中国温带阔叶红松林不同演替系列土壤有机碳矿化特征

土壤有机碳矿化与陆地生态系统碳循环和全球气候变化关系密切,为准确评估中国温带小兴安岭阔叶红松林不同演替系列土壤有机碳矿化特征及变化规律。以年代序列法代替群落次生演替过程,采用室内恒温培养(碱液吸收法)测定阔叶红松林不同演替系列(中生演替系列、湿生演替系列、旱生演替系列)6种群落类型土壤有机碳矿化量和矿化速率。3个演替系列土壤有机碳含量均表现出一致的剖面变化特征,随着土层深度的加深有机碳矿化量逐渐降少。且不同演替系列土层间有机碳矿化量不同,中生演替系列原始阔叶红松林土壤有机碳累计矿化量最大,其次为旱生演替系列,湿生演替系列最小。3个演替系列土壤有机碳矿化速率随时间变化呈现基本一致的趋势,即培养前期快速下降、后期逐渐趋于平稳。3个演替系列6种群落类型土壤有机碳矿化差异显著,表现为原始阔叶红松林白桦次生林云冷杉红松林红松枫桦次生林蒙古栎红松林蒙古栎、黑桦次生林。阔叶红松林不同演替系列土壤有机矿化采用非线性指数拟合效果较好。阔叶红松林不同演替系列土壤有机碳矿化与土壤全氮、凋落物量显著正相关,与土壤含水率、容重、土壤酸碱度显著负相关。不同演替系列群落的演替历史、土壤质地和养分状况等生态因子是导致阔叶红松林不同演替系列土壤有机碳矿化差异的原因。     

面向土系调查制图的小尺度区域景观分类——以宁镇丘陵区中一小区域为例

土系是中国土壤系统分类的基层分类单元,与所处微域景观联系密切,对小尺度样区进行景观分类研究有助于对研究区景观建立系统的认识。以宁镇丘陵区一小尺度样区为例,结合景观生态分类理论及土系特点,探讨了面向土系调查制图的景观分类的原则与方法,建立了包括景观区、景观类、景观亚类和景观相的四级景观分类系统,并借助3S技术进行了景观制图,并以此为基础对样区开展土系调查,对景观分类体系进行了验证。结果表明,景观相与土系有较好相关性,对土系分布具有指示作用,此景观分类体系有助于对土壤所处景观条件形成深入系统认识,可为土系调查制图工作提供参考。     

Shading results in depletion of the soil seed bank

To what extent is the decline of characteristic dry alvar species related to the decline in the soil seed bank during scrub encroachment? We recorded the number of flower stems in the vegetation in relation to light attenuation along an encroachment series progressing from open alvar through small gaps inside dense scrub of Juniperus communis (cover of 60%) to intact dense scrub (cover of 100%) on the island of Öland, Sweden. This measurement of potential reproduction (number of flower stems) was then compared to the number of species in the soil seed bank at each site along the alvar encroachment series. Scrub encroachment results in light attenuation between and under the shrubs. The total number of flower stems averaged over all species was similar between gaps and open alvar, but that of alvar species was significantly lower in the gaps, indicating that light attenuation could reduce their seed set. Shading in gaps is related to depletion of the soil seed bank and loss of alvar species, particularly those that do not form a persistent soil seed bank.     

红壤坡地土壤水分时间序列分析

基于时间序列法,分析了2002—2004年3—9月茶园和农作区两种土地利用方式下土壤水分与降雨的相关关系.结果表明,降雨为不相关序列,而不同深度(10、30、50、70和90 cm)土壤含水量有高度自相关性,为自相关序列,相关时间域为30～45 d.降雨和土地利用方式是影响土壤水分与降雨相关关系的主要因素.降雨对土壤水分的影响强度由表层到深层不断减弱,其在土壤表层(10和30 cm)的有效性时间为7～8 d;在深层有效时间长短不一,但雨后2～3 d,降雨对土壤水分(0～100 cm)的影响最显著.旱季土壤含水量与降雨的相关时间比雨季短1～3 d,若持续5 d降雨量小于5 mm,土壤表层水分含量就会明显降低,可能引发季节性干旱.与农作区相比,降雨对茶园表层水分的影响较弱,但对深层水分的影响较强且持续时间长.     

