Mathematical modelling of runoff and material transport from drainage areas into recipient water bodies

This paper describes a set of mathematical models to calculate runoff, soil erosion and chemical substance yields for drainage areas. The models represent different degrees of complexity and details of describing hydrological and hydrochemical processes. The availability of initial information and the requirements of the task determine the choice of a model for each particular case. These models have been written as PC/AT programs, to enable their use by a wide range of specialists. The models have been tested in different physical and geographical conditions, e.g. in some small watersheds on the Karelian Isthmus, west of Lake Ladoga, and in experimental catchment areas located in the Valdai Hills area in the southern part of Lake Ladoga drainage area. In further applications the drainage area models have been combined with models of the recipient water body, to obtain a single model of a watershed-lake system. The results of tests have proved that the models can be used for evaluation, simulation and forecasting of the processes of rainfall and snowmelt runoff, infiltration, evaporation, water erosion and pollutant wash-off from drainage areas.     

Four fish species new to the Omo-Turkana basin,with comments on the distribution ofNemacheilus abyssinicus (Cypriniformes: Balitoridae) in Ethiopia

Four fish species,Pollimyrus isidori (Mormyridae),Barbus paludinosus, Labeo forskalii (Cyprinidae), andNemacheilus abyssinicus (Balitoridae), new to the Omo-Turkana basin, were recorded from the Gojeb River, a tributary of the Omo River (south-western Ethiopia). Occurrence of the latter species in the upper reaches of the Blue Nile and of the Omo drainage substantiates the belonging of the upper parts of these water systems to the Abyssinian highlands ichthyofaunal province.     

Estimating regional carbon stocks and spatially covarying edaphic factors using soil maps at three scales

Most estimates of regional and global soil carbon stocks are based on extrapolations of mean soil C contents for broad categories of soil or vegetation types. Uncertainties exist in both the estimates of mean soil C contents and the area over which each mean should be extrapolated. Geographic information systems now permit spatially referenced estimates of soil C at finer scales of resolution than were previously practical. We compared estimates of total soil C stocks of the state of Maine using three methods: (1) multiplying the area of the state by published means of soil C for temperate forests and for Spodosols; (2) calculating areas of inclusions of soil taxa in the 1:5,000,000 FAO/UNESCO Soils Map of the World and multiplying those areas by selected mean carbon contents; and (3) calculating soil C for each soil series and map unit in the 1:250,000 State Soil Geographic Data Base (STATSGO) and summing these estimates for the entire state. The STATSGO estimate of total soil C was between 23% and 49% higher than the common coarse scale extrapolations, primarily because STATSGO included data on Histosols, which cover less than 5% of the area of the state, but which constitute over one-third of the soil C. Spodosols cover about 65% of the state, but contribute less than 39% of the soil C. Estimates of total soil C in Maine based on the FAO map agreed within 8% of the STATSGO estimate for one possible matching of FAO soil taxa with data on soil C, but another plausible matching overestimated soil C stocks. We also compared estimates from the 1:250,000 STATSGO database and from the 1:20,000 Soil Survey Geographic Data Base (SSURGO) for a 7.5 minute quadrangle within the state. SSURGO indicated 13% less total soil C than did STATSGO, largely because the attribute data on depths of soil horizons in SSURGO are more specific for this locality. Despite localized differences, the STATSGO database offers promise of scaling up county soil survey data to regional scales because it includes attribute data and estimates of areal coverage of C-rich inclusions within map units. The spatially referenced data also permit examination of covariation of soil C stocks with soil properties thought to affect stabilization of soil C. Clay content was a poor predictor of soil C in Maine, but drainage class covaried significantly with soil C across the state.     

超声引导下神经阻滞麻醉联合全身麻醉对股骨头置换老年患者麻醉效果及术后认知功能的影响

摘要 目的：研究超声引导神经阻滞麻醉联合全身麻醉对股骨头置换老年患者的麻醉效果及对术后认知功能的影响。方法：选取2019年1月至2021年12月期间我院收治的150例拟行股骨头置换术的老年患者,随机分为对照组和观察组,各75例。对照组患者行常规全身麻醉,观察组在对照组的基础上行超声引导下神经阻滞麻醉,比较两组患者的血流动力学指标,拔管时间、苏醒时间和复苏室停留时间,苏醒后疼痛,术后认知功能及不良反应的发生率。结果：观察组患者各时间点的心率（HR）和平均动脉压（MAP）均较对照组低（P＜0.05）。观察组拔管时间、苏醒时间和复苏室停留时间均较对照组短（P＜0.05）。观察组患者术后视觉模拟评分（VAS）均低于同一时间点的对照组（P＜0.05）。与对照组相比,观察组患者术后1 h、12 h和24 h的简易智力状态检查（MMSE）评分均较高（P＜0.05）,观察组术后1 h、12 h和24 h术后认知功能障碍（POCD）发生率较对照组低（P＜0.05）。两组患者不良反应发生率无差异（P＞0.05）。结论：超声引导神经阻滞麻醉可稳定血流动力学,缩短拔管、苏醒及复苏室停留时间,减轻术后疼痛,改善术后认知功能,减少POCD的发生,值得临床推广。     

