,以磷高效利用型玉米(KH5)和磷低效利用型玉米(西502)为材料,研究了低磷(Pi25μmol/L,LP)和正常供磷(Pi2mmol/L,NP)2个供磷水平对其氮、钾素吸收和分配的影响。结果表明,磷高效利用型玉米氮钾素吸收和干物质积累受低磷处理的影响较小,表现出对氮、钾的高效吸收。正常供磷水平下,磷低效利用型玉米氮、钾素吸收量和干物质积累量显著高于磷高效利用型,但其氮、钾吸收和干物质生产能力远低于后者。低磷处理使玉米干物质和氮钾营养向根系分配的比例增加,磷低效利用型玉米这种趋势更为明显,反映其耐低磷能力较弱。     

施用钾肥对叶菜产量和品质的影响

Over a period of two years, field experiments were conducted on four silty loam soils grown with foliar vegetable crops including Chinese cabbage (Brassica pekinensis Rupr., cv.Lu-Bai 3), autumn greens (B. chinensis L., cv.Piao-Geng-Bai), winter greens (B. var.rosularis Tsen et Lee, cv.You-Dong-Er), and summer greens (B. chinensis L., cv.Zao-Shu 5), respectively. Each experiment included one CK treatment without K, N and P fertilizers applied, and four treatments with from low to high doses, 0~300 kg hm^-2 for Chinese cabbage, 0~150 kg hm^-2 for autumn and winter greens and 0~180 kg hm^-2 for summer greens, of K fertilizers in the form of sulfate of potash (SOP) applied together with N and P fertilizers. One treatment of K fertilizer in the form of muriate of potash (MOP) applied at high levels (150 or 180 kg hm^-2) together with N and P fertilizers was included in the experiments of autumn, winter and summer greens, respectively, in order to compare the effects of SOP and MOP. The market yields of the tested crops increased significantly with the increasing rate of K application. The crops supplied with K fertilizers yielded more stably as the CV% of their yields decreased with the rate of K application. K fertilization increased not only K contents but also the amounts of N, P and K absorbed in shoots of autumn, winter and summer greens, which were statistically significantly correlated to their yields. It can also be found that potassium improved the quality of the foliar vegetable crops as their dry mater contents were generally increased and Vc contents obviously increased and nitrate contents markedly decreased. As compared to MOP, SOP was more effective on the yields and quality of autumn, winter and summer greens at the high levels of fertilization.     

绿洲-荒漠交错带不同沙丘土壤水分时空动态变化规律

绿洲-漠交错带是植被恢复的一个重要区域，而植被恢复的关键又是了解沙丘土壤水分的变化规律。从2003年10月到2004年10月，对甘肃省张掖绿洲-荒漠交错带沙丘土壤水分进行了连续观测，并研究了生态垫在沙漠治理中的应用。结果表明：土壤水分时空动态变化主要受降雨、植被以及地表覆盖等因素的影响，沙丘土壤水分月变化滞后于降水变化。沙丘剖面土壤水分变异系数随土层深度的增加而减小，铺设生态垫减小了沙丘土壤水分的空间变异（CV=4．43％），流动沙丘0～40cm的含水量（0．19％～1.27％）低于固定沙丘（1.61％～1．75％），而其它各层的含水量（1．52％～1．73％）都高于固定沙丘（1．11％～1．38％）；流动沙丘含水量（1．27％～1．73％）从上部到下部依次升高，而固定沙丘（1．75％～1．11％）则与此相反；利用标准差和变异系数对沙丘土壤水分垂直变化进行分层，得出了土壤水分剖面分别为速变层、活跃层和次活跃层，并运用相关分析方法分析了生态垫覆盖下沙丘各层间土壤含水量及其与沙丘剖面平均含水量的关系。研究初步认为，生态垫能有效地保持沙丘土壤水分，将为沙漠治理提供一种新型的治沙模式。     

ESP值和黏粒含量对土壤表面封闭作用的影响

降雨导致土壤表面结皮形成封闭是自然现象，它能降低土壤入渗，增加土表径流，导致土壤侵蚀。该文系统地研究了不同性质土壤表面的封闭作用过程，分别确定封闭过程中的物理机械作用和化学作用。试验采用了具有不同土壤交换性钠百分率(ESP)值(2、5、10、20)和黏粒含量(10％、20％、40％、60％)的4种土壤进行降雨模拟试验，通过土壤表面播撒磷石膏(PG)(2000 kg/hm²)和PG与聚丙烯酰胺(PAM)(PG 2000 kg/hm²+PAM 20 kg/hm²)混合物的处理，分别抑制了土壤的化学封闭和物理封闭，论述了ESP值和黏粒含量对土壤化学封闭和物理封闭作用的影响，结果表明：在高ESP值土壤中，化学封闭作用占土壤封闭的主导作用；低ESP值土壤中，土壤的物理封闭作用增大。当黏粒含量较低时，土壤物理封闭作用较低；当黏粒含量较大时，土壤物理封闭作用显著增大。     

