Chemical soil conditions in pristineNothofagus forests of New Zealand as compared to German forests

In many German forest soils low base saturation of CEC in deeper soil layers was reported and acidic deposition is seen as the major cause of these findings. To test this hypothesis we sampled 5 New Zealand forest soils from pristine beech (Nothofagus fusca, N. menziesii, N. solandri) sites under climatic and geological conditions comparable to higher elevations in Germany. The soils developed from granite and greywacke. Soil samples were analyzed for pH and the exchangeable cations were extracted with 1M NH₄Cl. The base saturation of all soil profiles was very low, even in deeper layers and was thus similar to the patterns found in many German forest soils. The pH was generally higher in the New Zealand soils as compared to Germany. The reason for the depletion of base cations in deeper soil layers of New Zealand forest soils is most likely the leaching of base cations with HCO₃ ^- resulting from the dissociation of carbonic acid in connection with high amounts of seepage. Thus, under high rainfall conditions, the low base saturation found in deeper layers of forest soils cannot exclusively be attributed to the effects of acidic depositions and land use. ei]Section editor: R F Huettl     

Effects of long-term soil acidification due to nitrogen fertilizer inputs in Wisconsin

Agroecosystems are domesticated ecosystems intermediate between natural ecosystems and fabricated ecosystems, and occupy nearly one-third of the land areas of the earth. Chemical perturbations as a result of human activity are particularly likely in agroecosystems because of the intensity of that activity, which include nutrient inputs intended to supplement native nutrient pools and to support greater biomass production and removal. At a long-term fertility trial in South-Central Wisconsin, USA, significant increases in exchangeable acidity were accompanied by decreases in cation exchange capacity (CEC), base saturation, and exchangeable Ca²⁺ and Mg²⁺ with application of ammoniacal N fertilizer. Plant analysis shows that a considerable portion of the alkalinity generated by assimilation of N (and to a lesser extent by S) is sequestered in the above-ground plant parts as organic anions and is not returned to the soil if harvested. Elemental analysis of Ca-saturated soil clays indicates an loss of 16% of the CEC of the soil clay and minor increases in Fe and Al. The reversibility of these changes due to prolonged acidification is doubtful if the changes are due to soil weathering.     

Interacting effects of wildfire severity and liming on nutrient cycling in a southern Appalachian wilderness area

Aims

Wilderness and other natural areas are threatened by large-scale disturbances (e.g., wildfire), air pollution, climate change, exotic diseases or pests, and a combination of these stress factors (i.e., stress complexes). Linville Gorge Wilderness (LGW) is one example of a high elevation wilderness in the southern Appalachian region that has been subject to stress complexes including chronic acidic deposition and several wildfires, varying in intensity and extent. Soils in LGW are inherently acidic with low base cation concentrations and decades of acidic deposition have contributed to low pH, based saturation, and Ca:Al ratio. We hypothesized that wildfires that occurred in LGW followed by liming burned areas would accelerate the restoration of acidic, nutrient depleted soils. Because soils at LGW had extremely low concentrations of exchangeable Ca²⁺ and Mg²⁺ dolomitic lime was applied to further boost these cations. We evaluated the effectiveness of dolomitic lime application in restoring exchangeable Ca²⁺ and Mg²⁺ and subsequently increasing pH and Ca:Al ratio of soils and making Ca and Mg available to recovering vegetation.

Methods

Five treatment areas were established: severely burned twice (2000 & 2007) with dolomitic lime application (2xSBL); moderately burned twice with lime application (2xMBL); severely burned twice, unlimed (2xSB); moderately burned once (2000), unlimed (1xMB); and a reference area (REF; unburned, unlimed). In 2008 and 2009, we measured overstory, understory, and ground-layer vegetation; forest floor mass and nutrients; and soil and soil solution chemistry within each treatment area.

