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.     

Geochronology,geochemistry, and Sr-Nd isotopes of Early Carboniferous magmatism in southern West Junggar,northwestern China: Implications for Junggar oceanic plate subduction

West Junggar is a key area for understanding intra-oceanic plate subduction and the final closure of the Junggar Ocean. Knowledge of the Carboniferous tectonic evolution of the Junggar Ocean region is required for understanding the tectonic framework and accretionary processes in West Junggar, Central Asian Orogenic Belt. A series of Early Carboniferous volcanic and intrusive rocks, namely, basaltic andesite, andesite, dacite, and diorite, occur in the Mayile area of southern West Junggar, northwestern China. Our new LA-ICPMS zircon U-Pb geochronological data reveal that diorite intruded at 334 (±1) Ma, and that basaltic andesite was erupted at 334 (±4) Ma. These intrusive and volcanic rocks are calc-alkaline, display moderate MgO (1.62%-4.18%) contents and Mg# values (40-59), and low Cr (14.5×10^-6-47.2×10^-6) and Ni (7.5×10^-6-34.6×10^-6) contents, and are characterized by enrichment in light rare-earth elements and large-ion lithophile elements and depletion in heavy rare-earth elements and high-field-strength elements, meaning that they belong to typical subduction-zone island-arc magma. The samples show low initial ⁸⁷Sr/⁸⁶Sr ratios (range of 0.703649-0.705008), positive ε_Nd(t) values (range of 4.8-6.2 and mean of 5.4), and young T_DM Nd model ages ranging from 1016 to 616 Ma, indicating a magmatic origin from depleted mantle involving partial melting of 10%-25% garnet and spinel lherzolite. Combining our results with those of previous studies, we suggest that these rocks were formed as a result of northwestward subduction of the Junggar oceanic plate, which caused partial melting of sub-arc mantle. We conclude that intra-oceanic arc magmatism was extensive in West Junggar during the Early Carboniferous.     

Projections of temperature extremes based on preferred CMIP5 models:a case study in the Kaidu-Kongqi River basin in Northwest China

The extreme temperature has more outstanding impact on ecology and water resources in arid regions than the average temperature. Using the downscaled daily temperature data from 21 Coupled Model Inter-comparison Project(CMIP) models of NASA Earth Exchange Global Daily Downscaled Projections(NEX-GDDP) and the observation data, this paper analyzed the changes in temporal and spatiotemporal variation of temperature extremes, i.e., the maximum temperature(Tmax) and minimum temperature(Tmin), in the Kaidu-Kongqi River basin in Northwest China over the period 2020–2050 based on the evaluation of preferred Multi-Model Ensemble(MME). Results showed that the Partial Least Square ensemble mean participated by Preferred Models(PM-PLS) was better representing the temporal change and spatial distribution of temperature extremes during 1961–2005 and was chosen to project the future change. In 2020–2050, the increasing rate of Tmax(Tmin) under RCP(Representative Concentration Pathway) 8.5 will be 2.0(1.6) times that under RCP4.5, and that of Tmin will be larger than that of Tmax under each corresponding RCP. Tmin will keep contributing more to global warming than Tmax. The spatial distribution characteristics of Tmax and Tmin under the two RCPs will overall the same; but compared to the baseline period(1986–2005), the increments of Tmax and Tmin in plain area will be larger than those in mountainous area. With the emission concentration increased, however, the response of Tmax in mountainous area will be more sensitive than that in plain area, and that of Tmin will be equivalently sensitive in mountainous area and plain area. The impacts induced by Tmin will be universal and farreaching. Results of spatiotemporal variation of temperature extremes indicate that large increases in the magnitude of warming in the basin may occur in the future. The projections can provide the scientific basis for water and land plan management and disaster prevention and mitigation in the inland river basin.     

复合潜流人工湿地对农村生活污水的净化效果 及其微生物群落结构特征

试验探究了复合潜流人工湿地对农村生活污水的净化效果及其微生物群落结构特征。结果表明，当水力负荷为0.35 m³·(m²·d）^-1时，系统对TN、NH₄⁺-N、COD和TP去除效率分别为（89.84±7.64）%、（98.67±1.31）%、（61.63±16.01）%和（70.21±8.00）%。湿地中一共发现11个主要菌门、18个主要菌纲和33个主要菌属，变形菌门（Proteobacteria）、蓝藻门（Cyanobacteria）、拟杆菌门（Bacteroidetes）、厚壁菌门（Firmicutes）、绿弯菌门（Chloroflexi）、酸杆菌门（Acidobacteria）、放线菌门（Actinobacteria）是其中的优势菌门，它们在各级湿地中表层和底层的相对丰度分别是57.26%、61.37%、91.60%、93.22%、88.78%、88.02%。蓝藻菌纲（Cyanobacteria）、α-变形菌纲(Alphaproteobacteria) 、芽孢杆菌纲(Bacilli)和γ-变形菌纲(Gammaproteobacteria)、β-变形菌纲(Betaproteobacteria)是其中优势菌纲，约占主要菌纲的70%。共有17个优势菌属，在各级湿地中的分布情况不同，其中芽孢杆菌属（Bacillus）相对丰度最高，集中分布于第三级湿地，其次是Leptolyngbya、席藻属（Phormidium），在第一、二级湿地中广泛分布。复合潜流人工湿地具有良好污水净化效果，系统中有机物和氮素的去除主要依靠微生物作用，磷素的去除主要依靠基质吸附沉淀作用。     

