宽垄沟灌覆膜条件下土壤水分运移初探

宽垄沟灌作为一种大田作物栽培灌水方式已逐步受到关注.为研究灌水前后水分在垄沟间的运移及再分布,本试验在大棚内模拟宽垄沟灌垄上覆膜栽培条件以及灌水方案,采用中子仪进行水分观测.试验数据显示,在本试验条件下,垄背剖面的两个观测点表层,灌水前其含水量仅为田间持水量的65%和66%,灌水后垄沟水分的侧向入渗,144 h(6 d)分别达到田间持水量的73%和80%,408 h(17 d)达到田间持水量的78%和79%.试验结果表明,在宽垄沟灌覆膜条件下,水平向及垄背垂直向含水量梯度的存在导致水分侧向及向垄背的补给明显,且在覆膜条件下,垄背蒸散发损失少,起到减少土壤水分无效损耗、高效利用之效果.     

空间电场阴极聚水机理及初步试验研究

为了解决干旱地区缺水问题,采用施加正向空间电场的方法,使悬浮在气体中的雾粒荷电在静电力的作用下定向移动,迅速地积聚到作为阴极的土壤表面,同时也抑制了土壤水分蒸发,从而实现了空间电场的阴极聚水.为此,设计了一种电极电压、异极距和间歇工作节拍可调的空间电场聚水试验系统,研究了空间电场对土壤含水率的影响规律.初步试验结果表明,在气候条件比较干旱的情况下,在正向空间电场中的土壤水分蒸发明显要比在大气电场中的慢,说明了适宜的正向空间电场可以抑制土壤水的蒸发.     

棉花营养钵机械化制作技术的研究

阐述了机械化制作的棉花营养钵适于机械化育苗移栽又不影响棉苗生长发育的要求,对影响机械化制钵强度的因素营养土中纤维与土的质量比、含水量和营养钵的压缩比进行了分析研究.结果表明:当土与纤维的质量比为1.8～2.3,含水量为18%～23%、压缩比为1.8～2.2时,压制的钵体强度可达到适合机械化育苗、移栽要求又不影响棉苗生长的钵体强度300～450N,所需静压制力为1000～1500N.     

西瓜可溶性固形物含量近红外透射检测技术

设计的近红外透射式西瓜可溶性固形物含量（SSC）检测系统主要包括光纤光谱仪、光纤透射附件、数据采集卡以及自制光源。对50个麒麟瓜SSC进行了预测试验，采用主成分回归和偏最小二乘回归法分别建立了样品的原始光谱、一阶微分光谱、二阶微分光谱和SSC的预测模型，结果表明偏最小二乘回归法建立的模型具有较高的相关性，相关系数为0．951，均方根校正误差0．347，均方根预测误差0．302，样本真实值与预测值的相关系数为0．910。     

水、氮效应与叶绿素关系试验研究

以冬小麦和夏玉米为试验对象，研究了不同水、氮条件对作物植株含氮及叶绿素含量的影响，作物叶片含氮、作物产量与叶绿素含量之间的量化关系，并提出了利用叶绿素仪预测作物氮素胁迫的方法。研究结果表明，田间的不同水、氮制度将影响作物的含氮水平及叶绿素含量，它们之间呈正响应关系。氮素对作物叶绿素含量起着较强的影响作用。作为一种测量叶片叶绿素含量的仪器，叶绿素仪可以作为测量作物含氮的仪器使用，具有快速、准确、简便的特点。     

施用沼肥对保护地蔬菜栽培土壤理化性质的影响

本文以等有机质含量的猪粪、沼渣为基肥，追肥（化肥与沼液）以等N、等P、等K进行施用，采用二裂式区组设计的方法，研究了沼肥、猪粪、化肥等不同施肥组合对保护地土壤pH值及土壤速效养分含量的影响。结果表明：番茄收获期，各处理土壤pH有下降的趋势，但没有酸化现象发生；施用沼渣在防止土壤pH值下降方面有较好的作用；施用沼渣、沼液在提高土壤有机质含量方面的效果分别优于施用猪粪、化肥，沼渣与沼液配合施用在提高土壤有机质及碱解N含量方面效果显著，猪粪与化肥配合施用有利于提高土壤速效P和速效K的含量。     