Results

All wildfire burned sites experienced substantial overstory mortality. However, understory biomass doubled between sample years on the most recently burned sites due to the rapid regrowth of ericaceous shrubs and prolific sprouting of deciduous trees. Burning followed by lime application (2xSBL and 2xMBL) significantly increased shallow soil solution NO₃-N, but we found no soil solution NO₃-N response to burning alone (2xSB and 1xMB). Surface soil base saturation and exchangeable Ca²⁺ were significantly affected by liming; Ca²⁺ concentrations were greater on 2xMBL and 2xSBL than 2xSB, 1xMB and REF. There was a smaller difference due to moderate burning along with greater soil Ca²⁺ on 1xMB compared to REF, but no difference between 2xSB and REF. Surface and subsurface soil exchangeable Al³⁺ were lower on 2xSBL than 2xSB, 2xMBL, 1xMB, and REF. Liming decreased soil acidity somewhat as surface soil pH was higher on the two burned sites with lime (pH?=?3.8) compared to 2xSB without lime (pH?=?3.6).

Conclusions

Liming resulted in decreased soil Al³⁺ on 2xSBL coupled with increased soil Ca²⁺ on both 2xSBL and 2xMBL, which improved soil Ca/Al ratios. However, the soil Ca/Al ratio response was transitory, as exchangeable Al³⁺ increased and Ca/Al ratio decreased over time. Higher lime application rates may be necessary to obtain a substantial and longer-term improvement of cation-depleted soils at LGW.     

The effect of afforestation with Scots pine (Pinus silvestris L.) of sandy post-arable soils on their selected properties. I. Physical and sorptive properties

Despite the extensive literature on the effect of afforestation of former arable land on soil properties, we still do not fully understand whether the changes proceed in the same direction and at the same rate or how long it takes to achieve a state of soil equilibrium typical of a natural forest ecosystem. Therefore, as part of a comparative study of post-arable sandy soils (Distric Arenosols) afforested with Scots pine (Pinus silvestris L.) with respect to arable soils and soils of continuous coniferous forests, a range and direction of the changes in some of their physical and sorptive properties were determined. The studies were carried out in SE Poland, 51°30′–51°37′N, 22°20′–22°35′E. Ten paired sites of the afforested soils (five with 14- to 17-year-old stands and five with 32- to 36-year-old stands) with adjacent cultivated fields and five sites of continuous forests with present stands of ca. 150 years were selected. For the physical properties, undisturbed soil cores were sampled from the upper part of each horizon while in the case of A horizon of the afforested soils, from two layers: 0–5 cm and 10–15 cm. For the remaining analyses, soil was taken from the whole thickness of the master horizons and in the case of A horizon of the afforested soils, from three layers: 0–5, 5–10 and 10–20 cm. The following properties were analysed: texture, bulk density (BD), total porosity (TP), water content at potential of −0.098, −9.81 and −49.03 kPa, hydrolytic acidity (Ha), base exchangeable cations: Ca²⁺, Mg²⁺, K⁺, Na⁺, total exchangeable bases (TEB), cation exchange capacity (CEC) and base saturation (BS). Afforestation caused a decrease in BD, an increase in TP and had no affect on water properties when compared with the cultivated soils. The changes referred to the A horizon, particularly to its 0–5 cm layer, and were related to the stand age. The CEC gradually rose in the former plough layer, beginning from the uppermost part, but during the first two decades its increase in the 0–5 cm layer was offset by a decline in the deeper layers. No substantial increase in CEC, in the whole A horizon, was recorded until three to four decades of afforestation. Afforestation also invoked an increase in Ha, a drop in TEB, particularly Ca²⁺, Mg²⁺ and K⁺, and reduction in BS. No differences between soils for all the studied properties for B and C horizons were observed. It was noted that more than 30 years after afforestation, the TEB and BS as well as Ca²⁺, Mg²⁺ and K⁺ content differed substantially, but in most cases not significantly, from their values in the cultivated soils and reached a level more similar to the soils of continuous coniferous forests. With respect to the water properties, Ha and CEC of the afforested soils still resembled arable soils, whereas regarding the TP and BD, they were somewhere in the middle. This implies that to understand changes in the soil properties resulting from afforestation and to predict future trends, long-term research is needed.     

