不同水肥条件下夏玉米/冬小麦农田生态系统碳平衡研究

农田生态系统碳平衡取决于农作物固定碳量和土壤异养呼吸排放碳量。为揭示水肥用量对农田生态系统碳平衡的综合影响，设置3个灌水水平：高水、中水和低水（W1、W0.85、W0.7夏玉米季分别为90、76.5、63mm，冬小麦季分别为140、119、98mm），4个施氮水平：高氮、中氮、低氮和不施氮（N1、N0.85、N0.7、N0夏玉米季分别为300、255、210、0kg/hm2，冬小麦季分别为210、178.5、147、0kg/hm2），4个施磷水平：高磷、中磷、低磷和不施磷（P1、P0.85、P0.7和P0夏玉米季分别为90、76.5、63、0kg/hm2，冬小麦季分别为150、127.5、105、0kg/hm2）进行了田间试验。结果表明：不同水肥处理下夏玉米/冬小麦农田生态系统表现为碳汇，夏玉米季净生态系统生产力固碳量（CNEP）为6805~7233kg/hm2，冬小麦季CNEP为5842~6434kg/hm2，夏玉米CNEP高于冬小麦。在高、中、低肥水平下，增加灌水量，夏玉米/冬小麦周年净初级生产力固碳量（CNPP）提高2.48%~5.96%，土壤微生物异养呼吸碳释放量（CRm）增加2.15%~15.20%，净生态系统生产力固碳量（CNEP）增加1.16%~6.47%。在高、中、低供水水平下，增加施肥量，夏玉米/冬小麦周年CNPP增加2.95%~3.43%，土壤CRm增加5.23%~18.67%，CNEP增加0.93%~2.79%，CNEP增加比例与供水水平呈负相关。在低水条件下，氮磷肥配施处理夏玉米/冬小麦农田周年CNEP较单施氮、磷肥分别增加4.86%、7.34%，且氮磷肥交互作用显著（P<0.05），水肥供应水平相差15%时对冬小麦农田CNEP有显著的正交互作用。氮磷肥配施、水肥协调供应均有助于促进夏玉米/冬小麦农田生态系统的净碳输入，在节水节肥原则下，夏玉米和冬小麦分别在W0.85N0.85P0.85和W0.7N0.85P0.85水肥供应条件下有利于增加农田CNEP。     

Poorly crystalline iron and aluminium oxides contribute to the carbon saturation and sorption of dissolved organic carbon in the soil

Soil carbon (C) saturation implies an upper limit to a soil's capacity to store C depending on the contents of silt + clay and poorly crystalline Fe and Al oxides. We hypothesized that the poorly crystalline Fe and Al oxides in silt + clay fraction increased the C saturation and thus reduced the capacity of the soil to sorb additional C input. To test the hypothesis, we studied the sorption of dissolved organic carbon (DOC) on silt + clay fractions (<53 µm) of highly weathered oxic soils, collected from three different land uses (i.e., improved pasture, cropping and forest). Soils with high carbon saturation desorbed 38% more C than soils with low C saturation upon addition of DOC, whereas adsorption of DOC was only observed at higher concentration (>15 g kg^?1). While high Al oxide concentration significantly increased both the saturation and desorption of DOC, the high Fe oxide concentration significantly increased the desorption of DOC, supporting the proposition that both oxides have influence on the DOC sorption in soil. Our findings provide a new insight into the chemical control of stabilization and destabilization of DOC in soil.     

动物饲料国际贸易、养殖密度与环境氮磷平衡的关系

粮食和饲料的国际贸易促进了许多国家农业生产系统的专业化和集约化。专业化动物养殖越来越多地依赖进口大豆和玉米,虽然提高了动物生产力,但也促使作物和动物生产系统在空间上的分离。本文综述了几十年来全球范围内大豆和玉米的贸易变化,并将其与养殖密度和整个食品系统中营养平衡的变化联系起来。这一变化与不同的营养管理条例的差异和动物饲养密度的空间变化有关。深入解析这些变化有助于理解动物饲料国际贸易、养殖密度与氮磷平衡之间的复杂关系。     

Effect of farm management on topsoil organic carbon and aggregate stability in water: A case study from Southwest England,UK

