连续模拟降雨下岩溶区含砾石堆积体坡面径流产沙特征

为明确砾石含量对岩溶区石灰土质堆积体坡面径流产沙特征的影响,以土质坡面为对照,采用室内模拟降雨试验方法,研究了递增型降雨(0.5,1.0,2.0,2.5,3.0 mm/min)条件下偏土质(砾石含量30%)和偏石质(砾石含量70%)石灰土坡面的径流特性及侵蚀特征。结果表明:(1)随雨强增大,各坡面径流率呈稳定增长—波动的变化趋势,且土质坡面径流率整体小于2种含砾石坡面;偏土质、偏石质坡面累计产流量较土质坡面增加了0.49,0.37倍;(2)1.0~3.0 mm/min雨强下,土质坡面侵蚀速率在0.16~5.4 g/(m^2·s)范围内波动,整体呈稳定—波动增加的变化趋势;偏土质和偏石质坡面分别为0.16~5.4,0.06~0.74 g/(m^2·s),前者侵蚀速率变化范围大且波动剧烈,后者变化范围小且稳定;随砾石含量的增加,各坡面累计侵蚀量呈先增后减的变化趋势,偏土质坡面侵蚀量较土质坡面增加2.5倍,偏石质坡面较其减少了0.9倍;(3)土质、偏土质和偏石质坡面的侵蚀速率与径流率分别呈极显著正相关幂函数、线性函数和线性函数关系。研究结果可为桂西北岩溶区弃渣场水土流失治理提供一定的科学依据。     

黄河口生态恢复工程对湿地土壤不同形态无机硫动态变化的影响

选择黄河口生态恢复前后的未恢复区（R₀）、2007年恢复区（R₂₀₀₇）和2002年恢复区（R₂₀₀₂）的芦苇湿地为研究对象，探讨了生态恢复工程对生长季湿地土壤无机硫形态变化的影响。结果表明，生态恢复工程不同程度地改变了湿地土壤中各形态无机硫含量。相对于R₀，R₂₀₀₂和R₂₀₀₇土壤中的水溶性硫（H₂O—S）含量分别降低46.7%和44.7%，吸附性硫（Adsorbed—S）和盐酸可溶性硫（HCl—Soluble—S）含量分别增加0.4%，116.0%和50.1%，29.1%，而盐酸挥发性硫（HCl—Volatile—S）含量在R₂₀₀₂下降8.0%，在R₂₀₀₇增加19.7%。不同恢复阶段湿地土壤中各形态无机硫含量在生长季呈不同的变化特征，这一方面与不同湿地植物生长节律以及地上与地下之间的硫养分供给关系密切相关；另一方面则与不同生态补水方式导致的环境因子，尤其是pH、EC和氮养分的变化有关。随着恢复年限的增加，湿地土壤的总无机硫（TIS）含量以及其占全硫（TS）含量的比例均呈降低趋势。湿地土壤的TIS储量整体随恢复年限的增加而降低，而这种降低主要取决于H₂O—S、Adsorbed—S和HCl—Soluble—S的贡献，且以H₂O—S占优（78%~80%）。研究发现，随着黄河口湿地的逐渐恢复以及每年冬季芦苇收割活动的进行，恢复湿地土壤中的无机硫养分逐渐趋于缺乏状态，长期来看将不利于维持湿地的稳定与健康。     

Early interspecific dynamics,dry matter production and nitrogen use in Kernza (Thinopyrum intermedium) – alfalfa (Medicago sativa L.) mixed intercropping

ABSTRACT

The global interest in growing perennial grain crops such as intermediate wheatgrass (Thinopyrum intermedium) (Kernza) for production of food and feed is increasing. Intercropping Kernza with legumes may be a sustainable way of supplying nitrogen to soil and associated intercrop. We determined the competitive interactions between intercropped Kernza (K) and alfalfa (Medicago sativa L.) (A) under three inorganic nitrogen (N) rates N0, N1, N2 (0, 200, 400 kg ha^?1) and five species relative frequencies (SRF) (100%K:0%A, 75%K:25%A, 50%K:50%A, 25%K:75%A and 0% K:100%A) in mixed intercrops (MI) in a greenhouse pot experiment. After 11 weeks of growth. Kernza dry matter yield (DM) and N accumulated (NACC) were low, but alfalfa DM and NACC high at 0 kg N ha^?1. 200 and 400 kg N ha^?1 fertiliser application increased the competitive ability (CA) of Kernza and reduced the CA of alfalfa. SRF had large impacts on alfalfa DM, NACC and NFIX only at 0 kg N ha^?1 fertiliser, and insignificant impacts on Kernza at all N fertiliser levels, indicating that adjustment of SRF may not be an effective way to modulate the interspecific competition of Kernza. Further research on the other factors that influence the interspecific competition are warranted.     