不同剂量右美托咪定联合超声引导下多点髂筋膜间隙阻滞在老年全髋关节置换术中的应用效果分析

摘要 目的：探讨超声引导下多点髂筋膜间隙阻滞联合不同剂量右美托咪定在老年全髋关节置换术（THA）中的应用效果。方法：选取2019年11月-2022年12月北京积水潭医院贵州医院择期行THA的老年患者120例,按照随机数字表法分为A组（n=40）、B组（n=40）、C组（n=40）,三组均接受超声引导下多点髂筋膜间隙阻滞治疗,在此基础上,A组、B组、C组分别给予0.5 μg/kg、1.0 μg/kg、1.5 μg/kg右美托咪定注射液。对比三组临床指标、血流动力学指标、应激反应指标、脑神经损伤情况,观察三组围术期间不良反应发生情况。结果：B组、C组的阻滞消退时间、拔管时间长于A组,首次下床时间短于A组（P<0.05）。B组、C组的阻滞消退时间、拔管时间、首次下床时间对比无差异（P>0.05）。三组麻醉诱导后即刻（T1）~手术结束时（T3）时间点心率（HR）、平均动脉压（MAP）升高后降低（P<0.05）。B组、C组的T1~T3时间点HR、MAP均低于A组,且B组低于C组（P<0.05）。三组T3时间点皮质醇（Cor）、白介素-6（IL-6）、肿瘤坏死因子-α（TNF-α）升高（P<0.05）。B组、C组的T3时间点Cor、IL-6、TNF-α均低于A组,且B组低于C组（P<0.05）。B组、C组的T3时间点中枢神经特异性蛋白（S100β）均低于A组,且B组低于C组（P<0.05）。B组、C组的T3时间点脑源性神经生长因子（BDNF）均高于A组,且B组高于C组（P<0.05）。三组不良反应发生率组间对比无差异（P>0.05）。结论：超声引导下多点髂筋膜间隙阻滞联合1.0 μg/kg右美托咪定在THA中具有更好的麻醉效果,可缩短首次下床时间,减轻机体应激反应、血流动力学波动以及脑部神经损伤。     

超声引导下隐神经联合IPACK阻滞对老年全膝关节置换术患者应激反应、炎性细胞因子及膝关节活动度的影响

摘要 目的：探讨超声引导下隐神经联合腘动脉与膝关节后囊间隙（IPACK）阻滞对老年全膝关节置换术（TKA）患者应激反应、炎性细胞因子及膝关节活动度的影响。方法：根据随机数字表法,将无锡市中医医院2021年3月~2022年9月期间收治的102例初次行TKA的老年患者分为观察组（超声引导下隐神经联合IPACK阻滞镇痛处理）和对照组（超声引导下隐神经镇痛处理）,每组各51例。对比两组疼痛情况、炎性细胞因子、应激反应指标、不良反应发生率、膝关节活动度。结果：观察组术后6 h、术后12 h、术后24 h视觉模拟评分法（VAS）评分低于对照组（P<0.05）。观察组术后48 h肿瘤坏死因子-α（TNF-α）、白细胞介素（IL）-6、IL-1β、β-淀粉样蛋白（Aβ）低于对照组（P<0.05）。观察组术后48 h血管紧张素Ⅱ（AngⅡ）、皮质醇（COR）低于对照组（P<0.05）。观察组术后24 h、术后48 h膝关节活动度大于对照组（P<0.05）。两组不良反应发生率对比无差异（P>0.05）。结论：超声引导下隐神经联合IPACK阻滞用于TKA患者,具有较好的镇痛效果,可减轻应激反应,抑制炎性细胞因子过度分泌,改善膝关节活动度,麻醉效果较好。     

