Soil salinity and pH in Japanese mangrove forests and growth of cultivated mangrove plants in different soil conditions

Soil conditions of mangrove forests in southern Japan were found to correlate largely with zonal distributions of the species.Kandelia candel grew in soils with low salinity and low pH,Avicennia marina, Rhizophora stylosa andSonneratia alba in soils with high salinity and high pH, andBruguiera gymnorrhiza in soil with a wide range of pH but limited range of salinity.Lumnitzera racemosa colonized soil with a wide range of pH and medium salinity. Seedlings ofKandelia candel, Bruguiera gymnorrhiza andRhizophora stylosa were planted in soils with differing salinity and pH. Optimum seedling growth ofKandelia, Bruguiera andRhizophora occurred when plants were cultivated in soils similar to those of their natural habitats, suggesting that growth of mangrove species and their zonal distributions were regulated by salinity and soil pH.     

Spatial distribution of pH and organic matter in urban soils and its implications on site-specific land uses in Xuzhou,China

The spatial variation of soil pH and soil organic matter (SOM) in the urban area of Xuzhou, China, was investigated in this study. Conventional statistics, geostatistics, and a geographical information system (GIS) were used to produce spatial distribution maps and to provide information about land use types. A total of 172 soil samples were collected based on grid method in the study area. Soil pH ranged from 6.47 to 8.48, with an average of 7.62. SOM content was very variable, ranging from 3.51 g/kg to 17.12 g/kg, with an average of 8.26 g/kg. Soil pH followed a normal distribution, while SOM followed a log-normal distribution. The results of semi-variograms indicated that soil pH and SOM had strong (21%) and moderate (44%) spatial dependence, respectively. The variogram model was spherical for soil pH and exponential for SOM. The spatial distribution maps were achieved using kriging interpolation. The high pH and high SOM tended to occur in the mixed forest land cover areas such as those in the southwestern part of the urban area, while the low values were found in the eastern and the northern parts, probably due to the effect of industrial and human activities. In the central urban area, the soil pH was low, but the SOM content was high, which is mainly attributed to the disturbance of regional resident activities and urban transportation. Furthermore, anthropogenic organic particles are possible sources of organic matter after entering the soil ecosystem in urban areas. These maps provide useful information for urban planning and environmental management.     

典型岩溶洼地土壤水分的空间分布及影响因素

在桂西北典型岩溶洼地的旱季和雨季,用地统计学结合GIS方法研究了洼地表层(0—16cm)土壤水分的空间分布特征及其影响因素。结果表明:土壤含水量受前期降雨量的影响,且旱季土壤水分对降雨量的反应较雨季敏感。土壤水分均呈中等变异且变异系数随着平均含水量的增加而减少。土壤水分的半方差参数显示土壤水分空间变异及其主导因素随旱、雨季而不同。此外,不同取样区域及取样时段内土壤含水量高低差别明显,分布格局及空间变异程度各异,这主要与当地环境和人为因素的综合影响有关。旱、雨季土壤水分均与前期降雨导致的土壤平均含水量变化呈相反趋势,且不同土地利用方式下的土壤含水量不同。土壤含水量还与土壤有机碳含量呈显著正相关,此外,地势及裸岩率也是造成洼地土壤水分变异及其分布差异的重要因素。下一步应根据旱季和雨季土壤水分分布及影响因素的差异,在岩溶洼地采取有针对性地土壤水资源利用及其水分管理策略。     

Divergent response of seasonally dry tropical vegetation to climatic variations in dry and wet seasons

