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941.
942.
943.
Nives Ogrinc Tjaša Kanduč Bor Krajnc Urša Vilhar Primož Simončič Lixin Jin 《Journal of Soils and Sediments》2016,16(2):382-395
Purpose
Soil carbon dynamics were studied at four different forest stands developed on bedrocks with contrasting geology in Slovenia: one plot on magmatic granodiorite bedrock (IG), two plots on carbonate bedrock in the karstic-dinaric area (CC and CD), and one situated on Pleistocene coalluvial terraces (FGS).Materials and methods
Throughfall (TF) and soil water were collected monthly at each location from June to November during 2005–2007. In soil water, the following parameters were determined: T, pH, total alkalinity, concentrations of Ca2+ and Mg2+, dissolved organic carbon (DOC), and Cl? as well as δ13CDIC. On the other hand, in TF, only the Cl? content was measured. Soil and plant samples were also collected at forest stands, and stable isotope measurements were performed in soil and plant organic carbon and total nitrogen and in carbonate rocks. The obtained data were used to calculate the dissolved inorganic carbon (DIC) and DOC fluxes. Statistic analyses were carried out to compare sites of different lithologies, at different spatial and temporal scales.Results and discussion
Decomposition of soil organic matter (SOM) controlled by the climate can explain the 13C and 15?N enrichment in SOM at CC, CD, and FGS, while the soil microbial biomass makes an important contribution to the SOM at IG. The loss of DOC at a soil depth of 5 cm was estimated at 1 mol m?2 year?1 and shows no significant differences among the study sites. The DOC fluxes were mainly controlled by physical factors, most notably sorption dynamics, and microbial–DOC relationships. The pH and pCO2 of the soil solution controlled the DIC fluxes according to carbonate equilibrium reactions. An increased exchange between DIC and atmospheric air was observed for samples from non-carbonate subsoils (IG and FGS). In addition, higher δ13CDIC values up to ?19.4?‰ in the shallow soil water were recorded during the summer as a consequence of isotopic fractionation induced by molecular diffusion of soil CO2. The δ13CDIC values also suggest that half of the DIC derives from soil CO2 indicating that 2 to 5 mol m?2 year?1 of carbon is lost in the form of dissolved inorganic carbon at CC and CD after carbonate dissolution.Conclusions
Major difference in soil carbon dynamics between the four forest ecosystems is a result of the combined influence of bedrock geology, soil texture, and the sources of SOM. Water flux was a critical parameter in quantifying carbon depletion rates in dissolved organic and inorganic carbon forms.944.
Samuel Raj Babu Arulmani Vimalan Jayaraj Solomon RobinsonDavid Jebakumar 《Journal of Soils and Sediments》2016,16(3):831-841
Purpose
This study was conducted to determine the existence of soil bacteria in soil by soil microbial fuel cell (SMFC). The main objectives were (1) to differentiate the type of soil which will influence the electricity production, (2) to demonstrate the impact of different volume of soil in the MFC and feeding MFC for long-term electricity production, and (3) to conclude that electricity production is directly proportional to the biofilm formation on the anode surface.Materials and methods
MudWatt kits were purchased from Keego Technologies USA, and 22 identical SMFCs were designed to study the electricity production from agricultural soil (S1) and vermicompost soil (S2). Ten milliliters of bioslurry is fed in SMFC to study the stability of electricity production at different stages. Microbes were isolated and characterized from the surface of the electrode. Biofilm analyses were done by high-content screening (HCS) system using 10 μl of acridine orange (100 μg/ml) at different stages of biofilm, and scanning electron microscopy is applied to confirm the matured biofilm on the surface of the anode.Results and discussion
Application of bioslurry at different stages of electricity production conquers the normal energy recovery of the SMFCs and S2 soil with bioslurry sample produced the highest open circuit voltage (OCV) of 2.8 V (460 days) and S1 soil sample with bioslurry produced 1.7 V (364 days). The difference between SMFCs and MudWatt kits significantly confirms that increasing the volume of soil in the anode part increases the electricity production. The maximum OCV of S1 and S2 in MudWatt kits were 1.5 V (90 days) and 1.8 V (190 days), respectively. Increased volume of soil in our SMFCs produce maximum OCV of 1.8 V (S1 for 173 days) and 2.2 V (S2 for 240 days), and HCS analysis of biofilm at different stages reveals that electricity production is directly proportional to the biofilm formation.Conclusions
Thus, it was concluded that the nature of soil and soil bacterium is important for the electricity production, and S2 soil sample produces maximum electricity than the S1 soil sample. Feeding of SMFCs with bioslurry aids the long-term and stabilized electricity production in both the soil samples.945.