Reducing acidic discharges from coastal wetlands in eastern Australia

Much of eastern Australia's coastal lowlands are underlain by Holocene sulfidic sediments. Large areas have been drained for agriculture. Drained, sulfidic sediments oxidize and produce highly acidic discharge (pH<4) with significant impacts on estuarine ecosystems. The rate of production of acid from drained floodplains is between 100 to 300 kg H₂SO₄ /ha/y and hundreds of tonnes of H₂SO₄ can be discharged in a single flood from the floodplain. Generation and export of acidity is controlled by the water balance of the floodplain, the characteristics of the drainage system and the distribution of sulfides. Evapotranspiration by native plants and crops plays a dominant role in the oxidation of sediments in dry periods. In wet periods, upland discharges to floodplains dominate the water balance. Drain spacing and drain depth are critical factors in the export of acidity into coastal streams. Amelioration of acidic outflows requires an understanding of the interaction between chemical and hydrological processes in sulfidic landscapes. Redesign of drainage systems to manage surface waters and reduce drain density with the treatment of drains with lime offer promise for treating acidic discharge and reducing impacts. Reflooding of drained, partially oxidized floodplains with freshwater may not be a panacea because of the large volumes of acid stored in the soil, a lack of labile organic matter in the sediments needed to reduce sulfate and irreversible changes to the soil due to oxidation. Tidal brackish water reflooding of unproductive acidified lowlands offers promise for rehabilitating wetlands. Sulfidic wetlands which are still undrained should remain so unless all acidic discharge can be treated.     

Fluctuations of the soil environment and fine root growth in a young Sitka spruce plantation

Summary From soil cores extracted at 5 day intervals from 3 May to 6 August it was found that the biomass of fine roots in a Sitka spruce plantation, 14 years old, fluctuated with maxima in late May and mid July. The earlier peak coincides with increasing soil temperatures during a period of high incident precipitation and the latter developed when the soil profile was rewetted. Fine root biomass and soil moisture tension (SMT) were significantly and negatively correlated in three of four soil horizons. Root mortality occurred whenever incident precipitation failed to maintain soil moisture tension near zero. In the very open pored horizons the critical SMT for root death was unexpected small, <0.1 bars; in the peat horizons it wasc 0.2 bars.     

Intracoronary application of nicorandil regulates the inflammatory response induced by percutaneous coronary intervention

Intracoronary application of nicorandil can effectively reduce the myocardial no‐reflow (MNR) after percutaneous coronary intervention (PCI). We sought to investigate the mechanisms of nicorandil in preventing MNR, besides that of dilating the coronary microvasculature. A total of 60 patients undergoing PCI were enrolled and randomly divided into a nicorandil group and a control group. Before PCI, 2 mg of nicorandil or an equal volume of normal saline was injected into the coronary artery. Blood samples were collected before, 24 hours and 1 week after PCI and inflammatory cytokines were tested. In the control group, the expression of pro‐inflammatory cytokines was significantly increased, while the anti‐inflammatory cytokines were decreased 24 hours after PCI. In contrast, these changes were reversed in the nicorandil group, indicating that nicorandil regulated the inflammatory response induced by PCI. Then, proteomic analysis was performed to further elucidate the potential mechanisms. A total of 53 differentially expressed proteins (DEPs) were found 24 hours after PCI in the control group, and the changes of these relevant genes were reversed in the nicorandil group. These DEPs were significantly enriched in the inflammatory pathways. In conclusion, the intracoronary application of nicorandil before PCI can regulate the inflammatory responses induced by PCI, which might be an important mechanism of nicorandil in preventing MNR.     

腰大池引流联合法舒地尔治疗动脉瘤性蛛网膜下腔出血的疗效及对血清sICAM-1、FABP、MCP-1水平和脑积水形成的影响

目的:分析腰大池引流联合法舒地尔治疗动脉瘤性蛛网膜下腔出血的疗效及对血清可溶性细胞间黏附分子-1(sICAM-1)、脂肪酸结合蛋白质(FABP)、核细胞趋化蛋白(MCP-1)水平和脑积水形成的影响。方法:选择我院2016年3月~2018年3月收治的112例动脉瘤性蛛网膜下腔出血患者,按随机数字表法分为对照组(n=48)和研究组(n=64)。对照组采用腰大池引流治疗,研究组基于对照组联合法舒地尔治疗。比较两组临床疗效,治疗前后血清sICAM-1、FABP、MCP-1水平、血压、大脑中动脉血流参数水平和神经功能的变化,脑积水发生率及不良反应发生情况。结果:治疗后,研究组总有效率显著高于对照组(89.02%vs.72.91%,P<0.05)。两组治疗后血清sICAM-1、FABP、MCP-1、血压、大脑中动脉血流参数水平和神经功能缺损评分量表(NIHSS)均较治疗前下降,格拉斯哥昏迷评分(GCS)均较治疗前上升,研究组以上指标较对照组改变更明显(均P<0.05)。两组不良反应发生情况比较差异无统计学意义(P>0.05)。结论:腰大池引流联合法舒地尔治疗动脉瘤性蛛网膜下腔出血的疗效明显优于单用腰大池引流治疗,其可显著降低血清sICAM-1、FABP、MCP-1水平,降低脑积水发生率,改善患者预后。