Boron: Spatial Distribution in an Area of North Nile Delta,Egypt

Boron (B) toxicity might be a problem, especially in dry regions of the world, however; its distribution still largely unappreciated and ignored by soil and crop scientists. Therefore, this study aimed to assess B spatial distribution in an area of northern Nile Delta, the most fertile and populated area in Egypt. Soil B was extracted by Mehilch-3 extraction and measured by inductively coupled plasma spectrometry (ICP). The mean B concentration was recorded as 5.19, 6.04, and 6.41 ug/g in surface (S), subsurface (Ss), and lower (L) layers, respectively. . The data were interpolated in ArcGIS software. The highest B concentration was observed in the central part of this area, which may be attributed to many reasons such as pollution sources and management practices. Our results indicated that more than 50% of the studied area highly concentrated in B, which represents a threat to soil and ecosystems in North Nile Delta.     

Micromorphology, chemistry, and mineralogy of bog iron ores from Poland

The influence of different land use history on the chemistry, mineralogy, and micromorphology of bog iron ores was studied in the vicinity of Warsaw, Poland. At three Holocene terraces of the Vistula River, eight profiles were chosen, which represent three different types of bog iron ore: (i) continuous hard layers (meadow, fallow at Wilanow), (ii) horizons with small ore fragments (arable land at Northern Praga), and (iii) soft bog iron ore (exploitation area at Brwinow). Chemical analyses of all bog iron horizons show a high content of Fe_d (up to 51%) with a Fe_o/Fe_d ratio from 0.19 to 0.58, indicating a mixture of crystalline iron and amorphous iron compounds. X-ray diffraction (XRD) analyses confirm the presence of ferrihydrite and goethite. The micromorphology of the bog ore at Wilanow shows a porous (vugh and channel) microstructure. The groundmass consists mainly of fine iron hydroxides. Compound coatings of radial distributed goethite needles and isotropic (“amorphous”) iron hydroxides line the pores. In many cases, several coatings of isotropic iron hydroxides, differing in colour intensity, fill the pores. Ploughing and draining at Northern Praga changed the continuous bog iron ore into small fragments embedded into an aggregate structure. It comprises of amorphous as well as crystalline iron compounds (large number of coatings of radial fibrous goethite in pores and channels). In some cases, a single pore can contain several generations of crystalline goethite. The higher crystallinity of the iron oxides fits very well to the lower Fe_o/Fe_d ratios compared to Wilanow. The differences can be attributed to the drainage, subsequent lower groundwater level, and better aeration, respectively, at Northern Praga. No hard bog iron ore is present at Brwinow because of exploitation, sporadically fragments of hard bog ore may be encountered in the topsoil. However, soft bog ore is still developing in subsoils. It shows a vughs microstructure. Besides goethite, manganese impregnations on the crystalline forms of goethite, and isotropic iron compounds, its groundmass also contains vivianite as well as siderite. The latter can be attributed to a more reductive environment.     

Holocene paleosols and colluvial sediments in Northeast Tibet (Qinghai Province,China): Properties,dating and paleoenvironmental implications

Colluvial deposits consisting of silts and loams were detected in several climatologically different areas of NE Tibet (3200–3700 m a.s.l.). Layering, distinct organic content and low content of coarse matter as well as location in the relief revealed an origin from low-energy slope erosion (hillwash). Underlying and intercalated paleosols were classified as Chernozems, Phaeozems, Regosols and Fluvisols. Fifteen radiocarbon datings predominant on charcoal from both colluvial layers and paleosols yielded ages between 8988 ± 66 and 3512 ± 56 uncal BP. Natural or anthropogenic factors could have been the triggers of the erosional processes derived. It remains unclear which reason was mainly responsible, due to controversial paleoclimatic and geomorphic records as well as insufficient archaeological knowledge from this region. Determinations of charcoal and fossil wood revealed the Holocene occurrence of tree species (spruce, juniper) for areas which nowadays have no trees or only few forest islands. Thus large areas of NE Tibet which are at present steppes and alpine pastures were forested in the past.     