There are few reliable data sets to inspire confidence in policymakers that soil organic carbon (SOC) can be measured on farms. We worked with farmers in the Tamar Valley region of southwest England to select sampling sites under similar conditions (soil type, aspect and slope) and management types. Topsoils (2–15 cm) were sampled in autumn 2015, and percentage soil organic matter (%SOM) was determined by loss on ignition and used to calculate %SOC. We also used the stability of macroaggregates in cold water (WSA) (‘soil slaking’) as a measure of ‘soil health’ and investigated its relationship with SOC in the clay‐rich soils. %SOM was significantly different between management types in the order woodland (11.1%) = permanent pasture (9.5%) > ley‐arable rotation (7.7%) = arable (7.3%). This related directly to SOC stocks that were larger in fields under permanent pasture and woodland compared with those under arable or ley‐arable rotation whether corrected for clay content (F = 8.500, p < .0001) or not (F = 8.516, p < .0001). WSA scores were strongly correlated with SOC content whether corrected for clay content (SOC_adj R² = .571, p < .0001) or not (SOC_unadj R² = 0.490, p = .002). Time since tillage controlled SOC stocks and WSA scores, accounting for 75.5% and 51.3% of the total variation, respectively. We conclude that (1) SOC can be reliably measured in farmed soils using accepted protocols and related to land management and (2) WSA scores can be rapidly measured in clay soils and related to SOC stocks and soil management.     

土壤团聚体有机碳研究进展

土壤有机碳是衡量土壤肥力的重要指标,对于促进土壤养分循环、增加养分有效性有重要作用。土壤团聚体是土壤的重要组成部分,是组成土壤结构的最小单元,受到自然因素和人为因素的影响,其形成转化过程与土壤固碳过程息息相关,因而研究团聚体和有机碳的关系及团聚体有机碳影响因素对于土壤结构的改善和土壤质量的提升具有重要意义。本文通过对文献的总结,明晰了土壤团聚体和有机碳的关系,阐述了土壤类型、施肥方式、土地利用和矿区复垦对土壤团聚体有机碳的影响,并从生物质炭的长期定位研究和复垦矿区的土壤修复两方面对土壤团聚体有机碳的研究进行展望,研究结果可为合理的农业生产提供科学依据。     

Glacier mass balance in High Mountain Asia inferred from a GRACE release-6 gravity solution for the period 2002–2016

We provide estimates of glacier mass changes in the High Mountain Asia (HMA) area from April2002 to August 2016 by employing a new version of gravity solutions of the Gravity Recovery and ClimateExperiment (GRACE) twin-satellite mission. We find a total mass loss trend of the HMA glaciers at a rateof –22.17 (±1.96) Gt/a. The largest mass loss rates of –7.02 (±0.94) and –6.73 (±0.78) Gt/a are found forthe glaciers in Nyainqentanglha Mountains and Eastern Himalayas, respectively. Although most glaciers inthe HMA area show a mass loss, we find a small glacier mass gain of 1.19 (±0.55) and 0.77 (±0.37) Gt/a inKarakoram Mountains and Western Kunlun Mountains, respectively. There is also a nearly zero massbalance in Pamirs. Our estimates of glacier mass change trends confirm previous results from the analysisof altimetry data of the ICESat (ICE, Cloud and Land Elevation Satellite) and ASTER (AdvancedSpaceborne Thermal Emission and Reflection Radiometer) DEM (Digital Elevation Model) satellites inmost of the selected glacier areas. However, they largely differ to previous GRACE-based studies which weattribute to our different post-processing techniques of the newer GRACE data. In addition, we explicitlyshow regional mass change features for both the interannual glacier mass changes and the 14-a averagedseasonal glacier mass changes. These changes can be explained in parts by total net precipitation (netsnowfall and net rainfall) and net snowfall, but mostly by total net radiation energy when compared to datafrom the ERA5-Land meteorological reanalysis. Moreover, nearly all the non-trend interannual masschanges and most seasonal mass changes can be explained by the total net radiation energy data. The massloss trends could be partly related to a heat effect due to increased net rainfall in Tianshan Mountains, QilianMountains, Nyainqentanglha Mountains and Eastern Himalayas. Our new results for the glacier mass changein this study could help improve the understanding of glacier variation in the HMA area and contribute tothe study of global change. They could also serve the utilization of water resources there and in neighboringareas.     

质量不平衡对单叶片叶轮径向受力的影响

为了寻找改善单叶片离心叶轮径向受力的方法,通过对一单端面配重的单叶片叶轮进行研究,在外特性试验验证定常数值计算精度的前提下,进行非定常数值计算,获得了单叶片叶轮的径向力矢量分布规律,发现设计工况附近,叶轮所受径向力的方向与叶片相对位置基本固定.基于整周期内径向力的矢量平均,获得平均径向受力的大小和方向.利用虚拟样机仿真技术,获得了质量平衡的叶轮,以及质量不平衡的叶轮;该叶轮的不平衡质量在旋转作用下产生的离心力,正好与平均水力径向力大小接近、方向相反.通过单向流固耦合仿真,发现偏心质量叶轮在实际运行中径向受力大幅度减小,证明了通过精确控制不平衡质量大小及相位角,减小和改善单叶片叶轮径向受力的方法是可行的.     

