油棕叶梗重组方材制备工艺

以油棕叶梗为原材料、酚醛树脂为胶黏剂，采用正交试验方法研究重组方材密度、施胶量、热压时间和热压温度对油棕叶梗重组方材力学性能的影响。结果表明，密度对油棕叶梗重组方材性能的影响较大，密度和施胶量越大，重组方材力学性能越好；热压温度和热压时间对油棕叶梗重组方材性能的影响比较复杂。综合考虑确定油棕叶梗重组方材的较优制备工艺条件为:密度0.7 g/cm³，施胶量12%，热压温度180℃，热压时间40 min；较优工艺条件下油棕叶梗重组方材的弹性模量为7 185 MPa，静曲强度为68.7 MPa，顺纹抗压强度为35 MPa，内结合强度为0.21 MPa。密度为0.7 g/cm³的油棕叶梗重组方材的弹性模量、静曲强度、顺纹抗压强度高于了杉木的性能。     

Biocrusts resist runoff erosion through direct physical protection and indirect modification of soil properties

Purpose

Biological soil crusts (biocrusts) are ubiquitous in arid and semi-arid regions and play many critical roles in soil stabilization and erosion prevention, greatly decreasing soil loss. Although sediments may be completely controlled by well-developed biocrusts, runoff loss is observed. Consequently, it is important to study how biocrusts resist runoff erosion in different developmental stages to evaluate and manage water erosion.

Materials and methods

In the Loess Plateau Region, we sampled 32 biocrust plots representing eight stages of biocrust development and 5 slope cropland soil plots as bare soil control plots. We then used a rectangular open channel hydraulic flume to test the effects of biocrust development on runoff erosion.

Results and discussion

As expected, the establishment of biocrusts enhanced soil stability, and accordingly, soil anti-scourability significantly increased with biocrust development. Biocrusts exhibiting more than 36% or 1.22 g dm^?2 of moss coverage or biomass fully protected the soil from runoff erosion. Moreover, soil properties, such as soil organic matter, soil cohesion and soil bulk density, were also important in reducing erosion. The findings indicated that biocrusts inhibited runoff erosion through direct physical protection related to biocrust cover and biomass and through the indirect modification of soil properties. In the early biocrust development stage (when moss cover was less than 36%), cyanobacterial biocrust played a primary role in providing resistance to runoff erosion, with resistance being positively related to cyanobacterial biomass (chlorophyll a) and influenced by soil properties.

Conclusions

The relationship between soil anti-scourability and moss coverage or biomass can be divided into two stages based on a moss cover or biomass threshold. The capacity of biocrusts to resist runoff erosion was limited when moss cover was below the threshold value. Therefore, the stage corresponding to this level of moss cover should be of concern when estimating, predicting and managing water erosion.

     

黄河未来输沙量态势及其适用性对策

[目的] 探索黄河输沙预测的新思路，预估黄河未来输沙态势与输沙量水平，为黄河流域生态治理规划提供参考。[方法] 结合黄河流域水土保持生态修复现状，采用单累积曲线法、滑动平均及频率分析方法，分析1950—2019年黄河主要来沙区间的实测输沙量变化特征及其未来态势。[结果] 1950—2019年黄河输沙量呈现阶梯式减少。1950—2019年黄河中游各站累积实测输沙量随时间的变化可用“左半抛物线”表征。黄河输沙量自1997年以来已进入相对稳定态势，目前已达企稳状态；黄河潼关站未来年输沙量在90%频率下为1.00×10⁸ t左右，在10%频率下为5.00×10⁸ t左右，未来多年平均输沙量为1.40×10⁸ t。[结论] 为了维持黄河输沙量低稳状态，提升水土保持措施质量与标准，补齐“后水土保持”短板，构建完善的水沙关系调控体系，维持黄河下游河道冲淤平衡，是黄河流域生态保护与高质量发展的保障。     

2种紫花苜蓿耐盐生理特性的初步研究

为研究2种紫花苜蓿(Medicagosativa L.)“阿迪娜”(耐盐基因型)和“秘鲁”(敏盐基因型)在盐胁迫处理下的生理特性与耐盐机理,采用150mmol/LNaCl胁迫处理2种紫花苜蓿幼苗,分别测定盐处理前和处理后2,4,6,8,16h的过氧化氢酶(CAT)、过氧化物酶(POD)、丙二醛(MDA)、脯氨酸(PRO)、相对含水量(RWC)和叶绿素(Chl)含量。结果表明:2种紫花苜蓿的过氧化氢酶活性、过氧化物酶活性和丙二醛含量在盐胁迫下总体呈上升趋势,脯氨酸含量和相对含水量表现出相反的趋势。叶绿素含量在盐胁迫前期稳定不变,但在胁迫后期显著性下降;2种紫花苜蓿的相对含水量和叶绿素含量的变化趋势与植株表型变化相对应。主成分分析表明,过氧化氢酶和丙二醛的贡献率最大,能更好地为苜蓿耐盐机理及分子育种研究提供理论依据。     

微喷带单孔水量分布影响因素试验研究

为了探究微喷带管径、喷孔结构、工作压力以及喷射角度对单孔水量分布影响,以常用的机械打孔的Ф28,Ф32,Ф40和Ф50这4种微喷带为研究对象,通过调节微喷带的喷射角度和工作压力,研究微喷带正常运行时单孔喷水(其他孔进行遮挡,不混入测试单孔的水流中)特性,测定了不同工作压力条件下射程、湿润面积、干燥区宽度等参数.结果表明:喷水射程随喷射角度先增大再减小,射程最大值为30°~ 40°,随工作压力的增大而增大;湿润区宽度与喷射角度、工作压力均存在正相关的关系;射程与干燥区宽度随喷射角度的变化规律相同;湿润区面积的最大值出现在喷射角度为50°时.在实际运行中,建议微喷带喷射角度为30°~50°,并应根据干燥区与射程合理布置相邻微喷带的铺设间距.     

