长期施肥条件下黑土有机碳、氮组分的分配与富集特征

研究不同管理措施下黑土有机碳、氮组分的变化特征是深刻认识和理解黑土固碳的基础.本文以黑龙江省农业科学院31年的长期定位试验为基础,采用物理分组法对土壤不同粒径颗粒进行分离,分析6种不同施肥处理31年后,黑土表层(0～20 cm)及亚表层(20～40 cm)土壤有机碳、氮在粗砂粒、细砂粒、粉粒及黏粒中的分配与富集特征.结果表明： 长期施用有机肥可显著提高土壤有机碳、全氮在粗砂粒和黏粒中的分配比例.在表层土壤,有机无机配施（NPKM）处理下粗砂粒有机碳和全氮的分配比例比对照分别提高191.3%和179.3%,单施有机肥（M）处理下黏粒组分的有机碳和全氮的分配比例分别提高45%和47%.亚表层土壤施用有机肥处理各粒级有机碳、氮含量的提高比例低于表层土壤.在表层和亚表层的粉粒组分中,贮存的有机碳占总储量的42%～63%和48%～54%,全氮占总储量的34%～59%和41%～47%.表层土壤施用有机肥可显著增加粗砂粒中有机碳、氮的富集系数,其中有机肥配施化肥（NPKM）处理富集系数最高（2.30和1.88）,而黏粒组分的有机碳、氮富集系数对长期施肥无响应.
     

Downward flux of water through roots (i.e. inverse hydraulic lift) in dry Kalahari sands

Downward transport of water in roots, in the following termed “inverse hydraulic lift,” has previously been shown with heat flux techniques. But water flow into deeper soil layers was demonstrated in this study for the first time when investigating several perennial grass species of the Kalahari Desert under field conditions. Deuterium labelling was used to show that water acquired by roots from moist sand in the upper profile was transported through the root system to roots deeper in the profile and released into the dry sand at these depths. Inverse hydraulic lift may serve as an important mechanism to facilitate root growth through the dry soil layers underlaying the upper profile where precipitation penetrates. This may allow roots to reach deep sources of moisture in water-limited ecosystems such as the Kalahari Desert. Received: 1 January 1998 / Accepted: 1 April 1998     

Does food‐searching ability determine habitat selection? Foraging in sand of three species of gerbilline rodents

The distribution of three gerbil species in the Negev Desert, Israel differs in relation to sandy habitats. Gerbillus gerbillus occurs in sand only, Gerbillus dasyurus lives in all habitat types except sand, Gerbillus henleyi occurs in sand at high density periods only. We hypothesized that the reason for this distribution pattern is differential ability of species to forage in sand. We tested the ability of gerbils to search for seeds in sand layers of different depths and predicted that a) G. gerbillus will have equal search success at different sand depths, b) G. henleyi (which is twice smaller than G. gerbillus and G. dasyurus) will find seeds in thin layers better than in deep layers, and c) G. dasyurus will successfully find seeds in the thinnest layers only. We predicted also d) that G. gerbillus relies on olfaction for seed location, so its foraging success will be higher in searching for whole seeds than for seed kernels, whereas this will not be the case for G. henleyi and G. dasyurus. We examined the responses of the three species to odor of whole seeds vs seed kernels in Y-maze. In regards to seed depth, the search success of G. gerbillus was significantly higher when the whole seeds rather than kernels were offered in all treatments except the control, but sand depth did not influence the search success. The search success of G. dasyurus and G. henleyi did not depend on the type of seeds offered. The search success of G. dasyurus was lower in experimental (1, 3, 5 and 8 cm sand depth) than in control (1 mm sand depth) treatments, but did not differ among most experimental treatments. The search success of the smallest G. henleyi depended on sand depth for both whole seeds and kernels. Gerbillus gerbillus and G. dasyurus did not lose body masses in any treatment, whereas body mass changes of G. henleyi were influenced by the depth of sand in which gerbils foraged. No species demonstrated differences in response to whole seeds vs kernels in Y-maze tests.     

