Effects of airborne sea salts on soil water acidification and leaching of aluminium in different forest ecosystems in Denmark

Studies on biogeochemical cycling of elements are performed in even aged forest ecosystems of Norway spruce, Sitka spruce and beech at several locations in Denmark. Episodes with high sea salt deposition and unusual low water surplus percolation caused extreme salt concentrations in the soil solutions. The changes were smallest beneath beech stands and most pronounced at the most salt-affected Sitka spruce stands. Contemporary, the pH drops and the Al³⁺ concentration increased above 20 mg L^-1 owing to cation exchange with Na⁺. The Cl^- and Al³⁺ concentrations reached levels reported as toxic for Norway spruce, but not for Sitka spruce and beech. The changes in the soil water chemistry must be considered as important factors for the reduced vitality in Norway spruce ecosystems in Denmark.     

Effect of wood ash application on the biomass distribution and physiological state of Norway spruce seedlings on sandy soils

The effect of wood ash applied as a fertiliser (0.25, 0.5 and 1 kg m^–2) to nutrient poor sandy soil on 4-year-old Norway spruce (Picea abies) growing in small-scale sample plots was studied. Analyses carried out with roots, stems, needles and shoots of different age showed that an increase in the pH level and K and Ca concentrations and a decrease in N and P concentrations in the soil was accompanied by a disbalance of nutrients in tree compartments. Stimulation of pigment synthesis in Norway spruce needles was observed, and no disbalances occurred in the pigment system (Chl a/Chl b, TChl/Car) guaranteeing normal process of photosynthesis. Biomass responses to wood ash application depended on the age of needles and shoots, being only slightly notable in current year organs. Inhibition of height growth of seedlings, but stimulation of root biomass was established.     

Comparison of Al speciation and other soil characteristics between meadow, young forest and old forest stands

The aim of this paper is to describe the influence of spruce (Picea abies) afforestation on soil chemical properties, especially on soil acidity and aluminium (Al) mobilization and speciation in soil. For our study we used a unique set of three adjacent plots, including a meadow and two spruce forest stands of different age, in otherwise comparable conditions. The plots were located in the region of Giant Mountains, north-eastern Czech Republic. In general, pH values decreased and Al concentrations increased significantly after afforestation. Speciation of KCl-extractable and water-soluble Al in soil samples was done by means of HPLC/IC method. The concentrations of Al(X)¹⁺ and Al(Y)²⁺ forms (in both extracts) are higher in humic and organically enriched (Bhs) horizons. The highest concentration of Al³⁺ in both extracts is in the B horizons of old forest.Generally, in all studied stands majority of Al in aqueous extract is in the Al(X)¹⁺ form, which indicates that a large amount of mobile Al is bound in organic complexes. It suggests that actual toxicity is rather low. On the other hand, we have proved that majority of KCl-extractable Al exists in Al³⁺ form. Thus we can conclude that disturbance of existing equilibrium may cause massive release of highly toxic Al³⁺ from soil sorption complex to the soil solution, and consequently it can endanger the whole ecosystem. Moreover, continuous soil acidification accelerated by anthropogenic factors leading to Al mobilization represents a chemical time bomb.     

Short-term effects of thinning and liming on forest soils of pitch pine and Japanese larch plantations in central Korea

The influences of thinning (50% of standing density) and liming (Ca+Mg, 2 Mg ha⁻¹) on soil chemical properties were investigated for 2 years (2001, 2002) in 40-year-old pitch pine (Pinus rigida Mill.) and 44-year-old Japanese larch (Larix leptolepis Gord.) plantations established on similar soils. In general, soil properties varied significantly among plantations and treatments. For both plantations, thinning significantly increased soil organic C (SOC) concentrations whereas there were no significant changes in soil pH and Ca and Mg concentrations. In addition, thinning increased total soil N and Na concentrations for the pitch pine plantation and available P concentration for the Japanese larch plantation in the second year after the treatment. Liming did not affect soil chemical characteristics for the pitch pine plantation except for Na concentration. However, for the Japanese larch plantation, liming significantly increased soil pH and K, Ca and Mg concentrations and decreased SOC and total soil N concentrations. For both plantations, soil Al concentration did not change after thinning and liming and decreased exponentially with increased pH values. The increases in SOC and total soil N concentrations after thinning were possibly due to increases in decomposition of organic matter and root death. Although differences were not statistically significant, soil available P concentration tended to increase at early stages of liming for both plantations. These results suggested that thinning and liming seemed to regulate soil chemical properties for pitch pine and Japanese larch plantations established on similar soils.     

