Computational Model of Soil Adhesion and Resistance for a Non-smooth Bulldozing Plate

Adhesive forces exist between soil and the surfaces of soil-engaging components; they increase working resistance and energy consumption. This paper tries to find an approach to reduce the adhesion and resistance of bulldozing plate. A simplified mechanical model of adhesion and resistance between soil and a non-smooth bulldozing plate is proposed. The interaction force between moist soil and a non-smooth bulldozing plate is analyzed. The pressure and friction distribution on the bulldozing plate are computed, and the anti-adhesive effect of a corrugated bulldozing plate is simulated numerically. Numerical results show that the wavy bulldozing plate achieves an effective drag reduction in moist soil. The optimal wavy shape of the corrugated bulldozing plate with the minimal resistance is designed. The basic principle of reducing soil adhesion of the non-smooth surface is discovered.     

DEM Simulation of Clod Crushing by Bionic Bulldozing Plate

Through evolving over millions of years, earthworm has developed the typical wavy body surface. The non-smooth surface shape can break the clods into small pieces, which is one of the important reasons to make earthworm move freely in soil. Based on engineering bionics, the non-smooth body surface of earthworm was regarded as the bionic prototype, and a bionic wavy plane bulldozing plate was designed. In order to analyze the clod crushing mechanism by the bionic bulldozing plate, the nonlinear mechanical model of contact between soil particles was established and the clod-crushing processes by the bionic bulldozing plate and the smooth bulldozing plate were simulated by Distinct Element Method (DEM). Simulation results indicate that the bionic bulldozing plate has stronger clod-crushing ability and can break much more clods than the smooth bulldozing plate can.     

Design Principles of the Non-smooth Surface of Bionic Plow Moldboard

1　IntroductionTransferringbiologyfunctiontoengineeringtech nology[1] isaprominentprogressintechnologicalfields ,whichenrichesthecontentofTRIZsystematicmethod .Thenon smoothsurfacesofthetypicalsoilan imalshavetheeffectsofreducingsoiladhesion ,whichhasbeenconvincedandgraduallyaccepted .Thebionicplowmoldboardisanappliedexampleofimitatingthecharacteristicsofsoilanimals’surfaceappearancesandpracticingtheBionicTheoryofNon SmoothSurface(TNSS) .ThebasisofTNSSisnon smoothsurfaceef fects[2 ,3] …     

Tangent Resistance of Soil on Moldboard and the Mechanism of Resistance Reduction of Bionic Moldboard

The tangent resistance on the interface of the soil-moldboard is an important component of the resistance to moving soil . We developed simplified mechanical models to analyze this resistance. We found that it is composed of two components, the frictional and adhesive resistances. These two components originate from the soil pore, which induced a capillary suction effect, and the soil-moldboard contact area produced tangent adhesive resistance. These two components varied differently with soil moisture. Thus we predicted that resistance reduction against soil exerted on the non-smooth bionic moldboard is mainly due to the elimination of capillary suction and the reduction of physical-chemical adsorption of soil.     

The Concept of Electroosmotically Driven Flow and Its Application to Biomimetics

1　IntroductionOneaimofthephysicsscienceresearchistodevel opfundamentalandportableconceptswhichhelpunitedifferentresearchfrontiers.Inthisrespect ,Helmholtz’selectricdoublelayer (DEL)theory ,whichwasdevel opedin 1879andrelatedtheelectricandflowparame tersforelectrokinetictransport ,isaseminal,havingprovidedaframeworkforinterpretingawiderangeofelectrokineticphenomena .DespitethesimplicityoftheEDLtheory ,whichwewilldescribeindetail,ithasprovidedachallengeformathematicianstounderstanditsimplic…     