Interannual variations of photosynthesis in tropical seasonally dry vegetation are one of the dominant drivers to interannual variations of atmospheric CO₂ growth rate. Yet, the seasonal differences in the response of photosynthesis to climate variations in these ecosystems remain poorly understood. Here using Normalized Difference Vegetation Index (NDVI), we explored the response of photosynthesis of seasonally dry tropical vegetation to climatic variations in the dry and the wet seasons during the past three decades. We found significant (p < 0.01) differences between dry and wet seasons in the interannual response of photosynthesis to temperature (γ^int) and to precipitation (δ^int). γ^int is ~1% °C^?1 more negative and δ^int is ~8% 100 mm^?1 more positive in the dry season than in the wet season. Further analyses show that the seasonal difference in γ^int can be explained by background moisture and temperature conditions. Positive γ^int occurred in wet season where mean temperature is lower than 27°C and precipitation is at least 60 mm larger than potential evapotranspiration. Two widely used Gross Primary Productivity (GPP) estimates (empirical modeling by machine‐learning algorithm applied to flux tower measurements, and nine process‐based carbon cycle models) were examined for the GPP–climate relationship over wet and dry seasons. The GPP derived from empirical modeling can partly reproduce the divergence of γ^int, while most process models cannot. The overestimate by process models on negative impacts by warmer temperature during the wet season highlights the shortcomings of current carbon cycle models in representing interactive impacts of temperature and moisture on photosynthesis. Improving representations on soil water uptake, leaf temperature, nitrogen cycling, and soil moisture may help improve modeling skills in reproducing seasonal differences of photosynthesis–climate relationship and thus the projection for impacts of climate change on tropical carbon cycle.     

Adaptation of soil bacterial communities to prevailing pH in different soils

Abstract: The bacterial community response to pH was studied for 16 soils with pH(H₂O) ranging between 4 and 8 by measuring thymidine incorporation into bacteria extracted from the soil into a solution using homogenization-centrifugation. The pH of the bacterial solution was altered to six different values with dilute sulfuric acid or different buffers before measuring incorporation. The resulting pH response curve for thymidine incorporation was used to compare bacterial communities from the different soils. There was a correlation between optimum pH for thymidine incorporation and the soil pH(H₂O). Even bacterial communities from acid soils had optima corresponding to the soil pH, indicating that they were adapted to these conditions. Thymidine incorporation was also compared with leucine incorporation for some soils. The leucine to thymidine incorporation ratio was constant over the tested pH interval when incorporation values were adjusted for isotope dilution. A good correlation was found between the scores along the first component (explaining 80% of the variation) and soil pH ( r ² = 0.85), if principal component analysis of the pH response curves for thymidine incorporation was used. The pH response curves differed most for the extreme pH values used, and a linear relationship was found between the logarithm of the ratio of thymidine incorporation at pH 4.3 to incorporation at pH 8.2 and the soil pH ( r ² = 0.86). Thus, a simplified technique using only two pH values, when measuring the thymidine incorporation, could be used to compare the response to pH of bacterial communities.     

Interactions between aluminium,phosphorus and pH in the response of barley to soil acidity

Summary Two acid soils showing different Al solubility as a function of pH were limed to a range of pH values (in 10^–2 M CaCl₂) between 4.1 and 5.6. The apparent critical pH for the growth of barley in pots was 0.25 lower in the soil showing lower Al solubility. The addition of phosphate reduced exchangeable and soluble Al in the soils, and lowered the apparent critical pH by 0.35 while maintaining the difference between the soils. The Al concentration at the critical pH, measured after cropping to take account of the treatment effects on soil Al, also varied with soil and with phosphate addition. These apparent critical values of both pH and soluble Al varied linearly with available phosphate, over the range 18 to 73 mg P/kg soil, as follows: pH from 4.9 to 4.3; soluble Al, from 0.010 mM to 0.056 mM; and the soluble Ca/Al mole ratio, from 1270 to 214.     

冬小麦干物质在各器官中的累积和分配规律研究

为修正冬小麦生长模型中的干物质分配,通过田间试验,对冬小麦干物质累积和在不同器官中的分配进行了描述。并且在此基础上结合文献资料,对冬小麦光合产物在各器官中的分配和转移系数的计算方法进行了探讨,分析了两者随相对发育阶段（RDS）的变化规律,并建立了函数表。同时运用试验资料进行了实地验证,取得较好的效果。     

Biotic communities of freshwater marshes and mangroves in relation to saltwater incursions: implications for wetland regulation

An ecosystem-level study was conducted in the Guandu wetlands insubtropical coastal Taiwan to examine how salinity influences the abundance,diversity, and structure of biotic communities. We surveyed eight permanentstudy sites, spanning freshwater marshes, to the gate on the dyke, andmesohaline mangroves representing a gradient of the extent of saltwaterincursions. Analyses of abiotic variables showed that salinity was the primarydetermining factor for discriminating habitat types in the wetlands, butcommunities differed in their sensitivity to salinity. The composition of plantand insect communities was most affected by the salinity gradient, suggestingthe utility of these communities for ecological monitoring of saltwaterincursions. However, spatial changes in communities at higher trophic levels,including macrobenthos, mollusks, fish, and birds, could not be explained simplyby the salinity gradient. Instead, changes in these communities were morerelevant to the composition of other biotic communities. Our results show thatspecies richness and diversity of plant communities were higher in the marshesthan in the mangroves. Nevertheless, insect communities censused in themangroves had higher diversity, despite lower abundance and species richness.Macrobenthos surveyed in the mangroves showed higher biomass and number of taxa.Mollusks and fish were also more abundant at sites near the gate compared to themarsh sites. This suggests that maintaining a tidal flux by means of gateregulation is necessary for conserving the spatial heterogeneity andbiodiversity of coastal wetlands.     

