Continuous measurement of oxygen concentration in citrus soil by means of a waterproof zirconia oxygen sensor

A limiting-current type of zirconia oxygen sensor has been developed and its efficiency was tested for the determination of oxygen in soil air. This oxygen sensor is waterproof and has a very short response time. By the use of the sensor, changes in soil oxygen concentration, due to undecomposed organic material and waterlogging, were observed. The sensor was found to be highly stable in the soil and suitable for continuous oxygen monitoring in the field.     

腹腔镜胆总管切开取石术后MRCP与T管造影的对照研究

摘要 目的：评估磁共振胰胆管造影（Magnetic Resonance Cholangiopancreatography, MRCP）是否可以成为腹腔镜胆总管切开取石术后T管造影的替代方法。方法：回顾性分析我院普外科自2017年1月至2020年12月收治的胆总管结石患者的临床资料,共收集接受腹腔镜胆总管切开取石术+T管引流术患者263例,将其中拔除T管前行MRCP者54例定为MRCP组,连续选取拔除T管前行T管造影者54例为T管造影组。对两组患者的检查结果、不良反应发生率、住院治疗比例、检查至拔T管时间、抗生素使用率、相关医疗费用等指标进行记录并分析。结果：T管造影组与MRCP组诊断胆总管残余结石的阳性率、假阳性率和准确率无统计学差异（P＞0.05）。T管造影组不良反应发生率、住院治疗比例、检查至拔T管时间、抗生素使用率和相关医疗费用均显著高于MRCP组,两组差异有统计学意义（P＜0.05）。结论：MRCP可替代T管造影作为腹腔镜胆总管切开取石术后拔除T管前的诊断方法。     

云南东川黄铜矿酸性浸矿废水中微生物群落分析

利用限制性片段长度多态性和16s rRNA PCR扩增及其序列分析来研究中国云南东川黄铜矿酸性浸矿废水(AMD)中微生物群落结构。基于建立16s rRNA克隆文库的分子方法常常被用来研究AMD中微生物生态。一小部分的rRNA被PCR扩增,克隆,然后用限制性片段长度多态性来筛选出其不同种类。在三个样地中,共挑选了357个克隆子,经限制性酶切分析后聚为100个可操作分类单元(OTU)。一个OTU代表各个样地中出现的同一种酶切图谱。有58个OTU被测序分析,结果在基因数据库中比对分析,其系统发育分析表明它们聚类为六大类:γ-proteobacteria,Acidobacteria,Clostridia,Actinobacteria,Nitrospira,α-pro- teobacteria。其中,γ-proteobacteria为最大的群落,在三个样地DCK-Ⅰ,DCN-Ⅰand DC-Ⅱ中分别占36%,57%,62%的比例。但与浸矿相关的微生物如At.ferrooxidans;L ferrooxidans等却发现的很少,仅在两个样地中各发现四个相关的OTUs。在这个AMD环境中浸矿相关的微生物都不是优势种群。     

Soil moisture dynamics and restoration of self‐sustaining native vegetation ecosystem on an open‐cut coal mine

Post‐mining landscape reconstruction on open‐cut coal mines aims to support restoration of self‐sustaining native vegetation ecosystems that in perpetuity require no extra inputs relative to unmined analogs. Little is known about the soil moisture retention capacity of the limited layer of topsoil replaced (often <30 cm deep), impacts of deep ripping of the profile, and the combined impacts of these on plant available water during the mine restoration process. We examined changes in soil moisture parameters (soil water potential, Ψ, and soil water content, Θ) daily using automated soil sensors installed at 30 and 45–65 cm depths on mine restoration sites aged between 3 and 22 years and on adjacent remnant vegetation sites following heavy rainfall events at Meandu mine, southeast Queensland, Australia. Consistent patterns in soil moisture attributes were observed among rehabilitated sites with generally marked differences from remnant sites. Remnant site soil profiles had generally higher Θ after drying than rehabilitated sites and maintained high Ψ for extended periods after rain events. There was a relatively rapid decline of Ψ on reconstructed soil profiles compared with remnant sites although the times of decline onset varied. This response indicated that vegetation restoration sites released soil moisture more rapidly than remnant sites but the rate of drying decreased with increasing rehabilitation age and increased with increasing tree stem density. The rapid drying of mine rehabilitated sites may threaten the survival of some remnant forest species, limit tree growth, and delay restoration of self‐sustaining native ecosystem.     

Evapotranspiration of tropical peat swamp forests

In Southeast Asia, peatland is widely distributed and has accumulated a massive amount of soil carbon, coexisting with peat swamp forest (PSF). The peatland, however, has been rapidly degraded by deforestation, fires, and drainage for the last two decades. Such disturbances change hydrological conditions, typically groundwater level (GWL), and accelerate oxidative peat decomposition. Evapotranspiration (ET) is a major determinant of GWL, whereas information on the ET of PSF is limited. Therefore, we measured ET using the eddy covariance technique for 4–6 years between 2002 and 2009, including El Niño and La Niña events, at three sites in Central Kalimantan, Indonesia. The sites were different in disturbance degree: a PSF with little drainage (UF), a heavily drained PSF (DF), and a drained burnt ex‐PSF (DB); GWL was significantly lowered at DF, especially in the dry season. The ET showed a clear seasonal variation with a peak in the mid‐dry season and a large decrease in the late dry season, mainly following seasonal variation in net radiation (R_n). The R_n drastically decreased with dense smoke from peat fires in the late dry season. Annual ET forced to close energy balance for 4 years was 1636 ± 53, 1553 ± 117, and 1374 ± 75 mm yr^?1 (mean ± 1 standard deviation), respectively, at UF, DF, and DB. The undrained PSF (UF) had high and rather stable annual ET, independently of El Niño and La Niña events, in comparison with other tropical rainforests. The minimum monthly‐mean GWL explained 80% of interannual variation in ET for the forest sites (UF and DF); the positive relationship between ET and GWL indicates that drainage by a canal decreased ET at DF through lowering GWL. In addition, ET was decreased by 16% at DB in comparison with UF chiefly because of vegetation loss through fires.     