陕西渭北旱塬土壤—植物—大气连续体中水分运转规律的研究──Ⅴ．田间冬小麦土壤—叶片途径水运转阻力研究

采用Ｍｉｓｈｉｏ和Ｙｏｋｏｉ（１９９１）的方法,在水分运转阻力短期内（如几个小时）恒定不变的假设下,研究了田间冬小麦土壤—叶片途径水分运转阻力．结果表明,一天中,当气孔没有“午休”现象或“午休”现象不明显时,冬小麦土壤—叶片途径水分运转阻力在白天保持恒定,到夜晚则明显增大;当气孔“午休”现象较明显时,冬小麦土壤—叶片途径水分运转阻力在气孔“午休”期间和夜晚明显增大,其余时间基本保持恒定．夜间和气孔“午休”期间阻力增大的原因不确定．土壤干旱条件下冬小麦土壤—叶片途径水运转阻力显著大于土壤湿润条件下,表明水运转阻力与植物抗旱性有关．土壤干旱条件下施肥处理冬小麦土壤—叶片途径水运转阻力显著大于不施肥处理,而土壤湿润条件下显著小于不施肥处理,表明施肥对植物具有调节作用,使之更好地适应干旱环境．     

Response of biological soil crusts to raindrop erosivity and underlying influences in the hilly Loess Plateau region,China

Biological soil crusts (biocrusts) are ubiquitous living covers in arid and semiarid regions, playing a critical role in soil erosion control in semiarid regions. So far, research separating the multiple mechanisms of erosion control by biocrusts has been limited. It was problematic to link the influence of biocrusts to existing erosion models. In the present study, the response of biocrusts of different successional stages to raindrop erosivity and underlying influences was investigated. Using single drop simulated rainfall, the erosion controlling capacities of biocrusts were analyzed from an energetic perspective. The results showed that biocrusts caused a dramatic improvement of soil erosion resistance, which depended on species composition and increased considerably with higher succession stages. While the accumulated raindrop kinetic energy sustained by dark cyanobacterial crusts was 0.93 J (~15 times higher than that of bare soil), that of 60 % moss covered crusts reached values up to 20.18 J (~342 times higher than that of bare soil) and for 80 % moss covered crusts even 24.59 J were measured. Besides the composition and successional stages, the resistance of biocrusts to raindrop erosivity was related to the substrate soil moisture, soil texture, slope gradients and seasonal variation. The accumulated raindrop kinetic energy measured for cyanobacterial crusts was highest on silty, followed by loamy and sandy soil. For moss-dominated crusts raindrop kinetic energy was highest on sandy, followed by silty and loamy soil. Dry biocrust samples reached significantly higher accumulated raindrop kinetic energies compared to moist biocrusts, whereas the moisture content within moist crusts did not have a significant influence. Erosion resistance increased significantly with higher slope gradients. The resistance capacities of biocrusts during monsoon and post-monsoon were significantly higher than these of pre-monsoon biocrusts. Our results suggest that the influence of biocrusts can be included into erosion models from an energy point of view. The raindrop kinetic energy resistance capacity provides a potential bridge between biocrust succession and soil erodibility in commonly used erosion models.     

Effects of salinity on microbial tolerance to drying and rewetting

Soil salinity and fluctuations in soil matric potential are stressors for soil microorganisms which, in turn, may affect soil organic matter turnover. In response to salinity and low soil water content, many microorganisms accumulate osmolytes. Therefore, it is conceivable that microorganisms in saline soils are more tolerant to drying and rewetting (DRW) stress than those in non-saline soils. An experiment was carried out with three different salinity levels: electrical conductivity (EC_1:5) 0, 2 and 4 dS m^?1 (EC0, EC2, EC4), and two water treatments: a constantly moist control or two DRW cycles. Respiration as an indicator of microbial activity was measured throughout the 59 days of incubation. At the end of the second dry period (day 35) and at the end of the following moist incubation (day 59), microbial biomass and microbial community structure were determined by phospholipid fatty acid (PLFA) analysis. Increasing salinity decreased microbial activity but did not affect its resistance to DRW. On day 59, cumulative respiration decreased in the order EC0 > EC2 > EC4 with no differences between water treatments. Fungal biomass was negatively affected by salinity at the end of the experiment, while bacterial biomass was unaffected. Microbial community structure in moist treatments differed between salinity levels, with EC4 influencing microbial community structure earlier than EC2. The resistance of microbial communities to DRW stress was salt level dependent; only beyond a critical salinity level adaptation to salt stress was able to reduce the impact of water stress on microbial community structure.     