Pools and composition of soils in the alpine zone of the Tatra Mountains

The basic physical, chemical, and biochemical properties of mountain soils were determined in alpine-zone meadow and moraine areas of the Tatra Mountains (Slovakia, Poland) in 2000–2001. The amount of soil (dry weight soil < 2 mm) varied from 38 to 255 kg m^?2 (average of 121 kg m^?2) in alpine meadows and averaged 13 kg m^?2 in moraine areas. Concentration of organic C was the parameter that most strongly and positively correlated with N, P, S, effective cation exchange capacity (CEC), exchangeable base cations, exchangeable acidity, and all biochemical parameters (C, N, and P in microbial biomass and C mineralisation rates). The relationship between C and P was less straightforward due to inorganic P forms associated with Fe and Al oxides. The average pools of C, N, P, and S, were respectively 696, 41, 2.9, and 1.9 mol m^?2 (i.e., 84, 5.7, 0.91 and 0.61 t ha^?1) in meadow soils, and 38, 2.1, 0.45 and 0.12 mol m^?2 (i.e., 4.5, 0.30, 0.14 and 0.04 t ha^?1) in moraine areas. Soil pH was generally low, with the lowest pH_{H 2 O} values (3.8–4.9) in the A-horizons. Average pools of CEC were 12 and 0.7 eq m^?2 in meadows and moraine areas, respectively. The base saturation (BS) was 4–45% (12% on average) of CEC, and was primarily based on Ca²⁺ and K⁺ (～40% and ～22% of BS, respectively). C:N molar ratios (14–20) were only slightly lower than those observed in the alpine Tatra Mountain zone ～40 years ago. Concentrations of C, N, and P in soil microbial biomass were high (on average 1.6, 3.4, and 25% of total C, N, and P concentrations), suggesting high microbial activity in alpine soils.     

Soil changes in different age classes of Norway spruce (Picea abies (L.) Karst.) on afforested farmland

The aim of this study was to test the hypothesis that afforestation changes the content and distribution of soil organic carbon, nutrients and pH in the A-horizon of land previously used in agriculture, and that such soil changes depend on stand development. The investigation was evaluated as a completely randomised design with three treatments representing different age classes of trees: 20 years (Y20), 40 years (Y40) and 55 years (Y55). Eighteen trial plots, six per treatment, were established in plantations of Picea abies (L.) Karst. on soils of similar texture and mineralogy. Tree volume was 220 m³ ha^-1 in Y20, 400 in Y40 and 440 m³ ha^-1 in Y55.Concentrations of carbon (C) and nitrogen (N) were significantly higher in the uppermost part of the soil in the older stands Y40 and Y55 than in Y20. The total amount of organic C in the litter layer plus the top 15 cm of the soil differed between age classes, with Y40 and Y55 having the largest amounts. A reference layer (15–20 cm) was used in calculating the amount of soil C that had accumulated in the horizon since afforestation, being about 10 tonnes ha^-1 of C in Y20 and 19 tonnes ha^-1 in Y40 and Y55.Cation exchange capacity (CEC) and base saturation (BS) was higher in the older stands. Carbon contents and CEC were strongly correlated. In Y40 and Y55, pH was significantly lower than in Y20 in the lower part of the soil horizon. There was a general decrease with depth of C, N, CEC, K⁺ and Mg²⁺ in the soil horizon. BS, Ca²⁺, Na⁺ and pH showed a somewhat different pattern of distribution, with deceasing values in the upper part of the soil horizon and increasing values in the lower part of the soil horizon.Abbreviations BD Bulk density - CEC cation exchange capacity - BS base saturation - Ca²⁺ calcium ion - Mg²⁺ magnesium ion - K⁺ potassium ion - Na⁺ sodium ion - C carbon - Ca _a accumulated carbon content - C _t total carbon content - N nitrogen - Y20 age class 20 years - Y40 age class 40 years - Y55 age class 55 years     

Impact of faunal complexity on nutrient supply in field mesocosms from a spruce forest soil

