农牧交错区化肥减量施用对马铃薯产量、

马铃薯种植中超量和长期施用化肥已造成产量、品质和耐贮性下降,为了充分利用农牧交错区产生的有机肥,提高马铃薯产量、品质和耐贮性,实现马铃薯产业可持续发展,研究了化肥减量施用和增施有机肥对马铃薯产量、品质和耐贮性的影响。结果表明,化肥减量施用和增施有机肥提高了马铃薯品质和耐贮性。处理2（50%常规施肥量+4 m3有机肥）的产量、蛋白质、淀粉、干物质、可溶性糖和VC含量最高,较对照（CK）分别提高了1.67%、15.66%、13.58%、11.63%、31.91%和21.17%,贮藏期软腐病、干腐病、环腐病和晚疫病发病率较低,较对照（CK）分别降低了44.72%、45.61%、50.14%和39.39%。建议在农牧交错区采用处理2来提高马铃薯产量、品质和耐贮性,降低化肥用量和施肥成本。     

大兴安岭人工林有机质层释放溶解有机碳(DOC)动态特征

溶解有机碳(DOC)是土壤碳库中最活跃的部分。研究人工林生长中有机质层释放DOC的动态,对阐述北方森林碳循环具有基础意义。以空间代替时间方法,在内蒙古大兴安岭根河林业局管辖范围内选取不同林龄人工林为研究对象,收集并测定了有机质层渗透水中DOC浓度,并分析了坡位和不同月份对于有机质层释放DOC的影响。结果表明:不同阶段人工林,有机质层释放DOC浓度呈增加的趋势,且每个样地仅与50年生落叶松人工林阶段DOC有显著差异(P<0.05);在6-9月,有机质层渗透水中DOC浓度随月份变化,整体呈降低趋势,并随着人工林生长,有机质层渗透水中DOC浓度最大值转向7月;在不同坡位中,中、下坡位DOC浓度高于上坡位。随着不同阶段的人工林及坡位和季节的变化,有机质层下DOC浓度发生了一定的变化。     

西瓜嫁接砧木资源及其杂交组合枯萎病抗性鉴定

为了筛选西瓜枯萎病抗性砧木材料,对近年来收集整理的部分西瓜亲本材料及选配的砧木组合进行苗期枯萎病抗性人工接种鉴定。以国际上公认的5个西瓜枯萎病鉴别寄主材料(‘Black Diamond’‘Crimson Sweet’‘Charleston Gray’‘Calhoun Gray’‘PI296341-FR’)以及选配的49份西瓜砧木资源为试材,采用尖镰孢菌(Fusarium oxysporum f.sp.niveum)孢子悬浮液人工接种法,鉴定试验所用的西瓜枯萎病菌生理小种和砧木材料的枯萎病抗性。结果表明:鉴别寄主‘Black Diamond’‘Crimson Sweet’‘Charleston Gray’‘Calhoun Gray’‘PI296341-FR’的病情指数分别达85.2、53.0、27.2、19.2和7.8,抗性级别分别为感病、轻抗、中抗和抗病;49份西瓜砧木材料中,筛选出对Race 1表现抗病的材料有10份,占总供试材料的20.4%,中抗材料29份,占59.2%,轻抗材料10份,占20.4%,不存在免疫和完全感病的材料。确认该试验所用尖孢镰刀菌为生理小种1,筛选确定了高抗西瓜枯萎病的4份亲本材料588、893、BEH和FR328,6份杂交材料威砧101、Be-3×893、(BEH-15×Sugarlee)×893、(BEH1-15×Sugarlee)×341、(BEH1-15×AW2-1)×341和(BYH-1×Sugarlee)×893,可为设施西瓜生产提供优良的嫁接砧木资源。     

Variation in glomalin in soil profiles and its association with climatic conditions,shelterbelt characteristics,and soil properties in poplar shelterbelts of Northeast China