科尔沁沙地植物群落圆环状分布成因地统计学分析

调查发现,在科尔沁沙地中部部分梁窝状沙丘的丘顶、丘坡和丘间地,植物群落依生境梯度而分布,呈典型圆环状分布格局．沙层水分状况分析表明,同一沙丘不同部位的沙层含水量为丘顶低于丘坡地,且二者均低于丘间地．地统计学分析表明,无论是流动沙丘还是固定沙丘,从丘顶、丘坡到丘间地,沙层含水量的空间异质性呈规律性的变化,块金值与基台值之比逐渐减小,变程逐渐减小,分维数逐渐增大,表明随机部分引起的空间异质性逐渐降低,而由空间自相关部分引起的空间异质性逐渐增高．因此,沙丘不同部位沙层含水量及其空间异质性的有规律变化是科尔沁沙地中部部分梁窝状沙丘植物群落呈圆环状分布格局的一个重要原因．     

Prey detection in antlions: propagation of vibrational signals deep into the sand

Trap‐building antlion larvae detect their prey according to the substrate vibrations produced during movement of the prey on the sand surface. Although most studies are devoted to surface vibrational waves, in the present study, we determine the role of vibrations travelling through deeper sand layers. A behavioural experiment confirms that vibrational stimuli from prey insects on the surface of the sand stimulate the antlions buried in deeper sand layers to move towards the surface. Sand depth and particle size both have a strong effect on signal transmission. The damping coefficient (α₁₀) varies from 0.49 dB to 3.30 dB cm^?1 and depends on frequency (in the range from 100 to 300 Hz), particle size (from finest to coarse sand) and distance from the source of the vibrations. The deeper the sand, the narrower the frequency range of the signal becomes. Sand is a filter for higher frequencies. The smaller the sand particles, the more intense the filtering becomes. Fine sand with a mean sand particle size of 360 μm is a more efficient filter than coarse sand; consequently, high frequencies (> 2.5 kHz) are eliminated at a depth of 3 cm. Mean frequency depends on both depth and particle size. However, low frequency signals still propagate at a certain distance, which is biologically important in prey detection. Although the most efficient signal propagation appears to occur in coarse sand, it contains overly large particles that are inconvenient for relatively small antlion larvae. Predators seek a compromise between fine and coarse sand choosing medium sand.     

Effect of bacterial extracellular polymers on the saturated hydraulic conductivity of sand columns.

Columns were packed with clean quartz sand, sterilized, and inoculated with different strains of bacteria, which multiplied within the sand at the expense of a continuous supply of fresh nutrient medium. The saturated hydraulic conductivity (HCsat) of the sand was monitored over time. Among the four bacterial strains tested, one formed a capsule, one produced slime layers, and two did not produce any detectable exopolymers. The last two strains were nonmucoid variants of the first two. Only one strain, the slime producer, had a large impact on the HCsat. The production of exopolymers had no effect on either cell multiplication within or movement through the sand columns. Therefore, the HCsat reduction observed with the slime producer was tentatively attributed to the obstruction of flow channels with slime. Compared with the results with Arthrobacter sp. strain AK19 used in a previous study, there was a 100-fold increase in detachment from the solid substratum and movement through the sand of the strains used in this study. All strains induced severe clogging when they colonized the inlet chamber of the columns. Under these conditions, the inlet end was covered by a confluent mat with an extremely low HCsat.     

Effect of bacterial extracellular polymers on the saturated hydraulic conductivity of sand columns.

Columns were packed with clean quartz sand, sterilized, and inoculated with different strains of bacteria, which multiplied within the sand at the expense of a continuous supply of fresh nutrient medium. The saturated hydraulic conductivity (HCsat) of the sand was monitored over time. Among the four bacterial strains tested, one formed a capsule, one produced slime layers, and two did not produce any detectable exopolymers. The last two strains were nonmucoid variants of the first two. Only one strain, the slime producer, had a large impact on the HCsat. The production of exopolymers had no effect on either cell multiplication within or movement through the sand columns. Therefore, the HCsat reduction observed with the slime producer was tentatively attributed to the obstruction of flow channels with slime. Compared with the results with Arthrobacter sp. strain AK19 used in a previous study, there was a 100-fold increase in detachment from the solid substratum and movement through the sand of the strains used in this study. All strains induced severe clogging when they colonized the inlet chamber of the columns. Under these conditions, the inlet end was covered by a confluent mat with an extremely low HCsat.     