Changes in soil properties after afforestation of former intensively managed soils with oak and Norway spruce

In many European countries, surplus agricultural production and ecological problems due to intensive soil cultivation have increased the interest in afforestation of arable soils. Many environmental consequences which might rise from this alternative land-use are only known from forest establishment on less intensively managed or marginal soils. The present study deals with changes in soil properties following afforestation of nutrient-rich arable soils. A chronosequence study was carried out comprising seven Norway spruce (Picea abies (Karst.) L.) and seven oak (Quercus robur L.) stands established from 1969 to 1997 on former horticultural and agricultural soils in the vicinity of Copenhagen, Denmark. For comparison, a permanent pasture and a ca. 200-year-old mixed deciduous forest were included. This paper reports on changes in pH values, base saturation (BS_eff), exchangeable calcium, soil N pools (N_min contents), and C/N ratios in the Ap-horizon (0–25 cm) and the accumulated forest floor. The results suggest that afforestation slowly modifies soil properties of former arable soils. Land-use history seems to influence soil properties more than the selected tree species. An effect of tree species was only found in the forest floor parameters. Soil acidification was the most apparent change along the chronosequence in terms of a pH decrease from 6 to 4 in the upper 5 cm soil. Forest floor pH varied only slightly around 5. Nitrogen storage in the Ap-horizon remained almost constant at 5.5 Mg N ha^–1. This was less than in the mineral soil of the ca. 200-year-old forest. In the permanent pasture, N storage was somewhat higher in 0–15 cm depth than in afforested stands of comparable age. Nitrogen storage in the forest floor of the 0–30-year-old stands increased in connection with the build-up of forest floor mass. The increase was approximately five times greater under spruce than oak. Mineral soil C/N ratios ranged from 10 to 15 in all stands and tended to increase in older stands only in 0–5 cm depth. Forest floor C/N ratios were higher in spruce stands (26.4) as compared to oak stands (22.7). All stands except the youngest within a single tree species had comparable C/N ratios.     

Root and needle litter decomposition responses to enhanced supplies of N and S in a Norway spruce forest in southwest Sweden

The effects of additions of ammonium sulfate (NS) on the decomposition of litter derived from Norway spruce roots (< 2 and 2 - 5 mm in diameter) in the humus and mineral soil layers (0 - 15 cm) of a Norway spruce stand in southern Sweden were investigated over a 6-year period. To this purpose, litterbags were incubated in the humus layer and in the mineral soil in June 1996, with roots collected from NS and control (C) plots incubated in the NS and C plots, respectively. The N concentrations in fine roots (< 2 mm) in the NS- plots were higher than those in 2 - 5 mm roots in both humus and mineral soil layers. In the humus layer, N concentrations in the fine roots in the C- and NS- plots were 12.8 and 15.7 mg g ^{? 1}, respectively. By the end of the fifth year the < 2 mm roots in humus layer had lost 48.5 and 50% of their mass in the C and NS plots, respectively, while the corresponding values for the 2 - 5 mm diameter class were 44 and 54%. The fresh root litter may be a sensitive indicator to responses to enhanced N and S deposition, although decomposition rates of both litter types are affected.     

Effects of freezing on rhizosphere and root nutrient content using two soil sampling methods

This study investigated how deep freezing affects the mineral nutrient content of roots and rhizosphere soil. Two different methods of separating the rhizosphere from the roots were used: i) a brushing method, where the rhizosphere soil was brushed off and ii) a washing method, where the rhizosphere was extracted together with the roots.When unfrozen material was used, the concentrations of K and Fe were significantly higher in the washing method as compared with the brushing method. When the material had been deep frozen, significantly higher concentrations of K, Fe, Mg, and Al were found in the extract from the washing method, indicating a considerable leakage from the roots. No significant differences were found between frozen and unfrozen material with the brushing method. In bulk soil, freezing resulted in increased concentrations of Mn, Al and Fe, even when no roots were present. The brushing method can be used for both frozen and fresh material, although fresh material is preferable. Extraction of soil plus roots cannot be recommended for deep frozen soil.     