Emissions of CO2, CH4 and N2O from Southern European peatlands

Peatlands play an important role in emissions of the greenhouse gases CO₂, CH₄ and N₂O, which are produced during mineralization of the peat organic matter. To examine the influence of soil type (fen, bog soil) and environmental factors (temperature, groundwater level), emission of CO₂, CH₄ and N₂O and soil temperature and groundwater level were measured weekly or biweekly in loco over a one-year period at four sites located in Ljubljana Marsh, Slovenia using the static chamber technique. The study involved two fen and two bog soils differing in organic carbon and nitrogen content, pH, bulk density, water holding capacity and groundwater level. The lowest CO₂ fluxes occurred during the winter, fluxes of N₂O were highest during summer and early spring (February, March) and fluxes of CH₄ were highest during autumn. The temporal variation in CO₂ fluxes could be explained by seasonal temperature variations, whereas CH₄ and N₂O fluxes could be correlated to groundwater level and soil carbon content. The experimental sites were net sources of measured greenhouse gases except for the drained bog site, which was a net sink of CH₄. The mean fluxes of CO₂ ranged between 139 mg m⁻² h⁻¹ in the undrained bog and 206 mg m⁻² h⁻¹ in the drained fen; mean fluxes of CH₄ were between −0.04 mg m⁻² h⁻¹ in the drained bog and 0.05 mg m⁻² h⁻¹ in the drained fen; and mean fluxes of N₂O were between 0.43 mg m⁻² h⁻¹ in the drained fen and 1.03 mg m⁻² h⁻¹ in the drained bog. These results indicate that the examined peatlands emit similar amounts of CO₂ and CH₄ to peatlands in Central and Northern Europe and significantly higher amounts of N₂O.     

Comparison of Soil Properties and Microbial Activities between Air-Dried and Rewetted Desert and Oasis Soils in Northwest China

An air-drying and rewetting (AW) experiment was used to examine the responses of soil properties and microbial activities to abrupt alteration of water availability between desert and oasis soils in northwest China. The results revealed that AW increased soil pH and available nitrogen and phosphorus but decreased soil organic matter in the desert, while available phosphorus increased and available nitrogen decreased in the oasis. This AW also caused a burst of microbial activity in both desert and oasis soils, and the magnitude of the AW effect was correlated with the extent of soil rewetting, incubation temperature, land use, and the interaction between rewetting moisture and incubation temperature. The responses of soil properties and microbial activity to AW were greater in the desert than in the oasis. Different soil properties and microorganism composition resulted from land-use change and were likely to be the causes of the different responses to AW in the desert and oasis soils.     

The use of micromorphology in soil pollen analysis: The interpretation of the pollen content of slope deposits in Galicia, Spain

Humic horizons of soil profiles often contain pollen and spores. Comparison of the sequence of pollen associations of soil profiles with pollen zones of reference diagrams offers palyno-ecological information, relevant for reconstruction of landscape ecological development. In palynological studies of semiterrestrial and aquatic deposits, pollen is considered to be part of the sediment and anaerobic conditions in water-saturated deposits promote its conservation. This is not true for pollen in soils. Aerobic conditions in drained soils result in bio-oxidation of unprotected pollen grains. Interpretation of soil pollen associations requires knowledge of the processes of infiltration and conservation of pollen grains in the soil material. Micromorphology is an important technique to investigate these processes. This is demonstrated in a case study of polycyclic slope deposits in Galicia (Spain). The buried cambisols, in pleistocene solifluction deposits, contain post-sedimentary infiltrated pollen. The pollen associations reflect successive phases in soil ecological development. The holocene colluvial deposits contain syn-sedimentary incorporated pollen. The pollen associations reflect environmental conditions during the deposition of colluvial layers.     