CaCl2 extractable N fractions and K2SO4 extractable N released on fumigation as affected by green manure mineralization and soil texture

Repeated mild wet-dry cycles were imposed on a sandy loam to accelerate the mineralization of organic C involved in stabilising macro-aggregates. Soil maintained continually moist (control soil) was compared to that subjected to a series of 6 wet-dry cycles. Two patterns of rewetting and drying were investigated: (1) incubated dry at 25°C for six days between each wet-dry cycle (dry-incubated), or (ii) incubated moist for six days at 25°C between each cycle (moist-incubated). Changes in the proportion of >2 mm, 1–2 mm, 0.5–1 mm and 0.25–0.5 mm aggregates, and carbohydrate C extracted by hot-water or hot-1.5 M H₂SO₄, were measured after each wet-dry cycle, or weekly in the continuously moist control soil. Respiration rates (CO₂ efflux) were measured during the incubation of the moist soil between the wet-dry cycles and compared with the continually-moist control soil.The wet-dry treatments did not increase soil respiration in soil after re-wetting compared to soil kept continually moist and incubated for the same period of time. Despite this, the treatments caused changes in the amounts of acid- and water-extractable carbohydrate C fractions and substantial changes in aggregation. Macro-aggregation and the proportion of soil in each fraction did not change in the soil maintained continuously-moist for 6 weeks (control). However, effects of the two wet-dry treatments on total macro-aggregation were similar to those in the >2 mm, 1–2 mm and 0.25–0.5 mm aggregate fractions: there was a rapid decline in aggregation by 48–65% over the first two cycles, a sharp recovery to 78–100% of the initial aggregation after three cycles, and a further decline after 4–6 cycles.The resistance of organic C mineralization to mild wet-dry cycles confirmed that the organic C in this soil is very stable and resistant to decomposition. Despite aggregates being disrupted, the organic C stabilising these aggregates was resistant to decomposition as determined by CO₂ efflux. When soil was re-moistened and incubated to allow microbial re-colonization, aggregation was similar to that in the soil where microbial re-colonization was limited by rapid drying treatments. Short term changes in the aggregation of this soil appear to be dominated by chemical and/or physical processes.     

Soil Effects on Forest Structure and Diversity in a Moist and a Dry Tropical Forest

Soil characteristics are important drivers of variation in wet tropical forest structure and diversity, but few studies have evaluated these relationships in drier forest types. Using tree and soil data from 48 and 32 1 ha plots, respectively, in a Bolivian moist and dry forest, we asked how soil conditions affect forest structure and diversity within each of the two forest types. After correcting for spatial effects, soil‐vegetation relationships differed between the dry and the moist forest, being strongest in the dry forest. Furthermore, we hypothesized that soil nutrients would play a more important role in the moist forest than in the dry forest because vegetation in the moist forest is less constrained by water availability and thus can show its full potential response to soil fertility. However, contrary to our expectations, we found that soil fertility explained a larger number of forest variables in the dry forest (50 percent) than in the moist forest (17 percent). Shannon diversity declined with soil fertility at both sites, probably because the most dominant, shade‐tolerant species strongly increased in abundance as soil fertility increased.     