河朔荛花根中抑菌活性成分研究

在活性追踪指导下，采用多种分离技术从河朔荛花根甲醇提取物中分离得到12个化合物，经核磁共振波谱、质谱等技术并结合相关文献确定其结构分别为1-己酸-2,3-硬脂酸甘油三酯( 1 )、β-谷甾醇( 2 )、月桂醇( 3 )、顺-十八碳-9-烯酸( 4 )、(2E)-庚基-3-(3, 4-二羟基苯基)丙烯酸酯( 5 )、(–)-pluviatolide( 6 )、1β-hydroxy-10β-H-guaia-4,11-dien-3-one( 7 )、异狼毒素( 8 )、新狼毒素B( 9 )、瑞香酚( 10 )、单棕榈酸甘油酯( 11 )和(+)-去甲络石甙元( 12 )。其中，化合物 3 、 4 和 6 ~ 12 均为首次从河朔荛花中分离得到。抑菌活性测定结果表明:异狼毒素( 8 )和新狼毒素B( 9 )对马铃薯晚疫病菌Phytophthora infestans菌丝生长和孢子萌发均表现出明显的抑制作用，其中对菌丝生长的EC₅₀值分别为68.4 μg/mL和44.9 μg/mL，对孢子萌发的EC₅₀值分别为25.1 μg/mL和14.0 μg/mL。     

土壤温度对作物根区环境及玉米根冠生长的调控研究进展

土壤温度对作物的生长发育具有很强的调控作用。在全球气候变化背景下,根区土壤温度对玉米生长的影响及其调控机制已成为当前研究的一个热点。结合目前农业生产中土壤低温和高温对玉米造成危害的现状,从土壤温度对作物根区土壤环境以及玉米根系生长、冠层发育与产量形成的影响方面,综述土壤温度对玉米生长发育调控作用的研究进展,介绍改变土壤温度的措施以及对玉米土壤温度研究的发展方向进行展望,为今后的研究提供参考。     

12份美国玉米自交系配合力评价

以12份引进美国解禁玉米自交系为供试材料,4份课题组骨干玉米自交系(KA105、KA064、KB043和KB204)为测验种,采用NC-II遗传交配设计,进行配合力测定与分析。结果表明,测验种KA105和KA064产量一般配合力(GCA)效应表现优良,供试美国玉米自交系中PHPR5、MBST、LH213、2FACC、LH212Ht、LH209和PHR47产量GCA效应表现优良。杂交组合PHPR5×KA105、LH213×KA105、PHH93×KA105、2FACC×KA064、LH212Ht×KA105、PHPR5×KB204产量的超标优势较强,可进一步试验。     

Influences of sand cover on erosion processes of loess slopes based on rainfall simulation experiments

Aeolian-fluvial interplay erosion regions are subject to intense soil erosion and are of particular concern in loess areas of northwestern China.Understanding the composition,distribution,and transport processes of eroded sediments in these regions is of considerable scientific significance for controlling soil erosion.In this study,based on laboratory rainfall simulation experiments,we analyzed rainfall-induced erosion processes on sand-covered loess slopes(SS)with different sand cover patterns(including length and thickness)and uncovered loess slopes(LS)to investigate the influences of sand cover on erosion processes of loess slopes in case regions of aeolian-fluvial erosion.The grain-size curves of eroded sediments were fitted using the Weibull function.Compositions of eroded sediments under different sand cover patterns and rainfall intensities were analyzed to explore sediment transport modes of SS.The influences of sand cover amount and pattern on erosion processes of loess slopes were also discussed.The results show that sand cover on loess slopes influences the proportion of loess erosion and that the compositions of eroded sediments vary between SS and LS.Sand cover on loess slopes transforms silt erosion into sand erosion by reducing splash erosion and changing the rainfall-induced erosion processes.The percentage of eroded sand from SS in the early stage of runoff and sediment generation is always higher than that in the late stage.Sand cover on loess slopes aggravates loess erosion,not only by adding sand as additional eroded sediments but also by increasing the amount of eroded loess,compared with the loess slopes without sand cover.The influence of sand cover pattern on runoff yield and the amount of eroded sediments is larger than that of sand cover amount.Furthermore,given the same sand cover pattern,a thicker sand cover could increase sand erosion while a thinner sand cover could aggravate loess erosion.This difference explains the existence of intense erosion on slopes that are thinly covered with sand in regions where aeolian erosion and fluvial erosion interact.