黑河流域水化学空间分异特征分析

选取我国西北干旱区第 2大内陆河———黑河流域 ,对全流域地表水和地下水的水化学类型和水化学特征进行了系统分析。结果表明 ,黑河流域地表水中TDS (阴离子总量 )和主要离子含量沿流程均有不同程度的增加 ,但增幅不大。而地下水TDS从莺落峡出山后呈直线上升 ,下游TDS均大于 10 0 0mg/L ,主要离子含量增加明显 ,其变化特征与 TDS 基本一致 ;水化学成分和类型在空间上呈现出由上游向下游过渡变化的分带特征 :从上游山区、中游盆地到下游的尾闾盆地 ,河水的水化学特征依次为HCO3 -型、SO42 --HCO3 -型和Cl-型 ;山区和山前冲洪积扇中地下水为低矿化度的HCO3 -型水 ,中游盆地地下水矿化度升高 ,水化学类型为HCO3 -或HCO3 --SO42 -,下游盆地地下水矿化度进一步升高 ,水化学类型为Cl--SO42 -或Cl-;垂向变化上 ,由浅层到深层地下水矿化度降低 ,水化学类型变化不大 ,中游盆地主要为HCO3 -和HCO3 --SO42 -;下游盆地主要为Cl--SO42 -。     

晾晒和添加剂对白羊草青贮的影响

为探究含水量和添加剂对白羊草(Bothriochloa ischaemum)青贮的影响,以抽穗期新鲜的和晾晒的白羊草为原料,分别设计对照、添加甲酸(6 mL·kg^-1)或蔗糖(2%)处理,袋装密封青贮360 d后取样分析。结果表明:晾晒处理白羊草青贮饲料的pH较高,乳酸和氨态氮含量极显著下降(P<0.01);添加蔗糖或甲酸能够改善白羊草青贮饲料的发酵品质,甲酸或蔗糖均能够极显著降低白羊草青贮饲料的pH、乙酸和氨态氮含量(P<0.01),极显著提高乳酸含量(P<0.01);添加甲酸或蔗糖显著提高了白羊草青贮饲料的干物质保存率(P<0.05);青贮之后,硝酸盐含量下降。添加剂可改善白羊草青贮饲料的发酵品质,而白羊草晾晒后再进行添加剂青贮则效果更佳。     

4种结缕草光合特性及叶绿素含量的比较研究

以结缕草属4个不同种为试验材料,采用叶绿素测定仪以及光合测定仪,测定4种结缕草光合特征参数以及叶绿素含量。结果表明:(1)4种结缕草叶绿素含量由大到小依次为:日本结缕草,中华结缕草,沟叶结缕草,细叶结缕草;(2)日本结缕草和沟叶结缕草的光补偿点(LCP)为40μmol/(m2.s),接近于自然光照条件下阳性植物的光补偿点30μmol/(m2.s);(3)中华结缕草和细叶结缕草的LCP较高,为80μmol/(m2.s),光饱和点(LSP)都平均为1200μmol/(m2.s);(4)4种结缕草的表观量子效率(AQY)与自然光照条件下植物的AQY(0.03~0.06 mol/mol)一致,但是中华结缕草却显著高于其他3种,因此,可初步推断结缕草为阳性、且耐荫性较强的草坪草,并且中华结缕草以其优异的表现成为亚热带地区草坪草建坪中的最佳草种。     

基于Python的双过滤水肥一体机智能控制研究

为了满足不同生长时期植株水肥需求,基于基于Python的双过滤图像处理方法及环境监测技术,设计了可以自适应调节的水肥控制系统,主要包括氮肥含量控制和浇灌量控制.氮肥含量控制:首先,CCD摄头采集植株图像,应用Python的双过滤图像处理方法得到植株高度;其次,建立不同生长时期最高植株对应的氮肥浓度的曲线;再次,采用色度...     

Application of molybdenum fertilizer enhanced quality and production of alfalfa in northern China under non-irrigated conditions

Molybdenum (Mo) is an essential micro-mineral nutrient for plant growth and development. As an important legume forage, alfalfa (Medicago sativa) is frequently planted in marginal lands of northern China where water scarcity and infertile soil are limiting factors for alfalfa production. Mo plays an important role in nitrogen (N) metabolism in general and N fixation in legume species in particular. To evaluate the role of Mo fertilizer in alfalfa quality and production in semi-arid areas of northern China, we conducted a three-year field experiment in Inner Mongolia from 2012 to 2014. Mo fertilizer at the doses of 0, 150 g hm^?2, 300 g hm^?2yr^?1 was applied consecutively across the three years. Application of Mo at 300 g hm^?2yr^?1 significantly increased dry yield of alfalfa in 2014. Crude protein (CP) content of alfalfa without application of Mo exhibited a decline trend from 2012 to 2014. Application of Mo significantly enhanced total CP in 2012 and 2014, and delayed the reduction in total CP across the three years. In contrast to CP, Mo fertilizer had no significant effects on neutral detergent fiber and acid detergent fiber content. In addition, we found that nitrate reductase activity of alfalfa was increased by Mo fertilizer, which may account for the enhanced CP content in alfalfa. These findings highlight that application of Mo fertilizer can be an effective way to improve alfalfa production and quality in semi-arid areas in northern China.     