Development of on-line measurement system of bulk density based on on-line measured draught, depth and soil moisture content

On-line measurement of soil compaction is needed for site specific tillage management. The soil bulk density (ρ) indicating soil compaction was measured on-line by means of a developed compaction sensor system that comprised several sensors for on-line measurement of the draught (D) of a soil cutting tool (subsoiler), the soil cutting depth (d) and the soil moisture content (w). The subsoiler D was measured with a single shear beam load cell, whereas d was measured with a wheel gauge that consisted of a swinging arm metal wheel and a linear variable differential transducer (LVDT). The soil w was measured with a near infrared fibre-type spectrophotometer sensor. These on-line three measured parameters were used to calculate ρ, by utilising a hybrid numerical–statistical mathematical model developed in a previous study. Punctual kriging was performed using the variogram estimation and spatial prediction with error (VESPER) 1.6 software to develop the field maps of ρ, soil w, subsoiler d and D, based on 10 m × 10 m grid. To verify the on-line measured ρ map, this map was compared with the map measured by the conventional core sampling method.

The spherical semivariogram models, providing the best fit for all properties was used for kriging of different maps. Maps developed showed that no clear correlation could be detected between different parameters measured and subsoiler D. However, the D value was smaller at shallow penetration d, whereas large D coincided with large ρ values at few positions in the field. Maps of ρ measured with the core sampling and on-line methods were similar, with correlation coefficient (r) and the standard error values of 0.75 and 0.054 Mg m⁻³, respectively. On-line measured ρ exhibited larger errors at very dry zones. The normal distribution of the ρ error between the two different measurement methods showed that about 72% of the errors were less than 0.05 Mg m⁻³ in absolute values. However, the overall mean error of on-line measured ρ was of a small value of 2.3%, which ensures the method accuracy for on-line measurement of ρ. Measurement under very dry conditions should be minimised, because it can lead to a relatively large error, and hence, compacted zones at dry zones cannot be detected correctly.     

不同有机材料覆盖对土壤保水效果的影响

[目的]研究不同有机材料覆盖对土壤水分蒸发量、土壤含水量的影响,并筛选出保水效果最佳的材料。[方法]以木片、树皮及经过堆腐的园林废弃物为研究对象,进行模拟蒸发及桶装控制试验。[结果]不同粒径的园林废弃物覆盖均能降低土壤水分日蒸发量,日蒸发量从大到小依次为CK,3～5 cm粒径(M_3)、0～1 cm粒径(M_1)、1～3 cm粒径(M_2)。在连续蒸发14 d后,M_2,M_1,M_3和CK的土壤水分累积蒸发量分别为193.0,269.5,304.0和1 037.0 g,与CK相比,分别减少了81.4%,74.0%,70.7%;不同有机材料覆盖均能提高土壤含水量。除了雨季之外,不同土层土壤含水量从高到低依次表现为:木片覆盖(M_4)树皮覆盖(M_5)1～3 cm粒径园林废弃物覆盖(M_2)CK。土壤含水量的年变化整体呈现出双峰趋势,一年中4—5月含水量较低,6—8月含水量较高,不同土层土壤含水量的年变化趋势基本一致。M_4,M_5,M_2和CK的0—40 cm土层土壤年平均含水量分别为32.9%,30.3%,27.4%,26.8%。[结论]木片为保水效果最好的有机材料,其次是树皮和园林废弃物。     

钴对冬小麦生理生化性状和产量影响的初步研究

在潮土上采用大田小区进行了钴元素肥效试验。试验结果如下:施用适量的钴可以显著提高旗叶的叶绿素含量、硝酸还原酶活性以及小麦的根系活力;各施钴处理较对照增产7 4%～20 3%,施钴量在0 75kg/hm2以内,随着施钴量的增加,增产效应提高,当施钴量超过0 75kg/hm2时,随着施钴量的增加,冬小麦的产量增加,但增产效应下降。经回归分析,小麦产量与施钴量呈抛物线型,回归方程为y=-1263 9x2 2083 4x 4371 7,相关系数r=0 8910,达到5%显著水平。