Re-embodying Sand Drawing and Re-evaluating the Status of the Camp: The Practice and Iconography of Women's Public Sand Drawing in Balgo,W.A.

The documentation of Aboriginal women's sand-drawing practice in Central Australia has to date been based largely on Munn's research amongst the Warlpiri at Yuendumu. Data from Kutjungka women from the Balgo area of Western Australia show that there are marked geographic differences in the styles of public sand drawing used by women from the two areas, as well as differences in gender coding between the two systems. The account of Balgo women's public sand drawing presented here uses methodologies grounded in recent developments in phenomenology, practice theory and embodiment theory, to examine layers of meaning encoded in this everyday practice. It suggests that women's public sand drawing in this area is linked to Kutjungka thought about the Dreaming, through webs of thought about the significance of penetrating the surface of the land, in some ways foreshadowing aspects of the women's ceremonial practices. This account suggests that the relationship between male and female ‘graphic’ systems may be more accurately described as dialogical than dichotomous.     

Spatiotemporal pattern of seed bank in the annual psammophyte Agriophyllum squarrosum Moq. (Chenopodiaceae) on the active sand dunes of northeastern Inner Mongolia, China

The seed banks of active sand dunes are critical for the adaptation of psammophytes to unstable habitats. However, existing reports have failed to effectively elucidate the spatiotemporal structure of these seed banks and the factors regulating them. The seed bank pattern of the annual psammophyte Agriophyllum squarrosum Moq. in active sand dunes was studied by taking into consideration the time, the depth of the soil profile, dune positions, and seed bank type (released seed bank, belowground and aboveground canopy seed banks). Most canopy-stored seeds were unburied before the following March of the maturation year; however, they were buried from March to May. The seed bank mainly comprised the aboveground canopy-stored seeds from September of the year of seed maturation to the following March. The seed bank was concentrated in the surface soil layers (0–10 cm) from March of the year following seed maturation to June and was concentrated in the deep soil layers (10–50 cm) after June. The seed bank in the lower leeward slope tended to be larger than those in the other dune positions. The canopy-stored seed:released seed ratio differed between dune positions. The findings of this study are: (1) sand burial and wind erosion play key roles in shaping the spatiotemporal pattern of the seed banks of active sand dunes, and (2) delayed seed release may be a major factor regulating the spatiotemporal pattern of the seed banks of certain psammophytes.     

Production of vesicular-arbuscular mycorrhizal sporocarps,Glomus aggregatum,on fiberglass screens

Glomus aggregatum was culture onZea mays in sand. Fiberglass screen layers wrapped around the sand medium effectively provided a framework for sporocarp formation, and facilitated the subsequent harvest of the sporocarps.     

Effect of Bacterial Polysaccharide Accumulation on Infiltration of Water Through Sand

A study was carried out of the mechanisms of biological clogging of sand during prolonged percolation of water containing high levels of organic matter. It was found that polysaccharide-producing microorganisms predominated in clogged layers of sand. A positive correlation was observed between accumulation in the profile of polysaccharides and clogging of columns of sand in permeameters. The level of oxygen in the system appears to determine the equilibrium between production of clogging materials and their decomposition.     

Distribution of Methanotrophs in Trichloroethylene-Contaminated Aquifers in a Natural Gas Field

The distribution of methanotrophs was examined in shallow aquifers contaminated with trichloroethylene in the southern Kanto gas field, Chiba, Japan. The total populations of methanotrophs and the numbers of methanotrophs producing soluble methane monooxygenase (sMMO) were determined separately. Hydrostratigraphic units of a Pleistocene to Holocene stratum consisted of three aquifers separated by nontransmissive silt layers. Dissolved methane concentrations increased with depth and were highest in the third aquifer. The number of methanotrophs was higher in the second aquifer than in the first aquifer. A clear relationship was observed between microbial populations and lithofacies. The greatest abundance of methanotrophs was observed in the coarse sand layers of the second aquifer, with the lowest abundance observed in silt layers. The high abundance of methanotrophs in the coarse sand in the second aquifer implied that this part of the stratum plays an important role in in situ bioremediation.     