Interaction Between Plant Roots and Soil Water Flow in Response to Preferential Flow Paths in Northern China

Preferential flow is expected to provide preferential channels for plant root growth and variations in soil water flow, but few studies were conducted to imply the impacts of these changes, particularly for preferential flow in stony soils. This study aimed to characterize soil water flow and plant root distribution in response to preferential flow paths and quantitatively describe the relation between plant root distribution and soil water flow. Field dye‐tracing experiments centered on experimental plants were conducted to determine the root length density and soil water flow process. Laboratory analyses were performed to characterize changes in the relative concentration of the accumulated effluent and the degree of interaction between plant roots and soil water flow. The amount of fine plant roots with preferential flow paths decreased with increasing soil depth for all experimental plots. The largest plant roots were recorded in the upper soil layers to a depth of 20 cm. The relative concentration of the accumulated effluent increased with time and decreased with soil depth under saturated soil conditions, whereas a distinct early turning point for the relative concentration of the accumulated effluent was observed in the 0–20‐cm soil columns, and the relative concentration of the accumulated effluent initially decreased and then increased with time under unsaturated soil conditions. This study provides quantitative information with which to characterize the interaction between plant roots and soil water flow in response to preferential flow paths in soil–plant–water systems. Copyright © 2016 John Wiley & Sons, Ltd.     

基于HYDRUS-1D的不同质地土壤入渗过程数值模拟

基于HYDRUS-1D软件,对不同土质(淤泥、粉砂壤土、砂质粘壤土)的灌溉方案进行了系统的数值实验,模拟灌溉结束时及灌溉结束24 h之后的土壤剖面含水量和土壤湿润锋的变化情况。结果表明:在不产生径流的情况下,灌溉结束24 h后土壤的含水量分布和湿润深度只与土壤种类和灌溉量有关,与灌溉速度无关;对透水性较好的土质,灌溉水分重分布明显,以粉砂壤土灌溉速率0.7 cm·h~(-1)和灌溉时间3 h为例,灌溉结束时和灌溉24 h后土壤湿润深度分别为9.2 cm和20.6 cm,有55.3%的灌溉水参加了水分重分布;土壤湿润深度与灌溉量之间存在线性关系,拟合直线的斜率介于5.15(淤泥)和5.95(砂质黏壤土)之间。     

毛乌素沙地不同水分梯度根系垂直分布与土壤水分关系的研究

通过对毛乌素沙地不同水分梯度根系垂直分布的研究表明:不同水分梯度根系分布随土壤深度的增加呈指数形式下降,不同梯度由于土壤水分、植被根系类型的差异,不同水分梯度植被根系的空间分布也有差异,不同梯度根量随土壤垂直深度的模拟方程分别为:y=9.5736e-0.1341x,R2=0.8859(I);y=16.246e-0.2037x,R2=0.9301(II);y=32.001e-0.1904x,R2=0.9544(III);y=28.336e-0.1993x,R2=0.9484(IV)。不同水分梯度土壤含水率变化程度不同,同一水分梯度各层土壤含水率变化幅度亦有差异,0.1m土壤含水率变异系数最大,随着土壤深度增加变异系数减小,根据土壤含水率变异系数分析我们将各层土壤水分垂直变化划分为活跃层(0-0.1m)、次活跃层(0.2-0.6m)、相对稳定层(1m)(I、II、III);而对IV梯度划为活跃层(0-0.1m、1m)、相对稳定层(0.3m)。根系生物量垂直分布与其对应土壤含水率有明显相反的关系,土壤含水率的变化与根系生物量的变化趋于相反,当土壤含水率增大时相应区域根系生物量减小;反之则增加。随水分梯度的增加各梯度最高水分利用层逐渐向表层发展,从第I梯度0.4m的6.84到第IV梯度0.1m的14.33。     

含水量和装载量对松木片吸附溴甲烷的影响

在18℃、RH为60%～70%室内恒温条件下,对不同含水率和不同装载量的松木片的熏蒸结果表明:松木片含水量对溴甲烷熏蒸处理效果影响明显。在18℃、8g/m3处理24h,松材线虫死亡率(y)与碎木片含水量(x)之间关系式为:y=129.654-1.062x(R=0.967);碎木片对溴甲烷的吸附随水分含量升高而增加,58%、55%、49%含水率的碎木片对溴甲烷的吸附与含水率为30%、37%碎木片的吸附差异显著。载量对溴甲烷熏蒸处理松木片中松材线虫影响显著,松材线虫死亡率(y)与松木片载量(x)之间关系式为:y=105.809-0.247x(R=0.973);随实验碎木片载量的增加,对溴甲烷的吸附量也加大。     

Influence of salinity and moisture on the threshold shear velocity of saline sand in the Qarhan Desert,Qaidam Basin of China: A wind tunnel experiment

Determination of the threshold shear velocity is essential for predicting sand transport, dust release and desertification. In this study, a wind tunnel experiment was conducted to evaluate the influence of salinity and moisture on the threshold shear velocity of saline sand. Saline sand samples (mean particle size of 164.50-186.08 μm and the total silt, clay and salt content of 0.80%-8.25%) were collected from three saline sand dunes (one barchan dune and two linear dunes) in the Qarhan Desert, Qaidam Basin of China. Original saline sand samples were placed in two experimental trays for wet and dry processing to simulate deliquescence and desiccation, respectively. Surface moisture content ranging from 0.30% to 1.90% was generated by the steam method so that the saline sand can absorb water in a saturated water vapor environment. The motion of sand particles was determined by the observers with a solid laser. The laser sheet (0.80 cm thick), which was emitted by the solid laser, horizontally covered the sand surface and was bound to the sand. Results show that the cohesion of saline sand results from a combination of salt and water. The threshold shear velocity increases exponentially with the increase in crust thickness for the linear sand dunes. There is a positive linear correlation between the original moisture content and relative threshold shear velocity. The threshold shear velocity of dewatered sand is greater than that of wet sand with the same original moisture content. Our results will provide valuable information about the sand transport of highly saline soil in the desert.