Properties and spatial distribution of microbiotic crusts in the Negev Desert,Israel

Playing a cardinal role in surface stabilization and in carbon and nitrogen fixation, microbiotic crusts play a crucial role in arid regions where they may serve as useful biomarkers for wind power and wetness duration. This is especially the case on relatively unstable and infertile sand dunes in the Negev Desert where high correlations between the crust chlorophyll content and the daytime wetness duration were found. Yet, only scarce data are available as to the possible link between the chlorophyll content and other physical (color, thickness, strength, crack density, surface roughness and infiltrability) and biological (protein, carbohydrate, organic matter and species composition) factors, which determine, in turn, the crust type and its effect upon geomorphological and ecological processes. No data are available on crust type distribution. These were the aims of the current research.     

Host specificity and phenotypic diversity of Rhizobium strains nodulating Leucaena, Acacia, and Sesbania in Egypt

Phenotypic diversity was studied among 13 Rhizobium strains selected from a total of 160 Rhizobium isolates from root nodules of Leucaena leucocephala. Two strains from Acacia saligna and two strains from Sesbania sesban plants were included in the examination for host range in the greenhouse. The Rhizobium sp. (Leucaena) strains were different from the reference strains and fell into three distinct groups for the utilization of 95 different carbon sources. Four of the best symbionts constituted a group, the majority of the strains fell into a second group, and strain DS 91 was the only member of the third group. Strains were effective symbionts for their original hosts. Nine strains were tolerant to elevated temperature (>42°C), and three strains were resistant to high salinity (>3% NaCl). All Rhizobium sp. (Leucaena) strains effectively nodulated L. leucocephala and L. culensii, but nitrogen fixation was greater with L. leucocephala than with L. culensii. These strains failed to form effective symbioses with two other species of Leucaena (L. retusa and L. divursiflora) or with alfalfa, Medicago sativa. Rhizobium sp. (Leucaena) strains DS 65, DS 78, and DS 158 nodulated and efficiently fixed nitrogen with Phaseolus vulgaris, with DS 65 showing the highest symbiotic capability. Strain DS 65 also nodulated and fixed nitrogen with Glycine max and Vigna sinensis. Nodulation of Leucaena by two Bradyrhizobium sp. (Acacia) strains was sparse. Strain DS 101 from Sesbania formed nodules on Leucaena, whereas the other strain from Sesbania, DS 110, failed to nodulate this genus. Received: 30 September 1996     

Influence of Rootstocks,pH, Iron Supply (in Nutrient Solutions) and Agrobacterium radiobacter on Chlorophyll and Iron Concentration in Leaves of a Peach Variety

In this study, the influence of rootstocks, pH, iron (Fe) supply (in nutrient solutions), and Agrobacterium radiobacter on the leaf chlorophyll and Fe concentration of the peach cultivar ‘Sun Crest’ was investigated. The results showed that chlorophyll index (SPAD-502) and active Fe differed significantly at different pH levels. Chlorophyll index was highest at pH 6.0 and 9.0 and lowest at pH 7.0 and 8.0 Leaf active Fe concentration was highest at pH 6.0 and 7.0 Significant differences between rootstocks and interactions were also found. Chlorophyll index was highest in the leaves of GF677, Antafuel and MRS 2/5, while the leaves of seedling had the lowest chlorophyll index and chlorophyll a and b concentration. The chlorophyll index in the leaves of St. Julien 655/2 did not differ from those of MRS 2/5. However, seedling had the highest leaf active Fe concentration. Supply of trees with different Fe levels (in solutions) did not affect positively the leaf chlorophyll index, chlorophyll a and b concentration, or active Fe concentration. The leaf chlorophyll index and active Fe in the rootstocks GF677, Antafuel, and Siberian C were significantly reduced in trees inoculated with Agrobacterium radiobacter.     