Influence of Dimensions of UHMW-PE Protuberances on Sliding Resistance and Normal Adhesion of Bangkok Clay Soil to Biomimetic Plates

A number of investigations into application of polymers for macro-morphological modification of tool surface have been carried out. These researches, with extensive stress on convex or domed protuberations as one of the widely used construction units, have tried to harness benefits from using polymers in agriculture. Ultra high molecular weight polyethylene （UHMW-PE） has proved an emerging polymer in its application to reduce soil adhesion. This research was conducted to study the effect of shape （flat, semi-spherical, semi-oblate, semi short-prolate and semi long-prolate） and dimensions （base diameter and dome height） on sliding resistance and normal adhesion of biomimetic plates. To incorporate both shape and size, a dimensionless ratio of height to diameter （HDR） was introduced to characterize the effect of construction unit＇s physique. Experiments were conducted in Bangkok clay soil with dry （ 19.8% d.b.）, sticky （36.9% d.b.） and flooded （60.1% d.b.） soil conditions respectively. Soil at sticky limit exhibited the highest sliding resistance （77.8 N） and normal adhesion （3 kPa to 7 kPa）, whereas these values were 61.7 N and 〈0.2 kPa in dry, and 53.7 N and 0.5 kPa to 1.5 kPa in flooded soil conditions. Protuberances with HDR ≤ 0.5 lowered sliding resistance by 10% - 30% and the same reduced normal adhesion by 10% - 60%. The amount of reduction in both sliding resistance and normal adhesion was higher in flooded soil. Lighter normal loads obviously produced lesser resistance and adhesion.     

Actomyosin promotes cell plate alignment and late lateral expansion in <Emphasis Type="Italic">Tradescantia</Emphasis> stamen hair cells

Cytokinesis in higher-plant cells involves the formation of a cell plate in the interzone between the separating chromatids. The process is directed by the phragmoplast, an array of microtubules, actin filaments, and membranous elements. To determine if the role of actin in cytokinesis is dependent on myosin, we treated stamen hair cells of Tradescantia virginiana L. with 2,3-butanedione monoxime (BDM), an inhibitor of myosin ATPase and ML-7, a specific inhibitor of myosin light-chain kinase. Treatment with BDM resulted in a tilted cytokinetic apparatus during early initiation and a wavy cell plate with curved phragmoplasts during late lateral expansion. Treatment with ML-7 also resulted in inefficient late lateral expansion of the cell plate, with effects ranging from slower expansion to complete inhibition. Taken together, these results implicate myosin in the control of cell plate expansion and alignment.     

木麻黄抗逆性研究进展

木麻黄(Casuarina equisetifolia)是热带、亚热带常绿乔木, 天然生长于滨海疏松沙土中, 为多用途速生树种。长期生长在恶劣的沿海气候和环境中使其具有较强的抗盐、抗风、耐瘠薄、抗涝能力。木麻黄已广泛种植于我国东南沿海, 主要用于防风固沙、盐碱地改良和干旱地区绿化等, 在防御沿海自然灾害、改善生态环境方面发挥了巨大作用。杂交和盐碱地露地育苗等技术使木麻黄的抗寒性 也得到了较大提高。本文就近年来木麻黄抗非生物胁迫的研究进行了综述, 旨在为合理开发和利用木麻黄资源提供参考依据。     

Eap1p, an adhesin that mediates Candida albicans biofilm formation in vitro and in vivo

Candida albicans is the leading cause of systemic fungal infections in immunocompromised humans. The ability to form biofilms on surfaces in the host or on implanted medical devices enhances C. albicans virulence, leading to antimicrobial resistance and providing a reservoir for infection. Biofilm formation is a complex multicellular process consisting of cell adhesion, cell growth, morphogenic switching between yeast form and filamentous states, and quorum sensing. Here we describe the role of the C. albicans EAP1 gene, which encodes a glycosylphosphatidylinositol-anchored, glucan-cross-linked cell wall protein, in adhesion and biofilm formation in vitro and in vivo. Deleting EAP1 reduced cell adhesion to polystyrene and epithelial cells in a gene dosage-dependent manner. Furthermore, EAP1 expression was required for C. albicans biofilm formation in an in vitro parallel plate flow chamber model and in an in vivo rat central venous catheter model. EAP1 expression was upregulated in biofilm-associated cells in vitro and in vivo. Our results illustrate an association between Eap1p-mediated adhesion and biofilm formation in vitro and in vivo.     