The relationship between available molybdenum in soils of volcanic ash origin and the molybdenum content in red clover (Trifolium pratense,L) leaves

Summary The relationship between Mo content in red clover leaves and available Mo in two different soil series of volcanic ash origin (Iwate-san and Hizume soils) was studied.If results were treated separately for each soil series, positive single correlations were obtained between leaf Mo and soil Mo extracted by Grigg's pH 3.3, 0.55N ammonium oxalate method. Correlation between leaf Mo and soil Mo was not significant if data from both soil series were combined. This relationship appeared to be due to several factors. First, the recovery of added Mo was lower in Hizume soils than in Iwate-san soils. This tendency for Mo fixation was confirmed by a pot experiment. Second, the amount of Fe as free hydrous Fe oxides dissolved in the acidic ammonium oxalate extract was higher in Hizume soils than in Iwate-san soils. This was negatively correlated with leaf Mo content. Therefore, the multiple correlation and regression between leaf Mo of red clover and available Mo, free hydrous Fe oxides and Mo recovery of soils gave satisfactory results even if data from both soils were combined.However, in the two soils used in this study, extraction at pH 3.3 failed to give the highest yield of Mo. They were obtained at much lower pH even though the concentration of organic acid remained constant. This was particularly clear in Iwate-san soils. The acidic ammonium oxalate extraction procedure tends to underestimate soil Mo availability in these kinds of soils, especially in extraction of Iwate-san soils.     

Selection of Pupation Habitats by Oriental Fruit Fly Larvae in the Laboratory

We performed a series of laboratory experiments to determine the effects of shade, soil moisture, and soil compaction on the selection of pupation habitats by wandering late-instar Oriental fruit flies, Bactrocera dorsalis (Hendel). Larvae showed a strong preference toward pupating in shaded rather than brightly lit areas, in moist rather than dry soil, and in soil with larger particle sizes. These behavioral preferences are likely to lead to clumped distribution of Oriental fruit fly pupae in natural habitats. The implications of this for management of localized populations by chemical and biological methods are discussed.     

Effect of soil chloride level on cadmium concentration in sunflower kernels

Understanding soil factors related to cadmium (Cd) uptake and accumulation in plants is important for development of agronomic technologies, and breeding strategy to produce low Cd crops. The objective of the study was to examine the effect of soluble salts (chloride and sulfate) and other soil factors on the Cd concentration in sunflower (Helianthus annuus L.) kernels. Commercial nonoilseed hybrid kernels and soils were sampled from 22 farmer's production fields in North Dakota and Minnesota. The sites sampled included saline and nonsaline variants from 7 soil series. Soils were sampled at four depths. Relationships between kernel Cd level and soil physical and chemical characteristics were examined. The soil pH covered a narrow range (7.3–8.1) at these sampled sites. Regression analysis showed that there was no correlation between kernel Cd and soil pH at any depth. The kernel Cd level was highly correlated with DTPA-extractable Cd in all 4 depths, and with clay content in sub-soils. Soil chloride and sulfate concentrations varied among soil series and within soil series. The absence of a statistically significant effect of soil sulfate level on kernel Cd concentration, indicated that soil sulfate levels did not affect Cd uptake by sunflower plants. However, soil chloride levels in sub-soil were correlated with kernel Cd. The most important soil factor was DTPA-extractable Cd. When chloride was included in the multiple regression equations, R square (R²) values improved significantly. These results demonstrate that soil chloride concentration is another important factor related to Cd uptake in sunflower plants.     

Effect of some biological factors on soil variability in the tropics

Summary Field observations were carried out on an Egbeda soil series in western Nigeria to study the degree of soil-nutrient variability within and between plots due to pre-clearing vegetation. The soil showed lower soil pH, organic C, exchangeable K and Ca contents following cassava grown by traditional methods than following secondary forest vegetation or thicket regrowth. Except for exchangeable K, the degree of variability of the above parameters was observed to be in the following order: secondary forest vegetation > thicket regrowth > cassava plots. The available P status was generally low and showed little relation to pre-clearing vegetation. The implications of soil variability due to pre-clearing vegetation on soil sampling and in field experimentation are discussed. re]19760204     

Estimating root zone soil moisture at distant sites using MODIS NDVI and EVI in a semi-arid region of southwestern USA

This study investigates the potential of using Normalized Difference Vegetation Index (NDVI) and Enhanced Vegetation Index (EVI) to estimate root zone soil moisture at native in-situ measured sites, and at distant sites under the same climatic setting. We obtained in-situ data from Soil Climate Analysis Network (SCAN) sites near the Texas-New Mexico border area, and NDVI and EVI products from the Moderate Resolution Imaging Spectroradiometer (MODIS) sensor on board the Terra satellite. Results show that soil moisture values of the same depth are highly correlated (r = 0.53 to 0.85) among sites as far as 150 km apart, and that NDVI and EVI are highly correlated at the same site (r = 0.87 to 0.91). Correlation based on raw time series of NDVI and soil moisture is in general higher than that based on deseasonalized time series at every depth. The correlation reaches maximum value when vegetation index (VI) lags soil moisture by 5 to 10 days. NDVI shows a slightly higher correlation with soil moisture than EVI does by using the deseasonalized time series of NDVI and soil moisture. It is found that deseasonalized time series of NDVI and soil moisture are correlated at native sites (r = 0.33 to 0.77), but not at sites where soil moisture is very low. Regression analysis was conducted using deseasonalized time series soil moisture and deseasonalized time series NDVI with a 5-day time lag. Regression models developed at one site and applied to a similar distant site can estimate soil moistures, accounting for 50–88% of the variation in observed soil moistures.     