Physicochemical impacts associated with natural gas development on methanogenesis in deep sand aquifers

The Minami-Kanto gas field, where gases are dissolved in formation water, is a potential analogue for a marine gas hydrate area because both areas are characterized by the accumulation of microbial methane in marine turbidite sand layers interbedded with mud layers. This study examined the physicochemical impacts associated with natural gas production and well drilling on the methanogenic activity and composition in this gas field. Twenty-four gas-associated formation water samples were collected from confined sand aquifers through production wells. The stable isotopic compositions of methane in the gases indicated their origin to be biogenic via the carbonate reduction pathway. Consistent with this classification, methanogenic activity measurements using radiotracers, culturing experiments and molecular analysis of formation water samples indicated the predominance of hydrogenotrophic methanogenesis. The cultivation of water samples amended only with methanogenic substrates resulted in significant increases in microbial cells along with high-yield methane production, indicating the restricted availability of substrates in the aquifers. Hydrogenotrophic methanogenic activity increased with increasing natural gas production from the corresponding wells, suggesting that the flux of substrates from organic-rich mudstones to adjacent sand aquifers is enhanced by the decrease in fluid pressure in sand layers associated with natural gas/water production. The transient predominance of methylotrophic methanogens, observed for a few years after well drilling, also suggested the stimulation of the methanogens by the exposure of unutilized organic matter through well drilling. These results provide an insight into the physicochemical impacts on the methanogenic activity in biogenic gas deposits including marine gas hydrates.     

新疆古尔班通古特沙漠南部沙垄不同部位藻类的垂直分布特征

 通过2005和2006年夏季两次对新疆古尔班通古特沙漠南部荒漠土壤中藻类植物进行采样、培养、鉴定和生物量测定,分析了该区沙漠沙垄不同部位藻类物种组成、优势种和生物量的垂直变化。结果表明：1）在不同地貌部位的不同层次中,藻类的种类组成均有所差异。2）藻类优势物种主要集中在0～2 cm层次中,2 cm以下的土层中藻类细胞很少,绝大部分土层以具鞘微鞘藻(Microcoleus vaginatus)为第一优势种,有些部位的土层中第一优势种是伪双点颤藻(Oscillatoria pseudogeminata),如垄间低地和迎风坡的1～2 cm中。此外,大型集胞藻（Synechocystis crassa）、舟形藻 (Navicula sp.)、卵圆双眉藻(Amphora ovalis)数量也较多。3）除垄顶外,藻类生物量在其它3个部位不同层次的差异呈极显著水平（p<0.01）,生物量由表及里锐减;在同一土层,藻类生物量基本表现为垄间低地最高,迎风坡与背风坡居中, 垄顶最低,不同地貌部位对藻类生物量影响呈显著或极显著水平。     

Sequential Subterranean Transport of Excavated Sand and Foraged Seeds in Nests of the Harvester Ant,Pogonomyrmex badius

During their approximately annual nest relocations, Florida harvester ants (Pogonomyrmex badius) excavate large and architecturally-distinct subterranean nests. Aspects of this process were studied by planting a harvester ant colony in the field in a soil column composed of layers of 12 different colors of sand. Quantifying the colors of excavated sand dumped on the surface by the ants revealed the progress of nest deepening to 2 m and enlargement to 8 L in volume. Most of the excavation was completed within about 2 weeks, but the nest was doubled in volume after a winter lull. After 7 months, we excavated the nest and mapped its structure, revealing colored sand deposited in non-host colored layers, especially in the upper 30 to 40 cm of the nest. In all, about 2.5% of the excavated sediment was deposited below ground, a fact of importance to sediment dating by optically-stimulated luminescence (OSL). Upward transport of excavated sand is carried out in stages, probably by different groups of ants, through deposition, re-transport, incorporation into the nest walls and floors and remobilization from these. This results in considerable mixing of sand from different depths, as indicated in the multiple sand colors even within single sand pellets brought to the surface. Just as sand is transported upward by stages, incoming seeds are transported downward to seed chambers. Foragers collect seeds and deposit them only in the topmost nest chambers from which a separate group of workers rapidly transports them downward in increments detectable as a "wave" of seeds that eventually ends in the seed chambers, 20 to 80 cm below the surface. The upward and downward transport is an example of task-partitioning in a series-parallel organization of work carried out by a highly redundant work force in which each worker usually completes only part of a multi-step process.     

