干旱胁迫对水稻叶表面蜡质积累的影响

环境胁迫一直以来是影响植物生长和农作物产量的主要因素,而覆盖植物叶片表层的蜡质层在植物生长发育和适应外界环境方面起着关键作用。本试验以中花11、广盐2号和Z46这3个水稻品种进行干旱胁迫处理,通过扫描电镜观察叶片表面蜡质覆盖密度,以及测定叶片相对含水量、叶绿素浸提率以及失水率等生理指标,从而综合分析干旱胁迫对不同水稻品种叶片表面蜡质积累的影响。结果表明：干旱胁迫条件下,3个试验的水稻品种叶片相对含水量降低,叶表面蜡质覆盖量增加,叶绿素浸提率以及离体叶片失水率下降。     

Norway Spruce: A Novel Method using Surface Characteristics and Heavy Metal Concentrations of Needles for a Large-Scale Monitoring Survey in Austria

Epistomatal wax structure, occurrence of dust, gypsum-crystallites and microorganisms on the needle surfaces and trace metal contents of current-year Norway spruce needles from various Austrian sites with different pollution levels and sources were analyzed. The epistomatal wax structure was assessed with a recently developed quantification method. Generally, sites in the vicinity of various emissions sources (e.g steel works, chemical industry, magnesite/cement works, highways, conurbations) showed significantly stronger degraded wax structures than sites remote from sources. However, between the individual categories of emitters hardly any difference in the degree of the observed wax degradation could be stated. Various pollutants or emission types seem to cause epistomatal wax degradations. For these findings the following methodological prerequisites which were derived from results of the present monitoring survey were taken into account: the epistomatal wax structures of identical trees were found being significantly different between sampling years. The reasons in behind need further clarification. Therefore only data from the same sampling year should be used for site comparisons in relation to pollution status. The occurrence of mechanical abrasions of surface waxes (which may be caused by the steadily rubbing of needles through heavy wind events) was identified as a further excluding factor for site comparisons. Dust particles and gypsum-crystallites were only detected on needles from sites located in the vicinity of emission sources, whereas the occurrence of microorganisms on the needle surfaces was not related to the vicinity of pollution sources. Several heavy metals were found in elevated concentrations in needles close to respective sources (steel works: Fe, Mn, Zn, Pb, Hg; metallurgical works: Fe, Mn, Ni, Mo, Cr, V; highways: Zn, Cu, Pb). Some of these metals (Fe, Mn, Zn, Cu, Cr, V) were also detected in the dust adhering to the needle surface. These results and the relation of higher contents to the denser covering of the needles with dust suggest that recently deposited adhering dust particles are responsible for the higher elemental contents measured in the needles. In contrast to these needle surface parameters, the epistomatal wax quality did not show any relation to the concentration of the investigated heavy metals.     

Impacts of (NH4)2SO4 Deposition on Norway Spruce (Picea Abies [L.] Karst) Roots

The effects of enhanced (NH₄)₂SO₄ (NS) deposition on Norway spruce (Picea abies [L.] Karst) fine root biomass, vitality and chemistry were investigated using root-free in-growth cores reproducing native organic and mineral soil horizons. The cores were covered and watered every 2 weeks with native throughfall or throughfall supplemented with NS to increase deposition by 75 kg ha^-1 a^-1 NH₄ ⁺-N (86 kg ha^-1 a^-1 SO₄2--S). The in-growth cores were sampled after 19 months and assessed for root biomass, necromass, length, tip number, tip vitality and fine root chemistry. Root biomass and fine root aluminium (Al) concentration were negatively correlated, but NS deposition had no effect on root growth or root tip vitality. NS deposition caused increased fine root nitrogen (N) concentrations in the organic horizon and increased Calcium (Ca) concentrations in the mineral horizon. Fine root biomass was higher in the organic horizon, where fine root Al and potassium (K) concentrations were lower and Ca concentrations higher than in the mineral horizon. Results highlighted the importance of soil stratification on fine root growth and chemical composition.     

Foliar Nitrogen as an Indicator of Nitrogen Deposition and Critical Loads Exceedance on a European Scale

The foliar N content of bryophytes and Calluna vulgaris (L.) has been shown to be an indicator of atmospheric N deposition in the UK at a regional scale (1000km) and more recently on a smaller scale in the vicinity of intensive livestock farms. This work extends the geographical scale of the relationship between foliar N concentration of Calluna vulgaris and other ericaceous shrubs and N deposition with 2 measurement transects, one extending from northern Finland to southern Norway (2000 km) and the other extending from central Sweden to Stockholm, south east Sweden (330 km). Included in the second transect is a region of complex terrain in the Transtrand uplands, where the variation in N deposition with altitude and canopy cover was quantified using ²¹⁰Pb inventories in organic soil. The relationship between foliar N (F_N) and N deposition was shown to increase linearly with N deposition (N_D) over the range 0.8% N to 1.4% N according to F_N = 0.040N_D + 0.793 (r² = 0.70). The data are entirely consistent with earlier studies which together provide a valuable indicator of critical loads exceedance, the threshold value being approximately 1.5% N, which is equivalent to a N deposition of 20 kg N ha^?1 y^?1.     