Effects of mycorrhiza colonization on growth,root exudates,antioxidant activity and photosynthesis trait of cucumber grown in Johnson modified nutrient solution

Mycorrhiza can improve plant growth and increase nutrient uptake. This study was conducted as factorial experiment based on complete random design (CRD) to study effects of mycorrhiza inoculation under limited iron (Fe) condition on antioxidant activity, phenol content and photosynthesis trait of cucumber (Cucumis sativus cv. N3). Treatments were Johnson modified nutrient solution (MNS) with 25% Fe (MNS1) = 0.57 mg/L Fe, 50% (MNS2) = 1.14 mg/L Fe and 100% (MNS3) = 2.3 mg/L Fe and mycorrhiza inoculation (M+) and non-mycorrhiza inoculation (M?) with 3 replications under hydroponic conditions. The results showed that plant growth and shoot phenol content decreased in the MNS1 treatment; whereas phenol content of the root exudates and antioxidant activity significantly increased in this treatment. All photosynthesis attribute increased in the MNS3 treatment. Mycorrhiza inoculation increased plant growth, phenol content, antioxidant activity and photosynthesis trait of cucumber. Also, mycorrhiza inoculation enhanced SPAD value in the MNS2 treatment and photosynthesis rate, transpiration and mesophyll conductance in all the modified nutrient solutions. Moreover, mycorrhiza symbiosis was stimulated by the internal carbon dioxide (CO₂) content of the stomata in the MNS2 and MNS3 treatments. Furthermore, Mycorrhiza inoculation improved phenol content of the shoots and roots in all the nutrient solutions, whereas antioxidant activity was affected by mycorrhiza inoculation only in the MNS2 treatment.     

Fluxes and storage of fine-grained sediment and associated contaminants in the Na Borges River (Mallorca,Spain)

Samples of suspended and fine channel bed sediment were used to examine the spatial and temporal variability in the amount of fine-grained sediment and associated contaminants temporarily stored in the Na Borges River (319 km²) in Mallorca and the relationship of such channel storage to the fluxes of fine sediment and associated contaminant through the system. This Mediterranean groundwater-dominated river drains a predominantly agricultural catchment, although urbanisation during the twentieth century has changed the catchment hydrology. A re-suspension technique was used to obtain estimates of channel storage at monthly intervals during the 2004–2005 hydrological year at eight locations along the main stem of the stream (i.e. 26 km). The estimates of fine sediment storage ranged between 0 and 13,000 g m^− 2, with a mean value of 2400 g m^− 2. Only Cu exceeded the critical threshold (36 μg g^− 1), established by existing guidelines for the contaminant content of fluvial sediment. The results demonstrated significant spatial and temporal variability, in response to the influence of urban point sources, agricultural practises, seasonal groundwater interactions and the first-flush effect. The amount of fine sediment entering storage during the study period was 515.2 t, representing the net increase in storage over the study period. As a result, the mean specific storage was 21 t km^− 1. Suspended-sediment load and temporary fine sediment storage are the two basic components of the channel sediment budget that interact to determine sediment transport through a channel system, and they can therefore be used to compute the total input of sediment and associated contaminants to the system. Accordingly, storage values were compared with estimates of suspended sediment load and associated contaminant load values at three measuring stations along the river. During the study period, storage in the main channel system represented 87% of the sediment input and 68% of the contaminant input, indicating that deposition was more important than transport. The low gradient of the main channel and the low return period (i.e. 0–2.5 years) of the flood events that occurred during the study period meant that remobilised bed sediment and associated contaminants were redeposited downstream rather than being flushed to the catchment outlet as suspended sediment. Furthermore, the river bed is dry during the summer months, allowing sealing and crusting processes to stabilise the sediment deposited during the wet season and thereby reduce its availability for remobilisation at the beginning of the next wet season. Together, these factors promote sediment deposition and storage, with the result that sediment progressively accumulate over several hydrological years until a major flood event (i.e. return period ≈ 5 years) evacuates the stored sediment.     

Growth,Biomass Production,and Nutrient Composition of Eucalyptus Seedlings Irrigated with Municipal Effluent in Loamy Sand Soil of Indian Desert