Purpose
The aim of the present study was to investigate the effects of visitors’ activities on soil properties in parks of Tel Aviv-Jaffa city, Israel.Materials and methods
The city was divided into three geographical regions: south, central, and north. This division reflects the course of development of the city from south to north and encompasses various socioeconomic levels of residents. In each region, 9–15 parks were randomly chosen and classified into three groups according to their size (in m2): 2?×?103 to 10?×?103, 11?×?103 to 20?×?103, and 21?×?103 to 50?×?103. In each park soil, 0–2 cm of depth layer was sampled in areas under various levels of visitor pressure from July to August 2011, and organic matter, electrical conductivity, and sodium and chlorine contents were determined. Lawns and path and picnic areas represented low and high visitor pressure, respectively. Observations were conducted to characterize the various land uses of the parks and to estimate the numbers of visitors. Also, questionnaires were used at selected parks to assess visitors’ motivations or reasons for visiting the parks.Results and discussion
Socioeconomic indicators, such as the number of residents, the apartment areas, and the percentages of family households, differed among the regions. Soil properties differed between the areas of high and low visitor pressure: they were influenced by type of human activity, size of the park, and number of visitors.Conclusions
Soil properties are affected by variations in the intensity of park use by visitors and by the type of activities enjoyed by these visitors, both of which depend on the socioeconomic status of the park area.946.
Haroldo Lobo Leire Méndez-Fernández Maite Martínez-Madrid Michiel A. Daam Evaldo L. G. Espíndola 《Journal of Soils and Sediments》2016,16(12):2766-2774
Purpose
This study aimed at evaluating the acute effects of arsenic and zinc to the warmwater aquatic oligochaete Branchiura sowerbyi. Relative sensitivity with the coldwater species Tubifex tubifex was compared. Implications for the use of B. sowerbyi in the risk assessment of sediments in the tropics are discussed.Materials and methods
Water-only (96 h) and sediment (14 days) toxicity tests were conducted with both species evaluating a concentration series of arsenic and zinc. The tests were conducted considering the environmental conditions in the natural habitat of T. tubifex (predominantly temperate) and B. sowerbyi (predominantly tropical). Both lethal and sublethal endpoints (autotomy of the posterior body parts, abnormal behavior and appearance) were determined in the tests. The lethal (LC10 and LC50) and effect (EC10 and EC50) concentrations were also determined to assess metal sensitivity for both species.Results and discussion
Both test species were more sensitive to Zn than As in water-only tests, which is in agreement with previous studies evaluating the toxicity of these metals to aquatic oligochaetes. Sublethal effects were generally noted at concentrations lower than those leading to mortality. The warmwater oligochaete B. sowerbyi was more sensitive to both metals tested than the coldwater species T. tubifex.Conclusions
Study findings support the need for using indigenous tropical species in risk assessments in the tropics. In addition, sublethal effect parameters should be included in toxicity testing with aquatic oligochaetes.947.
以黄土高原安家沟流域为研究区域,利用GIS和RS技术,建立了安家沟流域的气象数据、DEM数据、土地利用数据,成功构建了基于SWAT模型的安家沟流域水文模型。以1982—1999年作为模型的率定期,2000—2010年作为模型的验证期,对模型进行了参数敏感性分析和参数率定。其中率定期的Nash-Sutcliffe效率系数Ens(0.71)、相关系数R2(0.73)和验证期的Nash-Sutcliffe效率系数Ens(0.69)、相关系数R2(0.68)均达到模型模拟要求。结果表明:SWAT模型基本上能反映安家沟的月径流水文过程,具有一定的实用性,以期为安家沟流域水资源高效配置提供依据。 相似文献
948.