A field study in an acidic spruce forest soil using soil mesocosms was conducted to investigate the effects of mesofauna and macrofauna on exchangeable cations, organic matter content, base saturation, and Ca-lactate extractable nutrients. In the field, intact soil monoliths were taken from the ground, defaunated by deep-freezing and wrapped in nets of various mesh-sizes to control immigration of different faunal size classes. The monoliths were then replanted in the field. Three types of treatments for the mesocosms were prepared: (1) microbiota only, (2) microbiota and mesofauna, (3) microbiota, mesofauna, and macrofauna (=complex fauna). After eight months the mesocosms and unmanipulated control plots (treatment 4) were destructively sampled and submitted to chemical analysis. Generally, the exchangeable base cations and Mn²⁺ showed higher contents with increasing faunal complexity, whereas the exchangeable acidic cations of Fe³⁺ and Al³⁺ decreased in the monoliths with complex fauna. These effects were significant for K⁺, Mg²⁺ and Mn²⁺ in the L/F-layer and for Ca²⁺, Mn²⁺, Al³⁺ and Fe³⁺ in the H-layer. As a possible explanation a rise of ion-binding sites in the course of enhanced humification processes is discussed.In the L/F-layer base cations showed higher concentrations in the monoliths with complex fauna as compared to the control plot, which contained intact roots. This might be due to nutrient uptake by roots in the control plot or enhanced mineralization in the monoliths with complex fauna, where roots had been cut.     

Effects of deforestation and cultivation on soil CEC and contents of exchangeable bases: A case study in Simlipal National Park,India

Deforestation in the tropics seems to be a serious problem probably because of the reduction in soil CEC and the consequent losses of nutrients from the soils. Here, changes in these parameters as influenced by deforestation as well as vegetative cover were studied; statistical methods were applied to interpret the results. Cultivation causes a significant reduction in CEC, total content of the exchangeable bases and exchangeable Ca2+ and Mg2+ levels compared to the adjoining unmanaged forest land. Levels of exchangeable K⁺ and Na⁺, however, do not change significantly. Evergreen forest soils have the highest levels of CEC, total exchangeable bases, exchangeable Ca²⁺ and K⁺. Deciduous forest, grassland and cultivated soils have statistically similar contents of exchangeable Ca²⁺, Mg²⁺, K⁺ and Na⁺. Exchangeable Mg²⁺, however, is not affected by vegetative cover. Soil CEC shows fairly good correlation with the organic carbon content only in evergreen forest soils. In others, organic carbon apparently does not influence CEC significantly. All soils show excellent correlation between their CEC and total exchangeable bases. It is concluded that for regeneration of weathered tropical soils, an evergreen cover provides the most effective means; deciduous vegetation or grass cover do not seem promising.     

Nitrogen deposition contributes to soil acidification in tropical ecosystems

Elevated anthropogenic nitrogen (N) deposition has greatly altered terrestrial ecosystem functioning, threatening ecosystem health via acidification and eutrophication in temperate and boreal forests across the northern hemisphere. However, response of forest soil acidification to N deposition has been less studied in humid tropics compared to other forest types. This study was designed to explore impacts of long‐term N deposition on soil acidification processes in tropical forests. We have established a long‐term N‐deposition experiment in an N‐rich lowland tropical forest of Southern China since 2002 with N addition as NH₄NO₃ of 0, 50, 100 and 150 kg N ha^?1 yr^?1. We measured soil acidification status and element leaching in soil drainage solution after 6‐year N addition. Results showed that our study site has been experiencing serious soil acidification and was quite acid‐sensitive showing high acidification (pH_(H2O)<4.0), negative water‐extracted acid neutralizing capacity (ANC) and low base saturation (BS,< 8%) throughout soil profiles. Long‐term N addition significantly accelerated soil acidification, leading to depleted base cations and decreased BS, and further lowered ANC. However, N addition did not alter exchangeable Al³⁺, but increased cation exchange capacity (CEC). Nitrogen addition‐induced increase in SOC is suggested to contribute to both higher CEC and lower pH. We further found that increased N addition greatly decreased soil solution pH at 20 cm depth, but not at 40 cm. Furthermore, there was no evidence that Al³⁺ was leaching out from the deeper soils. These unique responses in tropical climate likely resulted from: exchangeable H⁺ dominating changes of soil cation pool, an exhausted base cation pool, N‐addition stimulating SOC production, and N saturation. Our results suggest that long‐term N addition can contribute measurably to soil acidification, and that shortage of Ca and Mg should receive more attention than soil exchangeable Al in tropical forests with elevated N deposition in the future.     