Distributional patterns of freshwater taxa (fishes, crustaceans and plants) from the Mexican Transition Zone

Aim  To test whether distributional patterns of Neotropical freshwater taxa fit the generalized tracks already postulated for terrestrial groups occurring in the Mexican Transition Zone.
Location  The study units comprised 17 hydrological basins located along the Pacific coast of the Americas from Mexico to Panama, and in the Gulf of Mexico from the Papaloapan to the Grijalva–Usumacinta basin.
Methods  Distributional data for 22 fish species, 34 crab species of the tribe Pseudothelphusini, and 22 strictly freshwater species of angiosperms were analysed. Parsimony analysis of endemicity is based on presence/absence data of these taxa and uses the computer programs Winclada and NONA.
Results  Three generalized tracks were obtained: (1) Mexican North Pacific, (2) Mexican Central Pacific, and (3) Southern Mexico–Guatemala. A node resulted at the intersection of the first two tracks, coinciding with the Neovolcanic Axis in central Mexico.
Main conclusions  Freshwater generalized tracks with an altitudinal distribution below 1000 m, mainly including fishes and angiosperms, are close to the Tropical Mesoamerican generalized track. Generalized tracks above 1000 m, including freshwater crabs, have a stronger affinity with the Mountain Mesoamerican track. The Isthmus of Tehuantepec represents a node for the Neotropical freshwater and terrestrial biota. These results seem to indicate that common geobiotic processes have induced these patterns.     

酸性矿坑废水及目前研究酸性矿坑废水微生物群落的方法

本文通过对近期文献综述,阐明了酸性矿坑废水（Acid Mine Drainage,AMD）的形成机理以及AMD的微生物多样性。综述了AMD形成过程中的硫化金属矿、黄铁矿以及白铁矿的氧化作用,同时对影响AMD形成的化学、生物学以及物理因素及其过程进行了较为详尽的阐述。对目前使用分子生物学对AMD中微生物群落研究的几种手段进行的总结。最后对研究AMD微生物群落这几种分子生物学方法进行了归纳讨论。阐明了这几种分子生物方法对研究AMD微生物群落的重要意义。     

Genealogy and palaeodrainage basins in Yunnan Province: phylogeography of the Yunnan spiny frog,Nanorana yunnanensis (Dicroglossidae)

Historical drainage patterns adjacent to the Qinghai‐Tibetan Plateau differed markedly from those of today. We examined the relationship between drainage history and geographic patterns of genetic variation in the Yunnan spiny frog, Nanorana yunnanensis, using approximately 981 base pairs of mitochondrial DNA partial sequences from protein‐coding genes ND1 and ND2, and intervening areas including complete tRNA^Ile, tRNA^Gln and tRNA^Met. Two null hypotheses were tested: (i) that genetic patterns do not correspond to the development of drainage systems and (ii) that populations had been stable and not experienced population expansion, bottlenecking and selection. Genealogical analyses identified three, major, well‐supported maternal lineages, each of which had two sublineages. These divergent lineages were completely concordant with six geographical regions. Genetic structure and divergence were strongly congruent with historical rather than contemporary drainage patterns. Most lineages and sublineages were formed via population fragmentation during the rearrangement of paleodrainage basins in the Early Pliocene and Early Pleistocene. Sympatric lineages occurred only in localities at the boundaries of major drainages, likely reflecting secondary contact of previously allopatric populations. Extensive population expansion probably occurred early in the Middle Pleistocene accompanying dramatic climatic oscillations.     

First record of the black bullhead Ameiurus melas (Teleostei: Ictaluridae) in Poland

The North American catfish, the black bullhead Ameiurus melas, is recorded for the first time in Poland. The origin of these fish is not clear, but their presence may be associated with unregulated introductions by anglers.     

养殖排放农药和抗生素在红树林区中残留的初步研究

广西北海大冠沙红树林区是养殖废水的排放地,该文报道2008年10月农药和抗生素在该林区红树林滩、沙滩和潮沟三类生境的残留水、沉积物和底栖动物中的分布与含量。通过对103种农药和22种抗生素检测,发现该林区有16种农药,4种抗生素,其中甲氰菊酯、仲丁威和醚菌酯是主要的污染农药。在残留水中检出12种农药,它们在红树林滩、沙滩和潮沟中的总浓度分别是42.70、29.63和27.41ng/L。在沉积物中检出10种农药,它们在红树林滩、沙滩和潮沟中的总浓度分别是7.90、6.70和7.29μg/kg.DW。在底栖动物体内检出4种农药和3种抗生素。分析表明,红树林滩(残留水和沉积物)比底栖动物更易受到养殖废水的污染,底栖动物对抗生素的富集能力似乎高于对农药的富集能力,生境间污染相似度高于样品间的污染相似度。