浙江天童森林公园植物群落演替对土壤物理性质的影响

对浙江宁波天童森林公园内的裸地、灌丛、马尾松林、马尾松木荷林、木荷林、栲树木荷林和栲树林等演替阶段土壤物理性质进行了比较分析。结果表明,尽管由于样地坡度和母质等因素的影响,演替群落土壤呈现趋砂性特征,但植物群落进展演替能明显降低土壤容重,阔叶林群落减少的幅度更显著;同时,演替能提高土壤空隙度;土壤含水量、土壤最大持水量、毛管持水量和最小持水量在演替过程中的增长趋势明显;土壤固相率减少,气相率增大。因此,植物群落进展演替能明显降低土壤紧实性,改善土壤通气性及持水性能,呈现出与土壤质地效应相反的变化趋势,促进了土壤肥力的发挥。而土壤物理性质的改善,也有利于群落物种更替和演替进程     

Sustainable phosphorous management in two different soil series of Pakistan by evaluating dynamics of phosphatic fertilizer source

Phosphorous (P) plays the prominent role to promote the plants storage functions and structural roles, as it is recognized as a vital component of ADP, ATP, Cell wall as well as a part of DNA. Soils acts as the sink to supply P to plants because soil pH and its physical condition are the main factor which regulate the solubility and availability P element. Phosphorus is not deficient in Pakistani soils but its availability to plants is the serious matter of concern. A pot experiment was conducted to evaluate P dynamics in two different soil series of Pakistan (Bahawalpur and Lyallpur) using Maize as test crop. The treatments applied were T0: Control (without any fertilizer), T1: Recommended DAP @648 mg pot^?1, T2: Half dose DAP @324 mg pot^?1, T3: Recommended rate of TSP @900 mg pot^?1, T4: Half dose TSP @450 mg pot^?1. Soil analysis showed that Bahawalpur soil has sandy clay loam texture with 33% clay and Lyallpur series has sandy loam texture with 15.5% clay; furthermore, these soil contain 4.6 and 2.12% CaCO₃ respectively. Results showed an increase in P concentration in roots (23 mg kg^?1) with the application of half dose of TSP in Lyallpur series and lowest in Bahawalpur series (14.6 mg kg^?1) at recommended dose of DAP. Concentration of P in shoots responded the same; increase at half dose of TSP (16.7 mg kg^?1) and lowest at full dose of DAP in Bahawalpur series as (15.58 mg kg^?1). Adsorbed P (17 mg kg^?1) was recorded highest in Bahawalpur soil with more clay amount in pot with DAP application but lower in Lyallpur soil series (14 mg kg^?1) with the application of applied TSP. The PUE was recorded highest in Lyallpur series with the application of half dose of TSP and it was 61% more than control and was Highest in Bahawalpur series was with the application of recommended dose of DAP is 72% more than control treatment. On estimation; results showed that applied sources made an increase in P availability than control, but TSP gave better P uptake than DAP unless of rates applied. Soil of Lyallpur series showed better uptake of P and response to applied fertilizers than Bahawalpur series which showed more adsorption of P by high clay and CaCO₃ amount. Conclusively, the study suggested that soil series play a crucial role in choosing fertilizer source for field application.     

Temporal variability and scaling behaviour in the fine-root system of kiwifruit (Actinidia deliciosa)

We show that temporal variability in root populations can depend upon the scale of measurement (particularly the sampled soil volume). The presence of roots in a range of volumes of soil was studied using perspex tubes installed horizontally into the soil around three mature kiwifruit vines. Roots intercepting lines scored on the tubes were counted using a periscope. For small volumes of soil (c. 2–4 cm³) the root counts varied with time in a very irregular manner, and as the interval between measurements increased the autocorrelation between the measurements decayed rapidly. At about half of the locations monitored there was no significant autocorrelation between measurements 27 d apart. Linear interpolation in these time series was unreliable, and where the correlation dimension could be resolved it was usually non-integer (suggesting chaotic behaviour). The time series measured at different locations were poorly correlated, indicating weak coordination. As the observed soil volume increased, the coordination between locations improved, the autocorrelation function increased, and linear interpolation errors decreased (although these remained substantial). Clearly there are considerable fundamental constraints on our ability to predict the root behaviour of kiwifruit vines at scales that are appropriate for mechanistic models of nutrient and water uptake. We discuss the need for a new conceptual model of the fine-root systems of kiwifruit and similar species.     