Abstract

An experiment comprised of five treatments [T₁ = municipal effluent @ 1 PET (without plant), T₂ = municipal effluent @ (1/2) PET, T₃ = municipal effluent @ 1PET, T₄ = municipal effluent @ 2 PET, and T₅ = good (canal) water @ 1 PET] was carried out with Eucalyptus camaldulensis. The aim was to utilize sewage water in growing tree plantation and to increase the supply of fuel wood to the growing urban population. Height, collar diameter, and number of branches were monitored periodically. Biomass and leaf and root growth were recorded at 24 months of age. Mineral composition and uptake were monitored to observe their removal from the soil. Increase in rate of municipal effluent application was associated with better tree growth compared to irrigation with canal water. At 24 month age, the T₄ was the best treatment in which E. camaldulensis attained 393 cm height and 6.6 cm collar diameter. Height and collar diameter of T₂ seedlings did not differ (P > 0.05) with respective parameters in T₅ treatment. Collar diameter increased by 1.2 times in T₃ treatment. Number of leaves and biomass increased with increase in quantity of municipal effluent. Modeling of total biomass against quantity of municipal effluent application produced better result with non‐linear fitting than the linear one. Mineral composition and accumulation in different parts of the seedling was high and varied with the quantity and nutrient composition of irrigation water. Concentration of total nitrogen (N), phosphorus (P), copper (Cu), iron (Fe), manganese (Mn), and zinc (Zn) was high in the municipal effluent irrigated seedlings compared to the good water irrigated seedlings. However, sodium (Na), potassium (K), calcium (Ca), and magnesium (Mg) were high in the seedlings of T₅ compared to T₂ and T₃ treatments. Municipal effluent did not show any toxicity to the seedlings up to 24 months age. Conclusively, the municipal effluents could be recommended as a good source of water and nutrient for tree biomass production to fulfill the requirement of fuel need in the suburban area.     

Staging of Pacific flyway brant in relation to eelgrass abundance and site isolation, with special consideration of Humboldt Bay, California

Spring distributions of black brant (Branta bernicla nigricans) are closely related to that of their primary food plant, eelgrass (Zostera marina). Using historical (1931-2001) brant data from Humboldt Bay, California, we show that proportional use of two main feeding areas in the bay strongly reflects food abundance. We used multiple regression to investigate whether the spatial relationship between brant and eelgrass holds at the flyway level. We related peak brant numbers at 11 staging areas in the Pacific flyway to the sites' Z. marina abundance and isolation from other important staging areas. We explained 90% of the variation in peak brant numbers across sites with these variables; isolated bays with high eelgrass abundance supported the most brant. Our results emphasize the importance of protecting large eelgrass habitats along the Pacific Coast, particularly in bays that are geographically isolated from other large staging areas.     

Influence of dew on biomass and photosystem II activity of cyanobacterial crusts in the Hopq Desert, northwest China

Dew is an important water source for desert organisms in semiarid and arid regions. Both field and laboratory experiments were conducted to investigate the possible roles of dew in growth of biomass and photosynthetic activity within cyanobacterial crust. The cyanobacteria, Microcoleus vaginatus Gom. and Scytonema javanicum (Kütz.) Born et Flah., were begun with stock cultures and sequential mass cultivations, and then the field experiment was performed by inoculating the inocula onto shifting sand for forming cyanobacterial crust during late summer and autumn of 2007 in Hopq Desert, northwest China. Measurements of dew amount and Chlorophyll a content were carried out in order to evaluate the changes in crust biomass following dew. Also, we determined the activity of photosystem II(PSII) within the crust in the laboratory by simulating the desiccation/rehydration process due to dew. Results showed that the average daily dew amount as measured by the cloth-plate method (CPM) was 0.154 mm during fifty-three days and that the crust biomass fluctuated from initial inoculation of 4.3 μg Chlorophyll a cm⁻² sand to 5.8-7.3 μg Chlorophyll a cm⁻² crust when dew acted as the sole water source, and reached a peak value of approximately 8.2 μg Chlorophyll a cm⁻² crust owing to rainfalls. It indicated that there was a highly significant correlation between dew amounts and crust moistures (r = 0.897 or r = 0.882, all P < 0.0001), but not a significant correlation between dew and the biomass (r = 0.246 or r = 0.257, all P > 0.05), and thus concluded that dew might only play a relatively limited role in regulating the crust biomass. Correspondingly, we found that rains significantly facilitated biomass increase of the cyanobacterial crust. Results from the simulative experiment upon rehydration showed that approximately 80% of PSII activity could be achieved within about 50 min after rehydration in the dark and at 5 °C, and only about 20% of the activity was light-temperature dependent. This might mean that dew was crucial for cyanobacterial crust to rapidly activate photosynthetic activity during desiccation and rehydration despite low temperatures and weak light before dawn. It also showed in this study that the cyanobacterial crusts could receive and retain more dew than sand, which depended on microclimatic characteristics and soil properties of the crusts. It may be necessary for us to fully understanding the influence of dew on regulating the growth and activity of cyanobacterial crust, and to soundly evaluate the crust's potential application in fighting desertification because of the available water due to dew.     