Oxygen-related facies in Lake Pannon deposits (Upper Miocene) at Budapest-Köbánya

Oxygen availability is considered to have been a major factor in shaping the sedimentary facies and biofacies of a Late Miocene (8–8.5 Ma old) Lake Pannon sequence studied in the Kozma-street outcrop in Budapest-Köbánya. The sequence contains blue clays deposited in low-oxygen conditions between the storm and the fair-weather wave bases and thin intercalations of laminated fine sand interpreted as tempestites. The storms caused temporary oxygenation of the bottom and thus promoted bioturbation, as indicated by the presence of trace fossils belonging to the Arenicolites ichnofacies or a lacustrine equivalent of the marine Skolithos ichnofacies. Fully bioturbated sand layers with the infaunal Dreissenomya and other littoral molluscs indicate longer periods of bottom ventilation. The blue clays immediately above these sand layers also contain abundant and diverse mollusc fauna. Oxygen deficiency on the “shelf” of Lake Pannon was a local phenomenon probably caused by a high organic loading and/or a salinity-induced stratification.     

Colonization of the root zone ofAmmophila arenaria by harmful soil organisms

The role of harmful soil organisms in the degeneration ofAmmophila arenaria at coastal foredunes was examined by the growing of seedlings ofA. arenaria in soil samples collected from its root zone. Three sites, each representing a successive stage in foredune succession were examined: (1) a highly mobile dune (sand accretion of 80 cm year⁻¹) with vigorousA. arenaria, colonizing only the upper 30-cm of the annually deposited layer of sand, (2) a mobile dune with vigorousA. arenaria (sand accretion of 22 cm year⁻¹) and a 1-metre soil profile completely colonized by roots and (3) a stable dune (no sand accretion) with degeneratedA. arenaria and young roots mainly present in the upper 0–10 cm. In the upper part of the highly mobile site, the presence of harmful soil organisms was confined to the root layers and at the mobile site for all depth layers a significant growth reduction ofA. arenaria was observed due to the activity of harmful soil organisms. At the stable site, however, growth had only been reduced in some of the depth layers. At all sites newly formed roots ofA. arenaria had been colonized by harmful soil organisms within one year. If present in sand prior to root growth harmful soil organisms reduced root length and root hair formation severely and they enhanced branching of the roots. It is concluded that harmful soil organisms initiate degeneration ofA. arenaria in stable dunes by attack of the root system, which makes the plants suffer from abiotic stress.     

The influence of soil texture on the soil water dynamics and vegetation structure of a shortgrass steppe ecosystem

We analyzed soil water data from three sites with different soil textures in the shortgrass steppe of northeastern Colorado, USA. Our objective was to evaluate the relationship between the occurrence of plant functional types and the effect of soil texture on soil water availability. Soil water availability was greatest in the upper soil layers at all three sites, but the loamy sand site had significantly greater soil water availability than the sandy clay loam and sandy clay sites in wetter years at depths below 60 cm. Calculations of proportional water availability by layer using both field data and fifty-year soil water model simulations, showed that the sandy clay loam and sandy clay soils on average had greater water availability in layers 30 cm and above, but that the loamy sand had the greatest water availability in layers beneath this, particularly at 105 cm. This observation can be linked to the occurrence of a fine textured subsoil at this site. The textural pattern in the loamy sand profile effectively creates two water resources: a shallow pool accessible to all plants; and a deep pool accessible only to deep-rooted plants. This is offered as an explanation for the co-dominance of the two main plant functional types at the loamy sand site. At the other two sites, shallow-rooted shortgrass vegetation dominated, being more consistent with the general pattern for the area. Thus the patterns of vegetation structure at the three sites were consistent with the hypothesis. Aboveground net primary production data for the three sites, along with transpiration estimates from the model simulations, indicated that the additional water availability in the coarse textured soil was associated with higher overall plant productivity.Nomenclature: Taxonomic nomenclature follows R. L. McGregor & T. M. Barkley (1986) Flora of the Great Plains. Great Plains Flora Association. University Press of Kansas, Lawrence.     