基于SD变化环境下农业水资源供需平衡模拟

为了探讨变化环境对农业水资源供需平衡的影响,运用系统动力学软件Vensim-Dss建立了农业水资源供需平衡的系统动力学模型,综合考虑社会经济发展和气候变化情景,仿真模拟了变化环境下农业供、需水量及缺水量的变化情况.石羊河流域模拟结果表明:未来农业供水量和需水量受气候变化的影响程度不同,但 2033年以后,农业供水量在不同气候变化情景下的变化趋势相同;不同行政区农业水资源系统对气候变化的响应存在明显差异,金昌市A2气候情境缺水率大于B2情景,在2029年、2038年缺水率分别达到32.0%,28.6%, B2情境下,2021年开始出现轻度缺水,中度缺水年仅出现在2023年和2039年,缺水率分别为30.7%,30.5%;武威市A2气候情境下缺水率小于B2情景,仅2038年为中度缺水,缺水率为24.9%,B2气候情景中度缺水年较多,2023年缺水率最大,达到33.2%.研究结果可以对变化环境下区域用水规划和农业发展规划提供指导.     

基于温室番茄产量和果实品质对加气灌溉处理的综合评价

【目的】研究不同灌水水平和滴头埋深条件下加气灌溉对温室番茄产量、灌溉水分利用效率（IWUE）和果实品质的影响,进而对不同试验处理进行综合评价。【方法】试验以常规地下滴灌（S）为对照,设置在W1、W2和W3（对应作物-皿系数k_cp分别为0.6、0.8和1.0）3个灌水水平与D1和D2（分别对应15 cm和25 cm）2种滴头埋深下进行加气灌溉（O）,共12个处理。基于各处理下果实产量和品质指标的差异,通过主成分分析法探索较优的试验处理。【结果】加气灌溉下单株产量、单果重、IWUE、果实中番茄红素、Vc、可溶性糖含量和糖酸比较对照分别显著增加了21.2%、23.9%、21.0%、28.1%、36.0%、22.8%和28.0%（P<0.05）。主成分分析中,第1主成分主要受番茄红素、Vc、灌溉水分利用效率和糖酸比的正影响,且处理W2D1O和W2D2O的得分分列第1和2名。因此处理W2D1O和W2D2O在兼顾节水和番茄果实营养品质方面较优。第2主成分主要受单株产量的正影响和有机酸的负影响,各处理有机酸含量未形成显著性差异且处理W3D1O的单株产量最高,因此得分最高。处理W3D1O的综合得分在12个处理中位列第1位。【结论】灌水水平k_cp为1.0,滴头埋深15 cm的加气灌溉处理可兼顾节水和温室番茄高产、优质的要求,为加气灌溉的实际应用提供理论依据。     

First serological evidence of West Nile virus infection in wild birds in Northern Algeria

While the epidemiology of Flaviviruses has been extensively studied in most of the Mediterranean basin, little is known about the current situation in Algeria. In order to detect the circulation of West Nile (WNV) and Usutu viruses (USUV) in Kabylia, 165 sera were collected from two wild birds species, namely the long distance migrant Turdus philomelos (song thrush) (n = 92) and the resident Passer domesticus (house sparrow) (n = 73). A total of 154 sera were first analyzed by commercial competition ELISA. WNV and USUV micro-neutralization tests were performed on all c-ELISA positive sera and all samples with poor volume. Overall, 7.8 % (CI95 %: 3.5–11.9) were positive by c-ELISA. Positive results were detected in 12.5 % (CI95 %:5.6–19.4) of song thrushes and 1.5 % (CI95 %: 0.0–4.5) for sparrow.Micro-neutralization tests revealed an overall seroprevalence of 6.7 % for WNV (CI95 %: 2.9–10.3), Neutralizing antibodies were found in 8.7 % (CI95 %: 3.0–14.4) for song thrushes and in 4.1 % (CI95 %: 0.0–8.7) of sparrows. The current study demonstrates significant seroprevalence of WNV antibodies in wild birds in Algeria.     

近30年华南中部可降水量的变化分析

本文利用NCEP/NCAR逐月可降水量的再分析资料,选取1983年1月-2012年12月共360个时次的数据,分析可降水量的变化趋势。得出结论：近30年内华南中部的可降水量总体上呈下降趋势；季节性变化明显,可降水量值呈夏高冬低趋势。     

1047年北宋宫廷祈雨的诸相

本文以1047年发生在北宋宫廷内的一场祈雨祭祀为研究对象,运用"剧场国家"理论,描绘了祈雨的"展演"相与"权力"相,研究了祈雨期内以展演为表征、以权力为暗流的人神、人地、人人关系。研究发现:一方面,祈雨是充满象征意义的展演式活动,祈雨人宋仁宗需要向天神与黎民展演德行,而展演德行又需借助于气象技术;另一方面,贾昌朝被罢相是多重因素作用下的结果,罢相反映出北宋中期朝廷内激烈的政治纷争,其仍为庆历新政后权力博弈的延续。可见这场祈雨是一场德行的展演,也是实在的操纵帝国的权力之争。     

茶和天下语境下历史典故的重温与传播——以“以茶代酒”为例

中华茶文化历史源远流长,文化内容博大精深,是中国文化乃至世界文化重要的组成部分。然而,历史茶文化尤其是历史典故,大多需要重新解读,只有将历史与现实结合起来,有针对性且有说服力地赋予新的时代内涵,才能扩大其在世界范围的价值认同。基于此,本文以“以茶代酒”为例,将其置于茶和天下的语境下,在重温这一历史典故的基础上,从增加中华茶文化魅力,促进历史茶文化的传播的角度出发,分析探讨了以茶代酒的当代价值或中华茶文化核心价值的当代体现,并根据全球化与茶文化传播的需要,从增强自信性、构建“同型性”、抢占先机性、设计备选性等方面,提出了如何通过以茶代酒,推动中华茶文化核心价值实现的相关策略。