The impact of harvester ants on decomposition, N mineralization, litter quality, and the availability of N to plants in the Mojave Desert

In arid areas of North America, nests of the seed-harvesting ant Pogonomyrmex rugosus tend to be elevated in mineral nitrogen and other soil nutrients relative to other microhabitats. We investigated the roles of decomposition, N mineralization, and plant nutrient uptake in maintaining high standing stocks of nutrients in P. rugosus ant nests. Decomposition rates of standard cellulose substrates placed on the surface of ant nests and other desert microhabitats suggest that conditions found in ant nests and bare areas are conducive to higher rates of decomposition than conditions under shrubs. In laboratory incubations of moist soil, net N mineralization rates were significantly higher in soil from ant nests than from bare areas and under two of three plant species. Net N mineralization rates measured in situ were much lower than those measured in laboratory incubations, but ant nest soil still exhibited higher rates at one of two sites. Litter collected from ant mounds, composed chiefly of seed chaff, was similar in N content to litter collected from underneath the dominant plant species, but had a significantly higher mean δ¹⁵N. Using this distinctive isotope signature as a tracer, we found no evidence that large perennial shrubs tap ant nests as a source of N. An invasive, annual grass species was significantly enriched in ¹⁵N, had higher leaf %N, and produced more seeds when growing on the mound than when growing several meters away; however P. rugosus nest surfaces are typically free of such annuals. We conclude that both high rates of nutrient cycling relative to other Mojave Desert microhabitats and low N utilization by the surrounding vegetation contribute to high standing stocks of mineral N in P. rugosus nests.     

Long-term response of spring flora to chronic herbivory and deer exclusion in Great Smoky Mountains National Park, USA

Chronic herbivory by white-tailed deer (Odocoileus virginianus Zimmerman) can have profound impacts on the function and structure of forest ecosystems. We examined the combined influence of intense herbivory associated with a deer population eruption and chronic herbivory by the post eruption population on the spring flora of Cades Cove, Great Smoky Mountains National Park. During the 1970s the deer population reached a peak of 43 deer per km², from which it has slowly declined in recent decades. To examine the influence of intense herbivory, we compared the abundance and flowering rates of early flowering plants in Cades Cove to a nearby reference site with similar bedrock geology, vegetation, and disturbance history but contrasting history of deer abundance. Our results suggest that significant changes (p ? 0.05) in the diversity, evenness, and species richness of the spring flora occurred during the eruptive phase. Trillium spp. and other liliaceous species appeared to be disproportionately impacted. Comparisons between control and exclosure plots established after the deer population eruption indicate that recovery has been largely restricted to species that were able to persist under intense herbivory. These species have increased in number in exclosures, suggesting continued impacts by deer on the plant community outside the exclosures. Little to no recolonization by browse sensitive species was observed. Consequently, to restore the natural diversity of early flowering plants once present in Cades Cove, active restoration may be necessary in addition to maintaining deer densities below current levels.     