The relation between vegetation and soil chemistry gradients in a ground water discharge fen

Abstract. The soil chemistry of a headwater valley fen is influenced by local ground water discharge that supplies base cations and alkalinity to the fen. An irrigation canal just upward of the fen is the source of this alkalinity. The ecological consequences of this artificial system are studied both on the soil and vegetation level. Rich-fen species of the alliance Caricion davallianae are connected to soil water alkalinity and soil base status. They depend directly on the alkaline ground water discharge. In addition, the local input of this water causes a gradient-rich pattern from poor to rich fen, and it is therefore concluded that it is responsible for the presence of intermediate fen vegetation too. High nutrient levels in the irrigation water have not influenced the fen until now. This case study illustrates the possibility for rich fen restoration after acidification. Irrigation with alkaline water is efficient if excess nutrients can be removed.     

祁连山西水林区土壤阳离子交换量及盐基离子的剖面分布

以祁连山西水林区分布的棕钙土、灰褐土、栗钙土和高山草甸土为对象,研究了阳离子交换量和盐基离子(K+、Na+、Ca2+、Mg2+)的剖面分布规律及其与土壤理化因子的关系。结果表明:土壤阳离子交换量(CEC,介于4.80—48.10 cmol/kg)和盐基总量(TEB,介于4.67—21.34 cmol/kg)随剖面深度的增加逐渐减小,不同土壤类型的大小顺序为:灰褐土>高山草甸土>栗钙土>棕钙土;土壤盐基组成以Ca2+、Mg2+为主(占TEB的比例平均为71.6%、22.9%),K+、Na+所占比例较低(占TEB的比例平均为3.3%、2.2%);棕钙土、灰褐土和栗钙土盐基离子的剖面分布由浅至深呈现:K+≈Ca2+>Na+≈Mg2+,高山草甸土盐基离子则呈现:K+>Na+>Mg2+>Ca2+。不同土壤类型间盐基离子的含量及饱和度随发生层次不同存在较大差异。土壤有机质是CEC的主要贡献因素,粉粒对CEC也有显著的促进作用,而砂粒、CaCO3对CEC有显著抑制作用。土壤生物复盐基作用弱于淋溶作用,造成盐基饱和度较大(BSP,介于44.4%—97.2%),并随剖面深度的增加逐渐增大。相关性分析表明,土壤交换性Na+、Mg2+的含量及饱和度均呈极显著正相关,交换性Na+、Mg2+饱和度与CaCO3含量呈极显著正相关;pH值与BSP呈极显著正相关;土壤速效P含量与CEC呈极显著正相关,速效K含量与交换性K+含量呈极显著正相关。     

Combined effects of waterlogging and salinity on electrochemistry, water-soluble cations and water dispersible clay in soils with various salinity levels