Cover distributions of vascular plants in relation to soil chemistry and soil depth in a granite rock ecosystem

The variability in the cover distribution of vascular plants, accounted for by soil chemical properties and soil depth, on a granite slope with shallow autochtonous soil in southeast Sweden was evaluated using multivariate statistical regression and graphical methods. Soil acidity and soil depth were, to an often high degree, able to account for the variability in the distributions of the ca. 30 most frequent species, including Rumex acetosella, Vincetoxicum hirundinaria, Filipendula vulgaris, Satureja acinos, Geranium columbinum, Silene rupestris, and Arenaria serpyllifolia. The best expression of soil acidity was pH-KCl, though exchangeable Ca and Al were also important measures of the soil-plant relationships. The Ca:Al ratio was inferior in this respect. Also exchangeable or acid soluble phosphate was significantly related to the distribution of several species, whereas soil organic matter content was almost unrelated.     

五种荒漠灌木群落土壤有机碳垂直分布及其与根系分布的关系

研究土壤有机碳与根系分布之间关系对评估碳储量和固碳潜力具有重要意义,而我国荒漠区灌木群落土壤有机碳与植物根系之间的关系尚不清楚。本研究选取深根性表层型灌木(表层根系生物量最大)梭梭(Haloxylon ammodendro)和中间锦鸡儿(Caragana intermedia)、深根性非表层型(表层根系生物量不是最大)灌木白刺(Nitratia tangutorum)、浅根性表层型灌木红砂(Reaumuria songarica)及浅根性非表层型灌木霸王(Sarcozygium xanthoxylon)为优势种的5种荒漠灌木群落为研究对象,测定100 cm深度内不同层次根系生物量及土壤有机碳含量,探讨灌木群落土壤有机碳的垂直分布格局及其与根系之间的关系。结果显示:(1)0~100 cm土壤有机碳密度与群落0~20 cm根系生物量碳密度显著正相关,与其他层次或累积深度不显著相关;(2)梭梭群落0~100 cm土壤有机碳密度显著低于与其他4个群落(P0.01),其他4个群落无显著差异(P0.05);(3)优势种为表层型的梭梭、中间锦鸡儿和红砂群落土壤有机碳密度与群落及优势种根系变化趋势一致,优势种为浅根性非表层型的霸王群落仅表层40 cm土壤有机碳与优势种灌木根系分布规律一致,优势种为深根性非表层型的白刺群落土壤有机碳与优势种根系分布规律一致。本研究表明,荒漠灌木群落0~100 cm土壤有机碳储量与群落0~20 cm根系生物量显著相关,群落优势种根系分布类型是影响土壤有机碳垂直分布格局的重要因素。     

水稻根系生长及其对土壤紧密度的反应

采用筒栽方法研究了杂交稻汕优63和65002在分蘖期,穗分化期,开花期和成熟期根系生长量和垂直分布以及开花期土壤容重对根系生长和分布的影响,结果表明,根系生长量以开花期最高,开花后下降,随生育进展,深层根系（20-45cm)比例提高,分蘖期到穗 分化期是根系重量增长最快,且根系向下生长的主要时期,随耕层以下土壤容重提高,根系生长量下降,同时深层根系比例下降。     

Short-term dynamics of culturable bacteria in a soil amended with biotransformed dry olive residue