镉和模拟酸雨胁迫对苦楝幼苗镉含量及叶片抗氧化系统的影响

为探讨苦楝在重金属Cd和酸雨的单一及复合胁迫下的生理响应特征,采用人工配置土壤盆栽试验,研究不同浓度Cd(0、30、60、90、120、150、180 mg·kg^-1)和3个梯度模拟酸雨(pH值5.6、4.5、3.5)单一及复合处理对苦楝幼苗生物量、Cd含量及叶片保护性酶[超氧化物歧化酶(SOD)、过氧化物酶(POD)和过氧化氢酶(CAT)]活性和抗坏血酸-谷胱甘肽循环(AsA-GSH)的影响。结果表明,除低浓度Cd(≤30 mg·kg^-1)单一及其与pH值4.5酸雨复合处理对幼苗地上部、地下部生物量有促进作用外,其他处理均表现出抑制作用,其中复合处理对苦楝幼苗的抑制作用更明显,表现为叠加效应;单一Cd处理时,随着Cd浓度的增加,幼苗根、茎、叶中Cd含量逐渐升高,且根系大于茎叶,复合处理抑制了植物对Cd的积累,对叶片的抑制作用最强;Cd和酸雨单一及复合处理下叶片SOD、CAT和POD活性均有所增加,分别在60 mg·kg^-1 Cd、pH值5.6,60 mg·kg^-1 Cd、pH值4.5和90 mg·kg^-1Cd、pH值4.5时出现阈值;在AsA-GSH循环中,单一Cd处理下,AsA、GSH含量和抗坏血酸过氧化物酶(APX)、谷胱甘肽还原酶(GR)活性均随着Cd浓度的增加呈先上升后下降的趋势,单一酸雨处理对上述4个指标的影响不尽一致,而复合处理下上述指标在Cd浓度≤60 mg·kg^-1、pH值≥4.5时均能保持较高值,且随着胁迫程度的加深均出现了阈值。综上所述,苦楝对重金属Cd和酸雨胁迫具有一定的耐性,可在Cd浓度≤60 mg·kg^-1和pH值≥4.5的酸雨双重污染区域正常生长。本研究结果为土壤Cd污染的酸雨区域的修复植物筛选提供了理论基础和参考依据。     

Specific ion effect of H+ on variably charged soil colloid aggregation

Specific ion effects (Hofmeister effects) have recently attracted the attention of soil scientists, and it has been found that ionic non-classic polarization plays an important role in the specific ion effect in soil. However, this explanation cannot be applied to H⁺. The aim of this work was to characterize the specific ion effect of H⁺ on variably charged soil (yellow soil) colloid aggregation. The total average aggregation (TAA) rate, critical coagulation concentration (CCC), activation energy, and zeta potential were used to characterize and compare the specific ion effects of H⁺, K⁺, and Na⁺. Results showed that strong specific ion effects of H⁺, K⁺, and Na⁺ existed in variably charged soil colloid aggregation. The TAA rate, CCC, and activation energy were sensitive to H⁺, and the addition of a small amount of H⁺ changed the TAA rate, CCC, and activation energy markedly. The zeta potential results indicated that the specific ion effects of H⁺, K⁺, and Na⁺ on soil colloid aggregation were caused by the specific ion effects of H⁺, K⁺, and Na⁺ on the soil electric field strength. In addition, the origin of the specific ion effect for H⁺ was its chemical adsorption onto surfaces, while those for alkali cations were non-classic polarization. This study indicated that H⁺, which occurs naturally in variably charged soils, will dominate variably charged soil colloid aggregation.     

氨基酸配合硼喷施对油麦菜硼营养及生长、品质的影响

为探究有机营养类物质氨基酸与硼酸配合喷施对油麦菜生长的应用效果,本研究采用盆栽试验,设置单独喷施1%硼酸处理,以及谷氨酸、丙氨酸和天冬氨酸3种氨基酸各设3个喷施浓度(5、10、20 mmol·L^-1) 与1%硼酸配合喷施处理,并以喷施清水为对照(CK),共11个处理,收获后测定植株的生长指标和硼含量。结果表明,单独喷施硼酸对油麦菜生物量无明显影响,低浓度氨基酸与硼配合喷施均能显著提高油麦菜生物量,其中丙氨酸-硼喷施处理油麦菜生物量较CK平均增加了9.4%。与CK相比,3种氨基酸与硼配合喷施均能明显提高油麦菜叶片总蛋白含量,同时降低硝酸盐积累,从而改善品质。与单独喷施硼酸相比,适宜浓度氨基酸与硼配合喷施均可显著提高油麦菜氮、钾积累量,另外谷氨酸-硼和天冬氨酸-硼喷施对油麦菜磷积累量也有明显促进作用。与单独喷施硼酸相比,氨基酸与硼配合喷施均可显著提高油麦菜地上部硼含量,其中丙氨酸-硼喷施处理油麦菜地上部硼含量平均增幅为41.0%;此外,丙氨酸-硼喷施对油麦菜地下部硼含量也有明显提升作用,平均增幅为15.6%;喷施丙氨酸浓度与油麦菜地上部和地下部硼含量均呈显著正相关关系。综合比较不同氨基酸与硼酸配合喷施对油麦菜的影响,可考虑将丙氨酸作为增效剂与硼肥配合施用,提高硼肥的应用效应。本研究为开发新型硼肥提供了理论依据。     