The combination effects of waterlogging and salinity on redox potential (Eh), pH, electric conductivity (EC), water-soluble cations (NH₄ ⁺, K⁺, Na⁺, Ca²⁺, Mg²⁺, Fe²⁺, and Mn²⁺) and water-dispersible clay (WDC) were studied in six soils collected near salt lakes in western Australia. The soils with various salinity levels were incubated under a waterlogged condition at 30 °C for 12 weeks. The Eh, pH, EC, and cations of soil solutions were monitored over the waterlogged period. The Eh values generally dropped to the lowest point within 12 days of waterlogging, then increased slightly, and reached equilibrium after 4 weeks of waterlogging. Increasing salinity levels increased soil Eh. While waterlogging increased soil pH in the first 3–4 weeks, increasing salinity level decreased soil pH during the entire waterlogging period. Waterlogging increased the EC values in the first 2 weeks, partly due to dissolution of insoluble salts. The concentrations of water-soluble NH₄ ⁺ were significantly increased with salinity level and waterlogging, and reached maximum values at week 2, and then declined to the initial level. Waterlogging and salinity increased the concentrations of water-soluble K⁺, Ca²⁺, Mg²⁺, Fe²⁺, and Mn²⁺ ions, but the magnitudes of changes were greatly affected by soil properties. Increases in water-soluble K⁺, Ca²⁺ and Mg²⁺ were attributed to increased solubility of insoluble salts, and increased competition for the adsorption sites of the soil exchange complex due to elevated concentrations of Na⁺, Fe²⁺ and Mn²⁺. Increases in water-soluble Fe²⁺ and Mn²⁺ induced by waterlogging were attributed to the dissolution of Fe and Mn oxides under reduced conditions. Waterlogging increased, but salinity decreased, the amounts of water-dispersible clay in the soils of low EC value. The higher salinity level can counteract the adverse effect of waterlogging on clay flocculation.     

Redox conditions and iron chemistry in highland swamps of Burundi

Iron toxicity is a major soil constraint to rice (Oryza sative L.) cropping in highland swamps of Burundi. These swamps have a wide range of carbon content. This study aims at determining the influence of carbon content and redox conditions on the release of iron from Fe-bearing minerals. The pe-pH pairs distribution and oxalate dissolution data strongly suggest a control of Fe²⁺ activity by a pool of poorly crystallized ferric oxides. Flooding results in high values of KCl-extractable Fe (up to 22 cmolc kg^-1) being released from that pool. The iron release is positively correlated with organic matter. On the other hand, highly organic, peaty soils have large CEC and their adsorbed Fe fraction remains relatively low. As the exchangeable Fe fraction has previously been correlated with Fe toxicity to rice, we may conclude that very organic (> 25% C), peaty soils exhibit a lower Fe toxicity hazard than soils with intermediate carbon content (10–25%).     

Requirement of divalent cations for photoactivation of the laten water-oxidation system in intact chloroplasts from flashed leaves

The effects of divalent cations on photoactivation of the latent water-oxidation system in intact chloroplasts isolated from wheat (Triticum aestivum L.) leaves grown under intermittent flash illumination were investigated by using A23187, an ionophore for divalent cations, and the following results were obtained. (a) Photoactivation in the intact chloroplasts was inhibited by A23187, but was restored on addition of a low concentration of Mn²⁺ (10 μM). (b) A high concentration of Mn²⁺ (70 μM) was inhibitory, in contrast, for photoactivation, but the inhibition was restored by the coexistence of a suitable concentration of Ca²⁺ (5 mM). (c) The Ca²⁺-dependent restoration was inhibited by a high concentration of Mg²⁺ or Sr²⁺, but the inhibition was restored by the coexistence of Ca²⁺. (d) Kinetic analyses of these competitive effects between divalent cations revealed that: (i) High concentration of Ca²⁺ inhibits photoactivation in competition with Mn²⁺. (ii) High concentration of Mn²⁺ inhibits photoactivation in competition with Ca²⁺. (iii) High concentration of Mg²⁺ affects photoactivation by inhibiting Ca²⁺-dependent restoration in competition with Ca²⁺. Based on these results, we propose that the latent water-oxidation center has two binding sites, each specific for Mn²⁺ and Ca²⁺, and that photoactivation takes place in the center having both Mn²⁺ and Ca²⁺ on their respective binding sites.     

Use of Soil Amendments to Reduce Nitrogen,Phosphorus and Heavy Metal Availability