Encystation in Acanthamoeba castellanii: development of biocide resistance

Since the early 1960s, axenic culture and the development of procedures for the induction of encystation have made Acanthamoeba spp. superb experimental systems for studies of cell biology and differentiation. More recently, since their roles as human pathogens causing keratitis and encephalitis have become widely recognized, it has become urgent to understand the parameters that determine differentiation, as cysts are much more resistant to biocides than are the trophozoites. Viability of trophozoites of the soil amoeba Acanthamoeba castellanii (Neff), is conveniently measured by its ability to form plaques on a lawn of Escherichia coli. Use of confocal laser scanning microscopy with Calcofluor white, Congo Red or the anionic oxonol dye, DiBAC4(3) or flow cytometry with propidium iodide diacetate and fluorescein or oxonol provides more rapid assessment. For cysts, the plaque method is still the best, because dye exclusion does not necessarily indicate viability and therefore the plate count method has been used to study the sequence of development of biocide resistance during the differentiation process. After two hours, resistance to HCl was apparent. Polyhexamethylene biguanide, benzalkonium chloride, propamidine isethionate, pentamidine isethionate, dibromopropamine isethionate, and H2O2 and moist heat, all lost effectiveness at between 14 and 24 h after trophozoites were inoculated into encystation media. Chlorhexidine diacetate resistance was observed at between 24 and 36 h. The molecular biology and biochemistry of the modifications that underlie these changes are now being investigated.     

Tribology of the root cap in maize (Zea mays) and peas (Pisum sativum)

Frictional resistance to a penetrating body can account for more than 80% of the total resistance to penetration of soil. We measured the frictional resistance between growing root caps of maize and pea and ground and smooth glass surfaces, which was linearly correlated to load, allowing calculation of the coefficient of kinetic friction and adhesion. Coefficients of kinetic friction between the root caps and the ground and smooth glass surfaces were approximately 0.04 and 0.02, respectively, the first measurements of the frictional properties of root tips at rates approaching those of root elongation, and an order of magnitude smaller than those previously reported. Results suggest that roots are well designed for penetrating soil, and encounter only small frictional resistance on the root cap. These data provide important parameters for modelling soil stresses and deformation around growing root tips.     

云南20种蕨类植物叶表皮微形态特征研究

利用光学显微镜对云南20种不同科、属的蕨类植物的叶表皮形态进行了观察和研究。结果表明：它们的叶片表面存在不同的附属物,而有的种类无附属物;20种蕨类植物共具8种气孔器类型(极细胞型、腋下细胞型、辐射状细胞型、双不等细胞型、无规则四细胞型、共环极细胞型、聚腋下细胞型和不规则型), 它们在气孔器组成上具多型现象,气孔均为下生型,分布方式及大小多样;叶表皮细胞的微形态在科属间表现出一定的差异,主要有不规则型、多边型或规则条状,表皮细胞垂周壁呈波纹状、深波状或波浪状。上述研究结果为蕨类植物的系统分类及演化提供依据。     

Effects of biochar amendment on the sorption and degradation of atrazine in different soils