“上膜下秸”措施对温室土壤水热盐调控试验研究

为了明确温室生产中不同耕作措施的水热盐调控效果,采用温室小区试验方法,以翻耕(CK)、翻耕结合地表覆盖地膜(M)、翻耕结合秸秆深埋(J)为对照,研究了翻耕结合地表覆盖地膜结合秸秆深埋(J+M)措施对温室土壤水热盐动态变化的影响。结果表明,与M、J及CK处理相比,J+M处理全生育期平均土壤含水率可分别提高8.96%、5.45%、14.32%,土壤温度分别提高3.35%、5.21%及8.32%,土壤全盐量分别降低24.44%、19.65%、26.64%,这一结果可为宁夏温室种植实施地膜覆盖与秸秆深埋改良措施提供参考。     

Effect of water deficit in different growth stages on stem sap flux of greenhouse grown pear-jujube tree

The effects of water deficit in different fruit growth stages on the variation of stem sap flux of 6-year old greenhouse-grown pear-jujube trees were investigated. Treatments included sufficient water supply during the whole fruit-growing period (T₁), mild water deficit during the flowering–fruit setting stage (T₂), moderate water deficit during the fruit rapid growth stage (T₃) and severe water deficit during the fruit maturing stage (T₄). Results showed that significant compensation effect on stem sap flux after re-watering was observed in T₂, but not in T₃ and T₄ stages. At the end of rapid growth stage, the diurnal variation of stomatal conductance generally had a similar trend as that of stem sap flux, but with a distinct midday depression from 12:00 to 14:00 p.m. In addition, a linear relationship between the relative available soil water content (RAWC) and the ratio of daily stem sap flux to that of sufficient water treatment was observed (R² = 0.4489).     

Effect of drying on soil strength and corn emergence

Summary Laboratory studies were conducted to evaluate the effects of drying on soil strength and corn emergence (Zea mays L.). Corn was germinated in Billings silty clay under a bank of heat lamps which operated 9, 14, 19, or 24 h per day. Soil strength (modules of rupture), soil moisture content and emergence were measured daily.The relationship of soil strength to corn seedling emergence as influenced by the four light and heat durations and bare and mulched soil surfaces was determined. As soil strength increased emergence decreased until it ceased at soil strengths of about 80 kPa. Strength of this soil had a high negative correlation with soil water content and increased with time. Mulching decreased initial rate of drying, decreased crust strength, and improved corn emergence. The 14-hour light and heat treatment resulted in the highest corn emergence.Contribution from Colorado State Experiment Station, USDA-ARS Snake River Conservation Research Center, and USDA-ARS Fort Collins, respectively     

保护地蔬菜栽培不同灌水方法对表层土壤盐分含量的影响

通过 3年连续保护地栽培蔬菜小区试验 ,对滴灌、渗灌、沟灌 3种灌水方法的土壤盐分积累状况进行了比较研究。试验后 0～ 2 0 cm土层土壤全盐含量以沟灌最高 ,渗灌次之 ,滴灌最低 ;滴灌土壤 p H下降幅度明显低于渗灌和沟灌土壤。在 0～ 2 0 cm土层内全盐含量呈幂指数形式分布 ,即地表处含量最高 ,随深度增加逐渐下降 ;而土壤 p H则随深度增加而直线上升。另外 ,土壤中可溶性盐的阴离以 NO-3 为主 ,阳离子以 Ca2 + 为主。这说明选择合理灌水方法 ,是防止土壤退化、提高保护地作物产量和质量的有效途径。