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.     

经皮椎间孔镜手术不同入路治疗单节段腰椎间盘突出症疗效对比的回顾性研究

摘要 目的：对比经皮椎间孔镜手术不同入路治疗单节段腰椎间盘突出症（LDH）的疗效。方法：回顾性分析2018年5月至2020年5月我院收治的80例单节段LDH患者的临床资料。患者均接受经皮椎间孔镜手术,根据手术入路的不同,分为经椎间孔入路（PETD）组和经椎板间入路（PEID）组,每组均40例。比较两组的手术相关指标、术后恢复指标、手术前后的Oswestry功能障碍指数（ODI）和视觉模拟评分法（VAS）评分,以及术后并发症情况。结果：PEID组的手术时间短于PETD组,X线透视次数少于PETD组,差异均有统计学意义（P<0.05）。两组的术中出血量相比,差异无统计学意义（P>0.05）。PETD组的术后卧床时间短于PEID组,差异有统计学意义（P<0.05）。两组的术后1 d直腿抬高试验角度、住院时间、复发率相比,差异无统计学意义（P>0.05）。两组患者术后1 d、术后3个月、术后12个月的ODI评分、VAS评分均低于术前,且呈降低趋势（P<0.05）;同一时间点两组间ODI评分、VAS评分比较,差异无统计学意义（P>0.05）。两组的并发症发生率相比,差异无统计学意义（P>0.05）。结论：PETD和PEID经皮椎间孔镜手术治疗单节段LDH总体疗效和安全性接近,PETD可缩短术后卧床时间,PEID的操作难度更低、可减少手术时间和X线透视次数。临床中应视患者实际情况选择合适的入路。     

右美托咪定联合经皮穴位电刺激对混合痔剥扎术后患者肠胃功能及术后疼痛的影响

摘要 目的：探讨右美托咪定联合经皮穴位电刺激对混合痔剥扎术后患者肠胃功能及术后疼痛的影响。方法：选择2022年3月-2022年7月我院行混合痔剥扎术的患者60例,将60例患者随机分为对照组（30例）与观察组（30例）,对照组患者给予右美托咪定镇痛,观察组给予术前经皮穴位电刺激,时间为手术开始前2 min至手术结束,右美托咪定使用方法、剂量同对照组。对比两组患者术前、术后0.5 h、1 h、2 h、3 h的疼痛评分,对比两组患者的术后疼痛疗效,对比两组创面愈合时间、腐肉完全脱落时间、住院时间及胃肠功能恢复情况,对比两组术前、术后的血管活性肠肽、胃动素及胃泌素水平。结果：术前及术后3 h时,两组的疼痛评分对比无统计学意义（P>0.05）;术后0.5 h、1 h、2 h时,观察组的疼痛评分明显较对照组低（P<0.05）。观察组的术后疼痛有效率明显较对照组高,P<0.05。观察组的创面愈合时间、腐肉完全脱落时间及住院时间明显较对照组低（P<0.05）。观察组的肠鸣音恢复时间、术后恶心呕吐发生率及排气时间明显较对照组短（P<0.05）。术前,两组的血管活性肠肽、胃动素及胃泌素水平对比无统计学意义（P>0.05）;术后,两组血管活性肠肽、胃泌素水平升高,胃动素水平降低,且观察组变化幅度明显较对照组低（P<0.05）。结论：右美托咪定联合经皮穴位电刺激可改善混合痔剥扎术后患者肠胃功能及术后疼痛情况。     

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.     

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。     

中心静脉导管引流对单孔胸腔镜肺癌根治术患者术后胸腔引流的应用分析

目的:探讨中心静脉导管引流对单孔胸腔镜肺癌根治术患者术后胸腔引流的应用效果。方法:回顾性选取2019年1月至2019年12月期间我院收治的行单孔胸腔镜肺癌根治术患者80例的临床资料,根据引流方式的不同分为A组(n=40,传统引流)和B组(n=40,中心静脉导管引流),对比两组患者临床指标、生活质量、炎性因子及并发症发生情况。结果:B组引流操作时间、术后住院时间短于A组(P0.05)。两组术后3个月生活质量简表(SF-36)各维度评分均较术前升高,且B组高于A组(P0.05)。两组术前、术后3d、术后7d白介素-6(IL-6)、C反应蛋白(CRP)、肿瘤坏死因子-α(TNF-α)呈先升高后下降趋势,且术后3d、术后7d B组以上指标低于A组(P0.05)。两组术后并发症发生率比较无差异(P0.05)。结论:与传统引流相比,单孔胸腔镜肺癌根治术患者术后采用中心静脉导管引流,效果显著,可减少炎性刺激,安全可靠,有效改善患者术后生活质量。     

低剂量与常规剂量扫描在CT引导下经皮穿刺肺活检术中的临床应用价值对比研究

摘要 目的：比较低剂量与常规剂量扫描在CT引导下经皮穿刺肺活检术中的临床应用价值。方法：选择2018年1月至2019年12月我院行CT引导下经皮穿刺肺活检术的患者96例,采用随机数字表法分为低剂量组和常规剂量组,每组48例,两组分别在低剂量扫描、常规剂扫描下行CT引导下经皮穿刺肺活检术,比较两组扫描范围、X射线剂量、图像质量、穿刺成功率及并发症发生情况。结果：低剂量组CT吸收剂量加权指数（CTDIw）、平均剂量长度乘积（DLP）显著低于常规剂量组（P<0.05）,两组扫描范围比较无统计学差异（P>0.05）。低剂量组图像质量1级1例、2级1例、3级46例;常规剂量组1级0例、2级1例、3级47例,两组图像质量比较无统计学差异（P>0.05）。低剂量组穿刺成功率87.50%,常规剂量组穿刺成功率89.58%,两组穿刺成功率比较无统计学差异（P>0.05）。低剂量组并发症发生率为12.50%,常规剂量组并发症发生率为10.42%,两组并发症发生率比较差异无统计学意义（P>0.05）。结论：与常规剂量扫描相比,在CT引导下经皮穿刺肺活检术中应用低剂量扫描可以有效降低辐射剂量,但不影响图像质量和穿刺成功率,患者并发症发生率也未增加,具有较好的临床价值。