陇薯系列高淀粉马铃薯品种的淀粉产量及品质性状综合评价

为了评价高淀粉马铃薯品种的综合品质性状,本研究以甘肃省农业科学院育成的15个马铃薯品种(系)为参试材料,2011-2018年连续8年定点田间试验,测定了块茎产量、营养品质(干物质、淀粉、维生素C、粗蛋白)含量和矿物质元素(钾、钙、铁、锌)含量。结果表明,参试材料的块茎产量和营养品质含量均存在显著的基因型、环境及基因型与环境的互作效应,其中块茎产量、淀粉产量、干物质含量、淀粉含量性状的基因型效应大于环境效应,而营养品质中的维生素C、粗蛋白和还原糖含量的环境效应大于基因型效应。参试材料的块茎产量24 549~50 140 kg·hm^-2,淀粉产量4 271~9 298 kg·hm^-2,干物质含量21.07%~30.18%,淀粉含量14.63%~21.83%,维生素C含量12.20~18.95 mg·100g^-1,粗蛋白含量2.17%~2.71%,还原糖含量0.18%~0.43%,钾含量4 316~5 368 mg·kg^-1,钙含量85.10~138.40 mg·kg^-1,铁含量10.17~24.50 mg·kg^-1,锌含量2.45~3.80 mg·kg^-1。大西洋的衍生品种陇薯8号、陇薯9号、陇薯12号、陇薯14号、L0527-2、L08104-12、LZ111和L1149-2淀粉含量均超过18%,其中,L1149-2总体表现优异,其平均块茎产量50 140 kg·hm^-2、淀粉产量9 298 kg·hm^-2、干物质含量26.75%、淀粉含量19.30%、维生素C含量14.62 mg·100g^-1、粗蛋白含量2.52%、还原糖含量0.28%、钾含量5 297 mg·kg^-1、钙含量138.40 mg·kg^-1、铁含量20.40 mg·kg^-1、锌含量3.20 mg·kg^-1;而陇薯5号淀粉产量及营养品质较差。本研究为合理利用陇薯系列高淀粉马铃薯品种提供了科学依据,对改良高淀粉马铃薯品种产量和品质具有指导意义。     

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。     

Whole wheat bread: Effect of bran fractions on dough and end-product quality

Consumption of whole-wheat based products is encouraged due to their important nutritional elements that benefit human health. However, the use of whole-wheat flour is limited because of the poor processing and end-product quality. Bran was postulated as the major problem in whole wheat breadmaking. In this study, four major bran components including lipids, extractable phenolics (EP), hydrolysable phenolics (HP), and fiber were evaluated for their specific functionality in flour, dough and bread baking. The experiment was done by reconstitution approach using the 2⁴ factorial experimental layout. Fiber was identified as a main component to have highly significant (P < 0.05) and negative influence on most breadmaking characteristics. Although HP had positive effect on farinograph stability, it was identified as another main factor that negatively impacted the oven spring and bread loaf volume. Bran oil and EP seemed to be detrimental to most breadmaking characteristics. Overall, statistical analysis indicates that influence of the four bran components are highly complex. The bran components demonstrate multi-way interactions in regards to their influence on dough and bread-making characteristics. Particularly, Fiber appeared to have a high degree of interaction with other bran components and notably influenced the functionality of those components in whole wheat bread-making.     

Time‐lapse monitoring of soil water content using electromagnetic conductivity imaging

The volumetric soil water content (θ) is fundamental to agriculture because its spatiotemporal variation in soil affects the growth of plants. Unfortunately, the universally accepted thermogravimetric method for estimating volumetric soil water content is very labour intensive and time‐consuming for use in field‐scale monitoring. Electromagnetic (EM) induction instruments have proven to be useful in mapping the spatiotemporal variation of θ. However, depth‐specific variation in θ, which is important for irrigation management, has been little explored. The objective of this study was to develop a relationship between θ and estimates of true electrical conductivity (σ) and to use this relationship to develop time‐lapse images of soil θ beneath a centre‐pivot irrigated alfalfa (Medicago sativa L.) crop in San Jacinto, California, USA. We first measured the bulk apparent electrical conductivity (EC_a – mS/m) using a DUALEM‐421 over a period of 12 days after an irrigation event (i.e. days 1, 2, 3, 4, 6, 8 and 12). We used EM4Soil to generate EM conductivity images (EMCIs). We used a physical model to estimate θ from σ, accounting for soil tortuosity and pore water salinity, with a cross‐validation RMSE of 0.04 cm³/cm³. Testing the scenario where no soil information is available, we used a three‐parameter exponential model to relate θ to σ and then to map θ along the transect on different days. The results allowed us to monitor the spatiotemporal variations of θ across the surveyed area, over the 12‐day period. In this regard, we were able to map the soil close to field capacity (0.27 cm³/cm³) and approaching permanent wilting point (0.03 cm³/cm³). The time‐lapse θ monitoring approach, developed using EMCI, has implications for soil and water use and management and will potentially allow farmers and consultants to identify inefficiencies in water application rates and use. It can also be used as a research tool to potentially assist precision irrigation practices and to test the efficacy of different methods of irrigation in terms of water delivery and efficiency in water use in near real time.