The dynamics of root meristem distribution in the soil

Plants must develop efficient root architectures to secure access to nutrients and water in soil. This is achieved during plant development through a series of expansion and branching processes, mostly in the proximity of root apical meristems, where the plant senses the environment and explores immediate regions of the soil. We have developed a new approach to study the dynamics of root meristem distribution in soil, using the relationship between the increase in root length density and the root meristem density. Initiated at the seed, the location of root meristems in barley seedlings was shown to propagate, wave‐like, through the soil, leaving behind a permanent network of roots for the plant to acquire water and nutrients. Data from observations on barley roots were used to construct mathematical models to describe the density of root meristems in space. These models suggested that the morphology of the waves of meristems was a function of specific root developmental processes. The waves of meristems observed in root systems of barley seedlings exploring the soil might represent a more general and fundamental aspect of plant rooting strategies for securing soil resources.     

西双版纳“龙山”片断热带雨林中小型土壤动物群落组成与多样性研究

对西双纳不同面积“龙山”片断干性季节雨林和保护区连续湿性季节雨淋凋落物层土壤动物群落多样性研究表明,土壤动物群落物种丰盛度,多度和多样性的变化不顾在随雨林片断化面积减少而降低的“种－面积效应”,而雨林片断化后因先锋植物（喜阳性）侵入产生的“干暖效应”,使片断雨林凋落物增多,腐殖质,土壤有机质,N,P等元素含量增高,土壤生境条件更有利于土壤动物生存,其群落多样性指数高于连续湿性季节雨林,但2种生境土壤动物群落种－多度模型均表现为对数级模式。     

鄂尔多斯高原弃耕农田恢复过程中土壤物理性质和生物结皮的变化

在鄂尔多斯高原软梁、硬梁弃耕农田上选取一系列不同时限的弃耕农田,研究弃耕演替过程中地表凋落物、生物结皮,以及不同土层土壤容重、机械组成、含水量的动态变化.结果表明: 软梁弃耕农田表层(0～10 cm)物理环境随弃耕年限增加明显改善,土壤黏粒含量、地表凋落物随弃耕年限增加明显增加,土壤容重明显降低,土壤含水率略微升高;中层(10～30 cm)土壤物理环境随弃耕年限增加稍显恶化,土壤黏粒含量升高,土壤含水量略微降低;深层(30～50 cm)土壤物理性质变异较大.硬梁弃耕农田土壤表面凋落物盖度、生物结皮盖度、生物结皮厚度随弃耕年限增加而增加,表层(0～10 cm)土壤容重、黏粒含量、含水量随弃耕年限变化总体变化不显著,深层(10～40 cm)土壤物理性质变异较大.地表凋落物和土壤黏粒物质的累积导致软梁弃耕农田土壤水分浅层化,可能是20年内浅根性多年生草本植物群落取代半灌木油蒿群落的关键因素.硬梁弃耕农田在演替过程中未见油蒿入侵,可能与较高的浅层含水量和生物结皮发育有关.     

Response of the microbial community to copper oxychloride in acidic sandy loam soil

AIMS: Determining the response of different microbial parameters to copper oxychloride in acidic sandy loam soil samples using cultivation-dependent and direct microscopic techniques. METHODS AND RESULTS: Culturable microbial populations were monitored for 245 days in a series of soil microcosms spiked with different copper oxychloride concentrations. Microbial populations responded differently to additional Cu. Protistan numbers and soil metabolic potential decreased. Experiments with more soil samples revealed that metabolic potential was not significantly affected by < or =100 mg kg(-1) additional Cu. However, a negative impact on protista was noted in soil containing only 15 mg kg(-1) EDTA-extractable Cu. The negative impact on protistan numbers was less severe in soils with a higher phosphorous and zinc content. CONCLUSIONS: Bacterial populations responded differently, and protista were most sensitive to elevated Cu levels. Protistan numbers in soil from uncultivated land were higher and seemed to be more sensitive to additional Cu than the numbers of these organisms in soil originating from cultivated land. SIGNIFICANCE AND IMPACT OF THE STUDY: Protistan sensitivity to small increases in Cu levels demonstrates the vulnerability of the soil ecosystem to Cu perturbations, especially when the importance of protista as link in the flow of energy between trophic levels is considered.     