Dry olive residue (DOR) transformation by wood decomposing basidiomycetes (e.g. Coriolopsis floccosa) is a possible strategy for eliminating the liabilities related to the use of olive oil industry waste as an organic soil amendment. The effects of organic fertilization with DOR on the culturable soil microbiota are largely unknown. Therefore, the objectives of this study were to measure the short-term effects of DOR and C. floccosa-transformed DOR on the culturable bacterial soil community, while at the same time documenting the bacterial diversity of an agronomic soil in the southeastern Iberian Peninsula. The control soil was compared with the same soil treated with DOR and with C. floccosa-transformed DOR for 0, 30 and 60 days. Impact was measured from total viable cells and CFU counts, as well as the isolation and characterization of 900 strains by fatty acid methyl ester profiles and 16S rRNA partial sequencing. The bacterial diversity was distributed between Actinobacteria, Alphaproteobacteria, Gammaproteobacteria, Betaproteobacteria, Bacilli, Sphingobacteria and Cytophagia. Analysis of the treatments and controls demonstrated that soil amendment with untransformed DOR produced important changes in bacterial density and diversity. However, when C. floccosa-transformed DOR was applied, bacterial proliferation was observed but bacterial diversity was less affected, and the distribution of microorganisms was more similar to the unamended soil.     

RAPD and ISSR marker mediated genetic polymorphism of two mangroves Bruguiera gymnorrhiza and Heritiera fomes from Indian Sundarbans in relation to their sustainability

Physiology and Molecular Biology of Plants - Increased salinity distresses some key species severely in Indian Sundarbans. Geomorphic characteristics coupled with demographic obligations have...     

Phytoavailability of zirconium in relation to its initial added form and soil characteristics

The various uses of zirconium (Zr) in chemical and nuclear industries generate a potential risk of environmental contamination by this element. This study was performed on two agricultural soils, an acidic soil (A) and a clayey calcareous soil (B), collected in the Meuse/Haute Marne experimental site of the French National Agency for radioactive waste management (Andra). Distribution coefficients (K _d), defined as the ratio of Zr concentration in the solid phase (mol/kg) to Zr concentration in the solution (mol/l), were obtained for both soils. Their high values (6,000 < K _d < 30,000 l/kg) suggest a rapid and strong retention of Zr on the soil constituents. Chemical extractions (0.01 M CaCl₂, Calcium chloride, 0.005 M DTPA, Diethylene Triamine Penta Acetic acid, and 0.1 M NaPP, Sodium Pyrophosphate) showed that organic matter had a high affinity for the added Zr. Soil–plant transfer experiments showed low plant uptake. A significant absorption of Zr was, however, observed for the two studied plants, tomato (Lycopersicon esculentum L. cv. St. Pierre) and pea (Pisum sativum L. cv. “express”). For the most available forms of Zr (acetate and oxychloride), concentrations reached from 8 to 57 mg Zr/kg dry weight of roots. Zr is mainly accumulated in plant roots and is more absorbed by tomato than by pea. Zr bound to root cell walls (i.e. apoplastic Zr) concentrations, determined by HCl extraction, are significantly much lower than root absorbed Zr concentrations. Transfer to roots seemed to be more effective in the acidic soil and was strongly dependant on Zr added form.     

黄土丘陵区紫花苜蓿生长与土壤水分变化

研究了黄土丘陵区紫花苜蓿生物量变化规律和土壤水分过耗与恢复特征.结果表明,紫花苜蓿在退耕地生长年限一般为10年,生长的高峰期为第4年～第5年,到第6年,由于土壤水分过耗严重,生物量开始逐年下降,草地开始衰败.紫花苜蓿茎叶生物量的垂直变化,在距地面0～35cm之间,茎生物量远大于叶生物量,茎叶比为1.7:1;在40cm高时茎叶比相等,在45～90cm之间叶生物量远大于茎生物量,叶茎比为1.42:1.紫花苜蓿土壤干层在生长的前两年不甚明显,随着生长年限的延长,干层厚度不断增大,由第3年的110cm扩大到第7年的260cm,含水量仅为4.6%～6.2%,土壤水分严重亏缺.紫花苜蓿退化草地土壤水分的自然恢复过程一般需5年,且随着恢复年限的延长,土壤水分逐年提高.     