Christine Stark Leo M. Condron Alison Stewart Hong J. Di Maureen O’Callaghan 《Biology and Fertility of Soils》2007,43(5):531-540
Because soil biota is influenced by a number of factors, including land use and management techniques, changing management
practices could have significant effects on the soil microbial properties and processes. An experiment was conducted to investigate
differences in soil microbiological properties caused by long- and short-term management practices. Intact monolith lysimeters
(0.2 m2 surface area) were taken from two sites of the same soil type that had been under long-term organic or conventional crop
management and were then subjected to the same 2.5-year crop rotation [winter barley (Hordeum vulgare L.), maize (Zea mais L.), lupin (Lupinus angustifolius L.), and rape (Brassica napus L. ssp. oleifera)] and two fertilizer regimes (following common organic and conventional practices). Soil samples were taken after crop harvest
and analyzed for microbial biomass C and N, microbial activity (fluorescein diacetate hydrolysis, arginine deaminase activity,
and dehydrogenase activity), and total C and N. The incorporation of the green manure stimulated growth and activity of the
microbial communities in soils of both management histories. Soil microbial properties did not show any differences between
organically and conventionally fertilized soils, indicating that crop rotation and plant type had a larger influence on the
microbial biomass and enzyme activities than fertilization. Initial differences in microbial biomass declined, while the effects
of farm management history were still evident in enzyme activities and total C and N. Links between enzyme activities and
microbial biomass C varied depending on treatment, indicating differences in microbial community composition. 相似文献
949.
Colin Southwell David Borchers Charles G. M. Paxton Louise Burt William de la Mare 《Journal of Agricultural, Biological & Environmental Statistics》2007,12(1):41-54
We use line transect detection functions together with generalized linear and additive models to estimate detection probability
when detection on the line (“g(0)”) may not be certain. The methods provide a flexible way of modeling detection probability
for independent observer surveys, and for investigating the effects of explanatory variables. Analysis of data from an aerial
survey of pack-ice seals produced g(0) estimates substantially below 1 for some observers (it varied from 0.80 to 0.98), demonstrated a fairly complex dependence
of detection probability on covariates, and showed negative correlation between observers’ search width and their g(0). In addition to illustrating the utility of generalized additive models for capturing the effect of covariates on detection
probability, the analysis suggests that detection functions may be sufficiently variable that use of g(0) correction factors obtained from other surveys would be inadvisable. We recommend that estimation of g(0) be considered for all aerial surveys; if g(0) is found to be very close to 1, estimation from subsequent surveys under the assumption that it is 1 may be reasonable,
but without any estimation of g(0), the assumption that it is 1 is a matter of faith. 相似文献
950.
沼液负压蒸发浓缩装置的设计与试验 总被引:2,自引:1,他引:2
为了解决沼液浓缩过程中有效成分流失的问题,采用低温负压蒸发浓缩的方法,结合沼液的理化性质,对沼液负压蒸发浓缩装置的主体部分(蒸发罐)和辅助设备(冷凝器、循环液槽、真空泵)分别进行了参数设计计算和设备选型,并在自制20 L负压蒸发浓缩装置上进行了系列试验。试验结果表明:当温度低于80℃时,沼液的有机质含量基本不变,蒸发温度高于80℃之后,有机质含量明显下降,80~100℃的变化率为9.4%;随着温度的升高,氮磷钾含量不断下降,氮含量流失最大,最大变化率为13%。蒸发浓缩后的沼液中有机质和氮磷钾含量随真空度的增大而升高;随着真空度的升高,沼液的蒸发温度逐渐降低,蒸发量不断增大,绝对真空度为0.025 MPa时,最低蒸发温度为67℃,蒸发量最高能达到8 324 m L/(m2·h),蒸发率为28.75%;绝对真空度维持在0.04 MPa到0.05 MPa之间,温度在75~80℃时,蒸发量能达到7 700 m L/(m2·h),蒸发率为26%左右。 相似文献