Notes on Lejeuneaceae: I. Microlejeunea diversiloba (Spr.) K.M.

Abstract

Previous work on the bryophytic component of dune communities has demonstrated changes in the representation of species with the progress of succession. The ability of some to act as pioneers and the restriction of others to later stages may be associated with their reactions to recurrent burial by wind-blown sand.

Eighteen species were selected for experimental investigation of the effects of sand burial, along the following lines:

(a) Transplants. Samples of eight species were transplanted to four sites representing different stages of the dune succession. Where the sand increment over 11 months exceeded about 4 cm. none survived but species found naturally in mobile dune areas emerged from about 3 cm. Those belonging to fixed dune communities survived only in the absence of burial, although on excavation all species showed some upward growth through the covering sand.

(b) Experimental burial, Method I: samples of the same eight species, grown in pots standing in water but not watered from above, were buried in sand to depths of 1, 2, 4, 5 and 6 cm. The maximum depth through which emergence took place was 4 cm., from which Ceratodon purpureus, Bryum pendulum and Brachythecium albicans reappeared. From shallower layers, however, a greater rate of emergence was shown by Tortula ruraliformis. Pseudoscleropodiun purum and Climacium dendroides did not survive depths greater than 2 cm., and 1cm. was the maximum for Hylocomium splendns and Rhytidiadelphus squarrosus.

Method II. Sample strips of fourteen species were placed in aquarium tanks and, apart from a small portion len exposed, were buried under a sand slope grading up to 7 cm. in depth. Watering was from above and the humidity was kept high by glass lids. The time taken for the appearance of shoots from increasing depths was recorded, also the periods required for reestablishment from increasing depths of 50% and 100% of the original shoot density. For species tested by both methods the results were in most cases similar. Marked powen of recolonization were also shown by Polytrichum piliferum, P. juniperinum and Pohlia annotina.

In P. annotina, Ceratodon purpureus and Dicramum scoparium re-establishment by means of vertically extending rhizoids producing protonemata at the surface is described.

The maximum depth from which the various species can emerge, the depths from which effective recolonization of the surface is achieved within a fairly short time, the ability to produce rhizoids in the overlying sand and the growth-form of the shoots on emergence are regarded as the most significant aspects of reaction to burial, in relation to the role of the species in their natural habitats.     

Early stages in biofilm development in methanogenic fluidized-bed reactors

Summary Biofilm development in methanogenic fluidized-bed reactors with sand as the carrier was studied on a laboratory scale. The microorganisms present in consecutive layers of the biofilm of mature sludge granules were preliminarily characterized on the basis of their morphology, element composition and adhesion capacity and were compared to bacteria which take part in the initial colonization of sand. The early phase of biofilm development was monitored with reactors receiving waste-waters containing different mixtures of volatile fatty acids and inoculated with fluidized-bed reactor effluent for different lengths of time. The results obtained indicate that facultative anaerobic bacteria abundantly present in the outermost biofilm layers of mature sludge granules are probably the main primary colonizers of the sand. Methanothrix spp. or other methanogens were rarely observed among the primary colonizers. The course of biofilm formation was comparable under the various start-up conditions employed including variations in waste-water composition, inoculation and anaerobicity. However, omission of waste-water and thus of substrate resulted in rapid wash-out of the attached biomass. Offprint requests to: W. Heinen