基于"量-质-域-流"四维指标体系的水资源荷载状况评价——以黑河流域三地市为例

随着社会经济用水不断增加，水资源供需矛盾加剧，水资源系统出现荷载不均衡现象，制约了区域发展，危及生态环境良性循环。本文从水资源系统的负荷需求和承载能力出发，基于“量、质、域、流”四个维度构建水资源荷载均衡评价指标体系，采用指标规范化的正态云模型，评价2015年黑河流域张掖市、酒泉市、阿拉善盟水资源配置方案的荷载均衡状况，并依据负荷与承载能力评分二维坐标，分出低负荷-高承载能力、低负荷-低承载能力、高负荷-高承载能力和高负荷-低承载能力四个分区。评价结果表明：2015年三地水资源荷载状况均为Ⅳ级，张掖市综合评分为3.697，酒泉市为3.657，阿拉善盟为3.901，三地均处于高负荷-低承载能力区域；三地在水质维度上处于低负荷-高承载能力区间，水质维度评分均处于Ⅱ级，酒泉市水质评分优于张掖市，张掖市水质评分优于阿拉善盟；在水量、水域、水流维度上均处于高负荷-低承载能力区间，水量方面三地处于Ⅳ级，张掖市优于酒泉市，酒泉市优于阿拉善盟；水域方面张掖和阿拉善盟评分均处于Ⅴ级，酒泉评分处于Ⅳ级；水流方面三地均处于Ⅴ级。需要采取调控手段在水量、水域、水流方面上进行“增强承载”和“卸荷”。     

外源褪黑素对干旱胁迫下大豆鼓粒期生理和产量的影响

干旱胁迫降低大豆产量,探究提高大豆耐旱能力和降低产量损失的机制对大豆生产具有重要意义。施褪黑素能缓解干旱胁迫对植株生长的抑制和氧化损伤。本试验于2017—2018年研究叶面喷施褪黑素对干旱胁迫下大豆鼓粒期叶片光合、抗逆、碳氮代谢和产量的影响表明,外源褪黑素提高干旱胁迫下大豆叶片抗氧化酶活性,抑制活性氧的产生和细胞膜损伤,缓解干旱胁迫对光合能力的抑制,提高碳氮同化能力,最终缓解干旱胁迫造成的产量损失。与干旱胁迫相比,褪黑素处理下单株荚数、单株粒数和百粒重两年平均提高了2.9%、0.8%和17.2%,产量(单株粒重)平均提高了14.7%。     

用于作物表型信息边缘计算采集的认知无线传感器网络分簇路由算法

随着无线终端数量的快速增长和多媒体图像等高带宽传输业务需求的增加，农业物联网相关领域可预见地会出现无线频谱资源紧缺问题。针对基于传统物联网的作物表型信息采集系统中存在由于节点密集部署导致数据传输过程容易出现频谱竞争、数据拥堵的现象以及固定电池的网络由于能耗不均衡引起监测周期缩减等诸多问题，本研究建立了一个认知无线传感器网络（CRSN）作物表型信息采集模型，并针对模型提出一种引入边缘计算机制的动态频谱和能耗均衡（DSEB）的事件驱动分簇路由算法。算法包括：（1）动态频谱感知分簇，采用层次聚类算法结合频谱感知获取的可用信道、节点间的距离、剩余能量和邻居节点度为相似度对被监控区域内的节点进行聚类分簇并选取簇头，构建分簇拓扑的过程对各分簇大小的均衡性引入奖励和惩罚因子，提升网络各分簇平均频谱利用率；（2）融入边缘计算的事件触发数据路由，根据构建的分簇拓扑结构，将待检测各区域变化异常表型信息触发事件以簇内汇聚和簇间中继交替迭代方式转发至汇聚节点，簇内汇聚包括直传和簇内中继，簇间中继包括主网关节点和次网关节点-主网关节点两种情况；（3）基于频谱变化和通信服务质量（QoS）的自适应重新分簇：基于主用户行为变化引起的可用信道改变，或分簇效果不佳对通信服务质量产生的干扰，触发CRSN进行自适应重新分簇。此外，本研究还提出了一种新的能耗均衡策略去能量消耗中心化（假设sink为中心），即在网关或簇头节点选取计算式中引入与节点到sink的距离成正比的权重系数。算法仿真结果表明，与采用K-medoid分簇和能量感知的事件驱动分簇(ERP)路由方案相比，在CRSN节点数为定值的前提下，基于DSEB的分簇路由算法在网络生存期与能效等方面均具有一定的改进；在主用户节点数为定值时，所提算法比其它两种算法具有更高频谱利用率。