Effects of ammonium sulphate application on the chemistry of bulk soil,rhizosphere, fine roots and fine-root distribution in a Picea abies (L.) karst. stand

The effect of ammonium sulphate application on the bulk and rhizosphere soil chemistry, elemental concentration of living fine roots (<2 mm in diameter), amounts of living and dead fine roots, root length density and specific root length density were investigated in a 28 year old Norway spruce stand in SW Sweden. The treatments started in 1988. Core samples of the LFH layer and mineral soil layers were sampled in control (C) and ammonium sulphate (NS) treatment plots in 1988, 1989 and 1990. Soil pH and NO₃-S and SO₄-S, Al, Ca, Mg, Mn and K concentrations were measured for both the bulk soil and rhizosphere soil.The pH-values of the bulk and rhizosphere soil decreased in 1989 and 1990 in NS plots compared to control plots, while the SO₄-S concentration increased. The Ca, Mg and K concentration increased in the NS treatment in almost all layers in the bulk and the rhizosphere soil. Ammonium ions may have replaced these elements in the soil organic matter. The NS treatment reduced Mg concentration in fine roots in all layers in 1990. The Al concentrations in the rhizosphere and bulk soil were higher in NS plots in all layers, except at 0–10 cm depth, both in 1989 and 1990. The Al content of living fine roots was higher in NS plots than C plots but the differences were not significant. The NS addition did not affect the P and K contents of fine roots in any soil layer, but the S concentrations of fine roots were significantly higher in NS plots in 1989 and 1990. The fine root necromass was higher in NS than in C in 1990, in the LFH layer, indicating a gradual decrease in the vitality of the fine roots. It was suggested that the NS treatment resulted in displacement of Mg and K from exchange sites in the LFH layer leading to leaching of these cations to the mineral soil. Further application of ammonium sulphate may damage the fine roots and consequently adversely affect the water and nutrient uptake of root systems.     

In-situ soil solution chemistry in an acid forest soil as influenced by growing roots of Norway spruce (Picea abies [L.] Karst.)

A new approach for non-destructive monitoring of soil solution chemistry in high spatial and temporal resolution for rhizosphere studies is presented. In a 5×10 mm grid, 30 micro suction cups (1mm) were installed in a rhizotron with Norway spruce (Picea abies [L.] Karst.) growing in low pH B-horizon soil. Roots grew through the grid, closely passing the suction cups. Soil solution composition before, during and after root passage was determined. For K⁺ and Mg²⁺ a significant decrease of soil solution concentration near root tips and elongation zones was observed, indicating a marked uptake of these elements. Mg²⁺ concentration was also significantly lowered when the root system aged, suggesting that this ion might also be taken up in older parts of the root system. No influence of growing roots was found on Na⁺-concentrations.     

Effects of soil fertilization and covering of the culture with plastic film on the provitamin A content of early lettuces

Summary Different growing conditions of early lettuces were assayed. Some plots of lettuces were grown covered with a perforated plastic sheet, and other plots were not covered. The soil of some plots was fertilized with a usual N+P+K+S fertilizer used at a normal rate, and the soil of other plots with a fertilizer containing only nitrogen at a rate about 40 times lower than the normal one for N. The total carotenes (provitamin A) contents of the ripe lettuces were measured. Covering with a plastic sheet always decreased the total carotenes contents. The N+P+K+S fertilizer used at normal rate increased, relatively to the nitrogen fertilizer lacking of P+K+S and used at low rate, the total carotenes contents of the non-covered lettuces, but had no or low effect on the total carotenes contents of the covered lettuces.     

Effects of liming on phosphate availability in acid soils

Summary The critical factors involved in the plant-soil-phosphorus-lime interaction are outlined and discussed. Conflicting reports suggest that the prior liming of highly weathered acid soils can result in an increase, a decrease, or no change in the availability of applied phosphate. Adsorption of phosphate by amphoteric soil surfaces generally decreases slowly as the pH is raised from 4.0 to 7.0. However, in soils initially high in exchangeable Al³⁺, liming results in the formation of new, highly active, phosphate adsorbing surfaces as the Al³⁺ ions precipitate as insoluble polymeric hydroxy-Al cation species. Thus, if an acid soil is reacted with lime and then phosphate, without intervening air drying, liming can increase phosphate adsorption. If the same limed soil is air dried before reaction with phosphate (e.g. adsorption isotherm studies), liming decreases phosphate adsorption. Apparently, air drying alters the surface characteristics of recently limed soils, probably by promoting the crystallization of the hydroxy-Al cation polymers as gibbsite.An important phenomenon, which is often overlooked, is that liming can increase phosphate availability by stimulating mineralization of soil organic phosphorus. However, at high soil pH values, the precipitation of insoluble calcium phosphates can decrease phosphate availability. Since Al toxicity is characterised by the inhibition of the uptake, translocation and utilization of phosphate by plants, liming often increases the utilization of soil phosphate by plants through amelioration of Al toxicity.When making lime recommendations or interpreting the data collected from lime-phosphate experiments, it is important to consider all the complex interacting soil and plant factors involved.     