The primary objectives of this study were to determine (1) the exchange characteristics of various soil amendments using a range of salt solutions, (2) the effect of selected soil amendments on heavy metal (Cu²⁺, Pb²⁺, and Zn²⁺) availability, and (3) the effect of selected soil amendments on NH₄ ⁺ and P availability. The CEC of zeolite and red mud obtained using solutions of 0.1?M BaCl₂ and 0.1?M BaCl₂/NH₄Cl were significantly lower than values obtained using 1?M KCl and 1?M NH₄Cl. The higher CEC obtained with monovalent cations indicated that larger divalent cations could not enter the mineralogical framework of zeolite and red mud, and, consequently, a number of exchange sites were only accessible to the smaller monovalent cations. These findings suggest that 1?M KCl and 1?M NH4NO3 should be used as the extracting solutions to obtain the best estimation of CEC and ECEC of red mud and zeolite. The ability of red mud, zeolite, and calcium phosphate (Ca-P), mixed at rates of 0%, 5%, 10%, and 20% (w/w), to sorb Cu²⁺, Pb²⁺, and Zn²⁺ generally followed the order: red mud>zeolite>>Ca-P, while the affinity sequence for these metals followed the order: Pb²⁺≥Cu²⁺>>Zn²⁺. The higher affinity of the sand/amendment mixtures for Pb²⁺ and Cu²⁺ relative to Zn²⁺ was attributed to metal hydrolysis and subsequent specific adsorption as Pb(OH)⁺ and Cu(OH)⁺. Zinc was considered to have been primarily sorbed as the divalent cation species. Rates of 5% (w/w) adequately reduced the availability of heavy metals to concentrations below environmental guidelines based on the Toxicity Characteristic Leaching Procedure. Red mud and zeolite added at a rate of 10% (w/w) to the A and B horizon of a sandy soil significantly increased their ability to remove NH₄ ⁺ from solution, but had negligible effect on P sorption compared with unamended soils. Increased NH₄ ⁺ removal was attributed to the associated increase in CEC and the greater selectivity of the exchange sites for this cation relative to resident exchangeable Ca²⁺ and Na⁺. The absence of P sorption by these two amendments was attributed to the high pH and predominantly negative surface charge of the red mud and the lack of sorption sites in zeolite. Gypsum, on the other hand, tended to depress NH₄ ⁺ retention but markedly increased P sorption. The depressive effect on NH₄ ⁺ was due to increased competition between NH₄ ⁺ and Ca₂ ⁺ for a limited number of exchange sites, while formation of calcium phosphates of low solubility was the possible mechanism for increased P sorption.     

Calcium-mediated stabilisation of soil organic carbon

Soils play an essential role in the global cycling of carbon and understanding the stabilisation mechanisms behind the preservation of soil organic carbon (SOC) pools is of globally recognised significance. Until recently, research into SOC stabilisation has predominantly focused on acidic soil environments and the interactions between SOC and aluminium (Al) or iron (Fe). The interactions between SOC and calcium (Ca) have typically received less attention, with fewer studies conducted in alkaline soils. Although it has widely been established that exchangeable Ca (Ca_Exch) positively correlates with SOC concentration and its resistance to oxidation, the exact mechanisms behind this relationship remain largely unidentified. This synthesis paper critically assesses available evidence on the potential role of Ca in the stabilisation of SOC and identifies research topics that warrant further investigation. Contrary to the common view of the chemistry of base cations in soils, chemical modelling indicates that Ca²⁺ can readily exchange its hydration shell and create inner sphere complexes with organic functional groups. This review therefore argues that both inner- and outer-sphere bridging by Ca²⁺ can play an active role in the stabilisation of SOC. Calcium carbonate (CaCO₃) can influence occluded SOC stability through its role in the stabilisation of aggregates; however, it could also play an unaccounted role in the direct sorption and inclusion of SOC. Finally, this review highlights the importance of pH as a potential predictor of SOC stabilisation mechanisms mediated by Al- or Fe- to Ca, and their respective effects on SOC dynamics.     

Cations stimulate proton pumping in Catharanthus roseus cells: implication of a redox system?

Abstract During growth, cultured Catharanthus oseus cells produce a transient acidification of the culture medium that may be controlled by cations. The removal of divalent ions from the medium by the chelator EGTA resulted in an inhibition of this acidification. Conversely, acidification can be stimulated by the addition of Ca²⁺, Mg²⁺ and La³⁺ in the basal medium. This acidification process and the proton-linked redox pump previously described (Marigo & Belkoura, 1985) respond in a similar manner to cations. These two systems, which are both inhibited by the Ca²⁺ -calmodulin antagonist calmidazolium, could be regulated by the Ca²⁺-calmodulin complex. By using ionic surfactant (CP⁺, SDS^?) it was demonstrated that the net surface charge of the plasmalemma plays a role in the activation of the two pumping processes. These results are interpreted to indicate that a transmembrane redox system could provide the energy for electrogenic proton extrusion.     