Characteristics of free sesquioxides and humic acids in soil distributed under Warm-temperate forest climate in Nyu mountains,Fukui Prefecture,Central Japan

The activity and crystallinity ratios of free iron oxides, and the ΔlogK and RF values of humic acids were analyzed in five soil types in the Nyu mountains, Fukui Prefecture, to examine the relation between the zonality of soils and the bioclimatic conditions under the Warm-temperate deciduous broad-leaved forest climate. The characteristics of free iron oxides and humic acids were as follows: The Dark red soil, Kunimidake series was a Dark Red soil under the Cool-temperate deciduous broad-leaved forest climate; the Dry brown forest soil (reddish), Tega series was a Yellow-Brown Forest soil under the Warm-temperate deciduous broad-leaved forest climate; the Dry brown forest soil, Takasu-1 series and the Yellow soil, Yada series were Yellow-Brown Forest soils under the Warm-temperate lucidophyllous forest climate; and the Red soil, Oshibayama series and the lower parts of the Tega series were paleo-red soils. These results indicated that zonal soils under the Warm-temperate deciduous broad-leaved forest climate were Yellow-Brown Forest soils in the Nyu mountains, Fukui Prefecture. The Dark red soil, Kunimidake series corresponded to a Hyperdystri-Rhodic Cambisol of World Reference Base for Soil Resources, WRB (FAO, ISRIC, and ISSS: World Soil Resources Reports 84, 1998). The Dry brown forest soil (reddish), Tega series, the Dry brown forest soil, Takasu-1 series, and the Red soil, Oshibayama series were compared with the Hyperdystri-Chromic Cambisol (WRB). The Yellow soil, Yada series was a Hypereutri-Chromic Cambisol (WRB).     

Role of soil organic matter in a desert soil on plant response to silver,tungsten, cobalt,and lead

Abstract

Barley plants grown in a soil very low in organic matter had higher concentrations of Mn, Cu, Zn, and Mo than when the plants were grown in soil considerably higher in soil organic matter. Application of some heavy metals (Co, W, Ag) resulted in much more severe phytotoxicity on low organic matter soil than on high organic matter soil. FeDTPA (ferric diethylene triamine pentaacetate acid) increased Fe levels in plants much more on low organic matter soil than on high organic matter soil. Low organic matter soil resulted in a lower Cs level from the applied Cs than from the high organic matter soil. Sulfur increased Mn concentration of plants even though all the soil was not neutralized.     

Waterlogging Induces High to Toxic Concentrations of Iron,Aluminum, and Manganese in Wheat Varieties on Acidic Soil

Six wheat varieties with different tolerance to waterlogging were studied in acidic soil (pH 4.5), neutral soil, and potting mix (pH 6.7–7.8) under controlled conditions. Waterlogging for 49 d reduced shoot dry weight by 48% to 85% compared with drained treatments. The ranking of varieties for waterlogging changed under different soils, and this change explains why waterlogging tolerance of these varieties may vary in different environments. In waterlogged acidic soil, shoot concentrations of aluminum (Al), manganese (Mn), and iron (Fe) increased by two- to 10-fold, and in some varieties they were above critical concentrations compared with plants in drained soil. These elements decreased or remained the same in shoots of plants grown in waterlogged neutral soil. Marginal nitrogen (N) deficiency was induced in most varieties in all soil types. The results support the importance of screening in soils from the target environment for accurate germplasm characterization for waterlogging tolerance.     

Impact of Cultivation Practices in Oasis Agriculture on Soil Fertility Dynamics and the Relationship with Cotton Nitrogen-Use Efficiency in the Southern Rim of the Tarim Basin,Xinjiang, China

Twenty croplands in the Cele Oasis, at the southern margin of the Tarim Basin of Xinjiang, representing 100, 80, 30, 15, and 10 years of cultivation, were selected to investigate the relationship between soil fertility and nitrogen-fertilizer-use efficiency (NUE) of cotton and its changes over time. After long-term cultivation, significant increases were observed in soil organic matter (SOM) and total macronutrients. The key factors contributing towards the soil fertility index (SFI) were SOM, available potassium (AK), and phosphorus. The values of SFI declined in the following order: 80 (0.95) > 100 (0.68) > 30 (0.43) > 15 (0.41) > 0 (0.37) > 10 (0.34) years. No significant relationship was found between SFI and NUE. A significant correlation was observed among cotton yield, partial factor productivity from applied N, and AK. This indicates that the variation of AK content plays the most important role in soil fertility and cotton yield. Moderate K fertilization is recommended in the oasis croplands.