Effect of liming on EUF-nutrient fractions in the soil,on nutrient contents of grape leaves and on grape yield

Summary In pot experiments with vine, liming significantly raised EUF-Ca 20°C as well as EUF-Ca 80°C values of an acid clay soil (pH 4.2). This resulted in a marked rise in Ca contents of vine leaves (Table 2). High amounts of K fertilizers without lime raised mainly the EUF-Ca 20°C values whereas the EUF-80°C values remained at a low level (Table 3). Liming lowered the EUF-K 20°C values and as a result the ratio EUF-K 80°C C/EUF-K 20°C increased from 0.7 to 1.0.High K applications raised the K content of the leaves at flowering stage but at grape ripening a marked decrease in K content was observed (Table 5). In contrast, the application of both lime and K fertilizer raised the K content of leaves at both flowering and ripening. Grape yield increased as well (Table 11).Liming raised the EUF-P values of the soil and to a lesser extent the P contents of leaves (Tables 6 and 7).High K applications without lime raised the Mn contents of leaves (Table 9), Exchange processes due to K fertilizer addition were reflected in increased EUF-Mn values (Table 9).The highest yield (three-year average) was obtained in a high K treatment (22 g K₂O/pot) in combination with lime (40 g CaO/pot).     

Experimental evidence of a deleterious soil microflora associated with Norway spruce decline in France and Germany

Norway spruce (Picea abies (L.) Karst.) seedlings were grown in a glasshouse pot experiment in soils from 11 declining and 7 healthy spruce stands from France and Germany. In soils from 9 declining stands, seedlings showed decline symptoms (needle yellowing). Soil pasteurization suppressed the symptoms, and reinoculation of the pasteurized soil with a rhizospheric extract from the corresponding stand re-induced yellowing. This suggests that a deleterious soil microflora is associated with spruce decline. The occurrence of this microflora seems to be correlated with the main chemical characteristics of the soils (low pH, low saturation of the adsorbing complex, low exchangeable Ca²⁺ and Mg²⁺, and high level of exchangeable Al). ei]R F Huettl     

Effects of liming and boron fertilization on mycorrhizas of Picea abies

Effects of liming and B fertilization on Norway spruce [Picea abies (L.) Karst.] mycorrhizas were studied in factorial field experiments. The lime was applied twice, about 30 years and 12 years before sampling (2000 and 4000 kg ha^-1 dolomite). B was applied at the rate of 1.5 kg B ha^-1 two years before sampling.Boron fertilization doubled the number of root tips in the top 10 mm of the humus layer. The proportion of dead short root tips was increased from 10 % in control plots to 29 % in the limed plots. Numbers of dead root tips were increased when both lime and B were applied. The % of mycorrhizas with external mycelium was slightly increased and the % of Piloderma croceum Erikss. and Hjortst. was decreased by lime. In conclusion, adverse effects of lime on mycorrhizas were found, which were ameliorated by B fertilization, but lime-induced B deficiency alone was not the only reason for the effects of lime on root mortality.     

Effects of pre-harvest soil acidification,liming and N fertilization on the survival,growth and needle element concentrations of Picea abies L. Karst. seedlings

There are concerns that the anthropogenic acidification of Swedish forest soils may have severe effects on forest yield, and it has been suggested that liming could be used to counter this problem. The aim of this study was to investigate the survival, growth and element concentrations of C+1 needles of Picea abies (L.) Karst. seedlings planted on plots that had been acidified (in 12 annual treatments totalling 600 or 1200 kg S ha^–1 in the form of elemental sulphur), limed (12×500=6000 kg lime ha^–1 in the form of CaCO₃) or N-fertilized (3×200=600 kg N ha^–1 in the form of urea) prior to harvest. Seedlings growing on plots given a combination of the N plus low S treatments were also tested. None of the treatments, given to triplicate plots, significantly influenced seedling survival during the first five growing seasons. Furthermore, none of the treatments significantly affected growth, although the average growth rate was slightly higher for limed plots. The survival and growth of the seedlings are discussed in relation to differences in the cover of field-layer vegetation between the treatments after the final felling. Needles from seedlings in the limed plots showed significantly lower concentrations of Mn and Al, and higher concentrations of Ca and Zn compared with needles from seedlings in the other plots (i.e. control, high S or N-treated). The K concentration in the needles was significantly higher in limed plots than in high-S plots. Changes of element concentrations observed in the soil, associated with the treatments, where in some cases reflected in the needle concentrations.