杭州湾滨海滩涂盐基阳离子对植物分布及多样性的影响

滨海滩涂由于其高含盐量显著影响了植物群落分布及生物多样性。目前有关滩涂含盐量与生物多样性的关系研究较多,但不同区域盐基离子组成不同,且对植物的影响也存在较大差异,以杭州湾南岸不同年代形成的滩涂为研究对象,系统监测了50个样方土壤交换性盐基阳离子的组成、分布和植物组成及多样性特征等,采用去趋势典范对应分析(DCCA)、线性回归和多元逐步回归分析了4种盐基阳离子对物种数量、分布和多样性的影响。结果表明,杭州湾南岸滩涂4种主要盐基阳离子含量(g/kg)大小顺序为Ca²⁺>Na⁺>Mg²⁺>K⁺,其中Ca²⁺占到总含量的61.97%;经DCCA分析发现4种盐基阳离子对植物群落的分布均有显著影响,但以Ca²⁺的影响程度最大;随着盐基离子含量的逐渐降低,物种数量逐渐增加,多样性指数逐渐增加,同时也发现Ca²⁺对两种多样性指数影响最大。     

Determination of cation exchange capacity of ryegrass roots by summing exchangeable cations

Cations were desorbed from root exchange sites of ryegrass (Lolium multiflorum Lam. cvs. Gulf, Marshall, Urbana, and Wilo) using BaCl₂, BaCl₂-triethanolamine, NH₄OAc, and KCl. Results were analysed using multivariate analysis of variance. Ba²⁺-containing desorbents displaced more Ca²⁺ while monovalent desorbents displaced more exchangeable monovalent cations. The sum of adsorbed cations was significantly correlated with root exchange capacity (CEC) as determined by the H⁺ titration procedure, although slightly larger values were obtained with all desorbents. Lower CEC values were obtained for ryegrass cultivars less sensitive to Al.     

Impact of chemical composition of legume residues and initial soil pH on pH change of a soil after residue incorporation

Reports on the effect of organic matter addition on soil pH have been contradictory. This study examined the effect of applying legume residues differing in concentrations of N (4.3-45.5 mg g^-1) and excess cations/organic anions (0.22–1.56 mmol g^-1) on pH change of five soils differing in initial pH (3.60–5.58 in 0.01 M CaCl₂) under sterile and non-sterile conditions. Addition of the legume residues at a level of 1% soil weight increased the pH of all soils by up to 2 units after incubation for 35 and 100 d under non-sterile conditions. Exceptions were the Lancelin (initial pH 5.06) and Kellerberin (pH 5.58) soils with addition of clover roots (excess cations 22 cmol/kg) for 100 d where soil pH decreased by 0.13–0.15 units as compared to the control. The amounts of alkalinity produced in soil correlated positively with concentrations of excess cations and total nitrogen of the added legume residues, and negatively with the initial pH of the soil. When soil was fumigated with chloroform during incubation, similar trends of soil pH changes and alkalinity production, due to legume residues addition, were displayed but the effects of the residue on alkalinity production in the Wodjil and Lancelin soils were much less than under non-sterile conditions. Direct shaking of soil with the residues under sterile conditions increased the amount of alkalinity in the soils with initial pH of 3.60–4.54, but not in the soils with initial pH of 5.06 and 5.58. The maximal alkalinity production was less than one third of that produced in the soil after 100 d of incubation under non-sterile conditions. The results suggest that the direction and the magnitude of pH change depend largely on the concentration of organic anions in the residues, initial soil pH and the degree of residue decomposition. The incorporation of crop residues, especially those with high concentrations of excess cations, is recommended in minimizing soil acidification in farming systems. This revised version was published online in June 2006 with corrections to the Cover Date.