Dynamic floristic changes of Swedish beech forest in relation to soil acidity and stand management

This study reports dynamic changes in the beech forest vegetation during one decade, using 95 permanent observation areas representing a wide variety of soils and management regimes. Current soil acidification, including decreasing pH and base cation pools, increasing solubility of toxic elements and increasing deposition of N, as well as recent changes in the beech forest management have created good conditions for the study. Most species of vascular plants increased their frequencies during the 1980's. However, there were several notable exceptions, in particularGalium odoratum, Viola riviniana/reichenbachiana, Polygonatum multiflorum, andMercurialis perennis. These species, demanding a comparatively low soil acidity for survival, are distinctly disfavoured by the long-term soil changes in the forests, which seem to have approached or exceeded their limits of existence in many sites. With most other species, differences in management regimes between the beginning and the end of the observation period were more important to the frequency changes. Sensitive to heavy thinning of the stands were, e.g.Oxalis acetosella, Lamium galeobdolon andMelica uniflora, favoured by thinning wereStellaria nemorum, Carex pilulifera, Milium effusum and an appreciable number of more ephemeral species normally occurring in clear-cut areas or otherwise open land, e.g.,Rubus idaeus, Galeopsis tetrahit, Athyrium filix-femina, Juncus effusus, Agrostic capillaris, Veronica officinalis, Urtica dioica, andMoehringia trinervia. Saplings of woody plants usually also became more frequent during the 1980's.     

Influence of pH on Cd and Cu uptake, distribution and their effect on nitrate reductase activity in cucumber (Cucumis sativus L.) seedling roots

Influence of different pH solutions (5.0 and 7.0) on Cu²⁺ and Cd²⁺ absorption and distribution in root cells as well as effects of these metals on nitrate reductase activity (NR) in roots of cucumber seedlings were estimated. The absorption of Cu and Cd by roots measured as metal depletion in uptake solution was similar, both metal absorption was independent of the pH of solution. However, after rinsing of roots in distilled water (30 minutes), more Cu than Cd was found in protoplasts of root cells. More Cu was measured in all cell fractions when Cu was uptaken from pH 5.0 than from 7.0. The nitrate reductase activity after one hour of metal treatments was drastically decreased by Cu. The strongest reduction of enzyme activity was observed in roots treated with Cu in buffer with pH 5.0. Influence of Cd on the enzyme activity was weaker and was independent of the pH of solution. Lower concentration of Cd in solution (20 μM) increased NR activity. The data obtained prove the higher mobility of Cu than Cd into the cells of root. The mobility of Cu depends on pH of solution. Cu ions, but not Cd, influenced membrane permeability (K leakage). Cu acted more drasticly than Cd on NR activity.     

近40年来辽宁地区气候干湿界线年代际波动及其成因

应用1961～2004年辽宁省内52个气象站的温度、降水、湿度、风和日照等气候资料,采用改进的Penman模型计算了辽宁地区近40年的潜在蒸发量,讨论了其时空代表性及分布特征;以干燥度指数为干湿气候区的划分标准,通过对该地区近40年干湿气候界线波动状况的对比,在10年际尺度上详细分析了其干湿气候界线波动及变化规律.结果表明,20世纪60年代以来,辽宁省干湿气候界线波动显著,呈现出整体移动的特征,但半湿润与湿润、半干旱与半湿润两条界线并未表现出同进、同退的年际变化特征.20世纪90年代辽宁省干湿气候存在一次突变,半湿润与湿润界限明显东移,半干旱与半湿润界线明显西移,半干旱和湿润区面积都显著缩小,半湿润区面积显著扩大.辽宁西部的气候干湿状况主要由西太平洋副热带高压和东南季风控制,辽宁东部的气候干湿状况除受西太平洋副热带高压和东南季风的影响外,还应考虑到地形降水的作用.     

Seasonal changes in soil arthropod abundance in the dry evergreen forest of north-east Thailand,with special reference to collembolan communities

A soil arthropod community was studied in a dry evergreen forest over a 3-year period from May 1998 to April 2001. Population abundance, species composition, and community structure were investigated over the 3-year study period. The soil arthropods consisted of Acari (75.38%), Collembola (16.11%), and others (8.51%), and their abundances showed a clear difference between the rainy and dry seasons. Population abundance of Collembola and Acari were low during drought conditions. The humidity was the most important factor determining distribution, abundance, and survival of soil Collembola in this tropical forest. High predation and low accumulation of organic matter caused low population abundance of Collembola in the tropical habitat. The collembolan community was dominated by a few dominant species over the study period. The pattern of seasonal changes in numbers of Collembola was similar over the 3-year study period. The species composition of the collembolan community was constant and persistent throughout a 3-year study period. Thus, the collembolan community showed constancy in its species composition with seasonal variability over the 3-year study period.