Sensitive and specific molecular detection of Burkholderia pseudomallei, the causative agent of melioidosis, in the soil of tropical northern Australia

Burkholderia pseudomallei, the cause of the severe disease melioidosis in humans and animals, is a gram-negative saprophyte living in soil and water of areas of endemicity such as tropical northern Australia and Southeast Asia. Infection occurs mainly by contact with wet contaminated soil. The environmental distribution of B. pseudomallei in northern Australia is still unclear. We developed and evaluated a direct soil B. pseudomallei DNA detection method based on the recently published real-time PCR targeting the B. pseudomallei type III secretion system. The method was evaluated by inoculating different soil types with B. pseudomallei dilution series and by comparing B. pseudomallei detection rate with culture-based detection rate for 104 randomly collected soil samples from the Darwin rural area in northern Australia. We found that direct soil B. pseudomallei DNA detection not only was substantially faster than culture but also proved to be more sensitive with no evident false-positive results. This assay provides a new tool to detect B. pseudomallei in soil samples in a fast and highly sensitive and specific manner and is applicable for large-scale B. pseudomallei environmental screening studies or in outbreak situations. Furthermore, analysis of the 104 collected soil samples revealed a significant association between B. pseudomallei-positive sites and the presence of animals at these locations and also with moist, reddish brown-to-reddish gray soils.     

荒漠人工固沙植被区土壤水分的时空变异性

表层土壤水分具有高度的时间和空间变异性.研究的目的:(1)揭示沙坡头人工固沙植被区浅层土壤水分的时空变异性特征;(2)确定驱动土壤水分变异的主要环境因子.在人工固沙植被区内一个4500m2的网格样地上每隔10m设置取样点,在连续7个月的时间内 (2005年4～10月),每隔15d用时域反射仪测量各样点表层以下15cm和30cm深度的土壤容积含水量.结果表明,该区网格尺度上浅层土壤水分的分布具有明显的空间变异性,其变异性随着土壤水分含量的降低而减小;相对海拔是驱动土壤水分空间变异的主要环境因子,其作用在降雨后尤为显著,且其对土壤下层的影响比上层更明显;植被和土壤水分含量的相关性时间序列与相对海拔一致--降雨使其相关性增加;土壤质地(土壤粒径分布)和土壤水分含量的相关性时间序列特征与植被和相对海拔相反,且其对土壤上层的影响比下层更明显.因此,在沙坡头荒漠人工固沙植被区,降雨后的短暂湿润期,地形和植被是驱动浅层土壤水分变异的主要影响因子,而随着降雨之后土壤逐渐变干,土壤质地的影响变得更加明显.     

Slow arbuscular mycorrhizal colonisation of field-grown cotton caused by environmental conditions in the soil

 Slow arbuscular mycorrhizal colonisation is characteristic of a growth disorder of cotton occurring in crops in northern New South Wales, Australia. To determine whether or not slow colonisation is caused by poor survival of mycorrhizal fungi between crops, we examined colonisation of cotton in field crops and in a series of pot bioassays. Cotton roots were sampled at sites with or without severe symptoms of the growth disorder in each of three fields in 1991 and two fields in 1993. The bioassays were at intervals over the winter fallow prior to the crops in both years. In each bioassay, soil was collected from the field sites and sown with cotton in pots in a controlled environment cabinet. Colonisation was assessed at 14, 28 and 42 days after sowing. In the bioassay series, colonisation at 14 days, which was representative of primary infections of roots and hence propagule density in soil, tended to decline over the winter fallow. In contrast, colonisation at 42 days, which included secondary spread of infection, first declined and then returned to its original level or higher. In the field, plants affected by the growth disorder were colonised slowly, while healthy plants were colonised rapidly. In the bioassays, however, colonisation in the soil from sites with the growth disorder equalled or surpassed that in soil from sites with healthier cotton. Thus, the slow colonisation and growth of field-grown cotton did not result from a lack of mycorrhizal inoculum and was most likely caused by soil factors. Accepted: 21 August 1998     

山楂种子体眠和萌发与营养物质植物生长物质关系的研究

对低温层积不同时期的山楂种仁中的氨基酸、植物生长物质等几项生理生化指标进行了定量分析的结果表明层积１５至１８个月时因缺水出现二次休眠,在种子内部发生一系列生理变化,从中得知脱落酸,吲哚乙酸为生长抑制剂,玉米素核苷,赤霉素为促进剂。脯氨酸对干旱比较明感,随着层积时间的延长营养物质趋于升高,酶的活性提高,为种子发芽提供了能量。