Glomalin-related soil protein(GRSP)sequesters large amounts of carbon and plays important roles in maintaining terrestrial soil ecosystem functions and ecological restoration;however,little is known about GRSP variation in 1-m soil profiles and its association with stand characteristics,soil properties,and climatic conditions,hindering GRSP-related degraded soil improvement and GRSP evaluation.In this study,we sampled soils from 1-m profiles from poplar(Populus spp.)shelterbelts in Northeast China.GRSP contents were 1.8–2.0 times higher in the upper 40 cm soil layers than at 40–100 cm.GRSP-related soil organic carbon(SOC)sequestration in deeper soil layers was*1.2 times higher than in surface layers.The amounts of GRSP-related nutrients were similar throughout the soil profile.A redundancy analysis showed that in both surface and deeper layers,soil properties(pH,electrical conductivity,water,SOC,and soil nutrients)explained the majority of the GRSP variation(59.5–84.2%);the second-most-important factor in GRSP regulation was climatic conditions(temperature,precipitation,and altitude),while specific shelterbelt characteristics had negligible effects(<5%).Soil depth and climate indirectly affected GRSP features via soil properties,as manifested by structural equation model analysis.Our findings demonstrate that GRSP is important for carbon storage in deep soils,regardless of shelterbelt characteristics.Future glomalin assessments should consider these vertical patterns and possible regulating mechanisms that are related to soil properties and climatic changes.     

木材及木基材料吸湿尺寸稳定性检测方法研究

为实现木材及木基材料吸湿尺寸稳定性横向比较,规范其检测方法,依据现有相关检测标准,借鉴日本工业木材吸湿尺寸稳定性检测方法,结合木质材料特性以及我国的具体情况,提出一种木材及木基材料吸湿尺寸稳定性的检测方法,即以温度20℃、相对湿度65%条件下的材料尺寸为基准,测定在温度40℃、相对湿度为75%和90%的两种吸湿环境条件下的材料尺寸变化。通过该方法对柚木、印茄木、朴木3种不同尺寸的木材和对多层材料、高密度纤维板、普通刨花板3种木基材料的吸湿尺寸稳定性进行测定,以评价该方法的适用性和可行性。结果表明:木材与木基材料试样不超过12 d即可达到吸湿平衡,不同材料尺寸变化率、湿胀系数的大小关系也与实际情况一致。因此木材与木基材料试样均适于用该方法。     

明胶骨原料碳、氮稳定同位素的地域性差异研究

为探讨不同地域来源的明胶骨原料中碳、氮稳定同位素的分布特征及其相关性,本试验采用元素分析-稳定同位素比率质谱仪测定了广西、内蒙古和山东3个主产区的牛骨样品及当地牧草饲料样品中的¹³C和¹⁵N同位素组成,并结合线性回归讨论了牛骨样品中δ¹³C和δ¹⁵N值的相关性与牛食谱组成的关系。结果表明,广西地区骨样品中δ¹³C和δ¹⁵N值的相关性较好(R²=0.401 8),而内蒙古和山东地区骨样品中δ¹³C和δ¹⁵N值的相关性较差(R²<0.1),反映了3地牛食物的来源稳定性及主要成分存在明显差异,对各地牛食谱结构推测的结果与实际牧草饲料样品中δ¹³C和δ¹⁵N值的地区分布规律也较为一致。本研究初步揭示了明胶骨原料中碳、氮稳定同位素产生地域性差异的原因,不仅为动物生态学研究提供了有益信息,更为动物制品产地溯源研究提供了新思路。     

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.     

典型喀斯特洼地植被恢复过程中土壤碳氮储量动态及其对极端内涝灾害的响应

西南喀斯特地区是我国主要的生态脆弱区之一,石漠化严重,旱涝灾害频发。植被恢复是提升脆弱生态系统土壤碳氮固持的有效方式,但该区不同植被恢复方式土壤碳氮动态监测的研究还很缺乏。本研究以典型喀斯特峰丛洼地为对象,选取人工林、牧草地、人工林+牧草地、撂荒地自然恢复4种最主要的植被恢复方式为研究对象,以耕地作为对照,对比分析退耕前(2004年)、退耕10年(2014年)和13年后(2017年)土壤碳氮储量动态变化特征。其中2004—2014年研究区未发生极端内涝灾害, 2014—2017年连续发生2次极端内涝灾害事件。研究结果表明,退耕10年后, 4种恢复方式下土壤有机碳(SOC)储量均显著增加,但退耕13年后,除撂荒地SOC持续增加外,其他3种恢复方式下SOC表现出下降趋势。植被恢复后土壤全氮(TN)储量提升相对缓慢,退耕10年仅牧草地显著增加,退耕13年后人工林+牧草和撂荒地TN增加,且撂荒地在退耕后呈持续增加趋势。相关性分析结果表明,土壤交换性Ca~(2+)与SOC、TN均呈显著正相关关系,且与2014年相比, 2017年不同植物恢复方式下土壤交换性Ca~(2+)均显著下降,这可能与研究区2015年和2016年连续内涝灾害有关。以上结果说明,不同恢复方式均能显著提升喀斯特地区土壤碳氮固持,并以自然恢复最佳,其生态系统能有效抵御极端气候灾害带来的负面影响。