ABSTRACT

Sugarcane top-derived biochar was added to an alluvial soil, a moist soil and a paddy soil at the rate of 0.2% and 0.5% (w/w). After the addition of 0.2% and 0.5% biochar, the sorption coefficients (K_d) of atrazine (Ce = 10 mg L^?1) were increased by 26.97% and 79.58%, respectively, in the moist soil with a low level of total organic carbon (TOC), while it increased by 31.43% and 60.06%, respectively, in the paddy soil with a high TOC content. The half-time persistence values of atrazine in the alluvial soil, moist soil and paddy soil were 28.18, 23.74 and 39.84 d, respectively. In the 0.2% biochar amended soils, the corresponding half-times of atrazine for the alluvial soil, moist soil and paddy soil were extended by 10.33, 11.81 and 1.42 d, and they were prolonged by 16.83, 17.52 and 14.74 d, respectively, in the 0.5% biochar amended soils. Atrazine degradation products (deisopropylatrazine and desethylatrazine) decreased after they accumulated to 3.2 and 1 mg kg^?1, respectively. Generally, increasing sorption was accompanied by decreasing degradation of atrazine which is found in biochar-amended soils.     

Litter decomposition in moist acidic and non-acidic tundra with different glacial histories

Plant species composition is a potentially important source of variation in soil processes, including decomposition rates. We compared litter decomposition in two common and compositionally distinct tundra vegetation types in the northern foothills of the Brooks Range, Alaska: moist acidic tundra (soil pH 3–4), which occurs primarily on older landscapes, and moist non-acidic tundra (soil pH 6–7), which occurs primarily on landscapes with a more recent history of glaciation and has higher graminoid and forb abundance and lower woody shrub abundance than acidic tundra. To separate the influence of plant community composition from that of the soil environment, we decomposed the same nine substrates at a moist acidic and a moist non-acidic site located less than 2 km apart. Substrates included leaf litter of the dominant species in each growth form (graminoid, deciduous shrub, evergreen shrub, forb, moss) as well as woody stems of the deciduous shrub Betula nana. Then, we estimated above-ground community-level decomposition by weighting the decay rate of each species in the community by its proportional contribution to overall above-ground net primary production (ANPP). In contrast to our expectations, community-level decomposition rates estimated using the site-average decay rate for each substrate were similar between the two sites, likely because growth forms differed little in their leaf litter decay. By contrast, when site-specific decay rates were used to estimate community-level decomposition, it was nearly twice as fast at the older, moist acidic tundra site because most substrates decayed faster at that site, indicating a more favorable environment for decomposition in acidic tundra. Site differences in soil moisture and temperature could not explain site differences in decomposition. However, higher soil N availability at the moist acidic tundra may have contributed to faster decomposition since, in a separate experiment, fertilization with N stimulated decomposition of a common substrate at both sites. In addition, lower pH in acidic tundra may promote greater abundance of soil fungi, perhaps explaining faster decomposition rates at that site. In summary, the large differences in plant species composition between moist acidic and non-acidic tundra are likely to not contribute to site differences in decomposition. Nevertheless, decomposition is much more rapid in moist acidic tundra. Thus, landscape age and associated differences in soil pH and nutrient availability are important sources of variation in decomposition rate in upland Alaskan tundra.     

Moist-Soil Plants as Ecohydrologic Indicators for Recovering the Flood Pulse in the Illinois River

The hydrologic regime of the Illinois River has been substantially altered by locks and dams, floodplain levees, water diversion, and development of the watershed over the past 100 years. The natural flood pulse, a fundamental rhythm to which the plants and animals of both the river and its floodplain had adapted, has been disrupted. State, federal, and non‐governmental organizations are currently trying to naturalize the Illinois floodplain‐river system. Little, however, is known about how to recover those elements of the flood pulse essential to the native biota. In this study we propose moist‐soil plants, whose life history is dependent upon flood pulsing, as ecohydrologic indicators of the flood pulse. We explain how moist‐soil plants are supported by the natural flood pulse and present a conceptual framework that links the flooding regimes of the river and the reproductive success of the plants. Successful germination and full growth of moist‐soil plants can be a useful indicator for optimum naturalization of flood regimes. The framework also shows how the interdisciplinary linkages between hydrology, ecology, and spatial analysis assist in predicting, measuring, and comparing consequences of alternative naturalization scenarios. A new ecohydrologic parameter, lowest elevation for successful moist‐soil plant production, is presented.