Nutrient Fluxes in Planted Norway Spruce Stands of Different Age in Southern Poland

The fluxes of N–NO ₃ ^? , N–NH ₄ ⁺ , S–SO ₄ ^2? , Na⁺, K⁺, Ca²⁺ and Mg²⁺ from bulk precipitation to throughfall, stemflow and soil water surface flows were studied during 1999–2003 in planted Norway spruce forest stands of different ages (11, 24, 91 and 116 years in 1999). Also, runoff from the corresponding Potok Dupniański Catchment in the Silesian Beskid Mts was studied. N deposition was above the critical load for coniferous trees. The interception increased with stand age as well as leaf area index and so did the leaching from the canopy of almost all the analysed elements, but especially S–SO ₄ ^2? , H⁺ and K⁺. The nutrient fluxes varied with age of the spruce stands. Throughfall showed a high amount of S and of the strong acids (S–SO ₄ ^2? and N–NO ₃ ^? ) deposited to the soil, especially in older spruce age classes. Decomposition of organic matter caused a rise in water acidity and an increase in the concentrations of all the analysed ions; the leaching of minerals, however, was low (under 1%). The horizontal soil water flow showed an increase in the amount of water and amount of ions and contributed to a further decrease of pH at the soil depth of 20 cm. Element concentrations and their amounts increased with water penetrating vertically and horizontally on the slopes. Considerable amounts of ions, especially S and alkaline cations, were carried beyond the reach of the root system and then left the catchment. In the long term, these mineral losses will adversely affect health and growth of the spruce stands, and the increased acidity with stand age will presumably have negative effects on the runoff water ecosystem.     

Ecogeochemical Investigation: Stream Water Quality as an Indicator of Pollution in the Border Areas of Finland, Norway and Russia

The Geological Surveys of Finland and Norway, and the Central Kola Expedition, Russia, carried out an environmental geochemical mapping project, including investigation of stream water quality. The project was carried out in 1992–1993 in the border areas of Finland, Norway and Russia, covering an area of 12 000 km², to determine the impacts of smelting industries at Nikel and Zapoljarnij. Stream water was one of eight different indicators providing an estimation of the degree and distribution of contamination in the study area. Contamination of surface water was assessed by analyses of 44 samples, 41 variables were measured on each sample. Indicators of human activities in surface waters are NO₃, K, electrical conductivity (EC), SO₄, Na, Cl and acidification indicated by alkalinity and pH. On the coast Na and Cl contents are also affected by marine salts. The results show considerably higher contents of K, Ca, Mg, SO₄, Na, heavy metals and EC in the samples close to Nikel and Zapoljarnij smelters than those sites more distant from the polluting sources. Especially chemical effects of high emissions of Ni, Cu and SO₂ on stream water quality from Nikel and Zapoljarnij smelters are clearly seen near the sources of emissions.     

Exploring Interactions between Pollutant Emissions and Climatic Variability in Growth of Red Spruce in the Great Smoky Mountains National Park

Concern exists as to the status of red spruce (Picea rubens Sarg.) in the Great Smoky Mountains, with evidence both for and against an unprecedented decline in radial growth during the past century. On the basis of a dendrological record from 1850 to 1998, our analyses support a decline in radial growth starting as early as the 1940s through to the 1970s; in the 1970s there was a reversal of this decline. In comparing trees near ridges (2000 m) with those in draws (1500 m), we found differences in the (a) timing of the decline, (b) rate of decline, and (c) homogeneity of the decline, with trees near ridges showing earlier, faster, and more homogeneous declines than trees in draws. We hypothesized that changes in climatic conditions and/or atmospheric pollutants, both of which changed beyond ranges of natural variability, were related to the observed decline in radial growth. In trees near ridges, up to 67.1% of changes in radial growth could be explained by a combination of climatic conditions (7.6%) and annual emissions of nitric oxides (NO_x) and sulfur dioxide (SO₂) (an additional 59.5%). In trees from draws, up to 38.3% of the changes in radial growth could be explained by climatic conditions only. A conceptual model is presented, where trees in naturally acidic soils with low base saturation provide a sensitive signal for the changing nature of acidic pollutants, but trees in anthropogenically acidifying soils with an initially higher baser saturation provide a signal that is confounded by a transient increase of calcium (Ca) and magnesium (Mg) in the soil that results in a transient increase in radial growth.     

Dissolved Organic Nitrogen Concentrations and Ratios of Dissolved Organic Carbon to Dissolved Organic Nitrogen in Throughfall and Soil Waters in Norway Spruce and Scots Pine Forest Stands Throughout Norway

Dissolved organic nitrogen (DON) plays an important ecological role in forest ecosystems, and its concentration is related to that of dissolved organic carbon (DOC). We investigated DON concentrations and ratios of DOC to DON in throughfall and soil waters in 16 Norway spruce and two Scots pine forest stands sampled at weekly intervals between 1996 and 2006. The stands are all included in the ICP Forests Level II monitoring program and are located throughout Norway. DON concentrations were significantly and positively related to DOC concentrations in throughfall (r ²?=?0.72, p?<?0.0001) and soil water at 5, 15, and 40 cm (r ²?=?0.86, 0.32, and 0.84 and p?<?0.0001, 0.04, and <0.0001, respectively). At most sites, the annual median DOC/DON ratio in throughfall ranged from 20.3 to 55.5, which is lower than values in soil water, which ranged from 24.5 to 81.3, gradually decreasing with soil depth. DON concentrations varied seasonally in throughfall at many plots and in soil water at 5-cm depth at one plot only, with higher values in the growing season, but there was no noticeable seasonality at greater depth. The ratios of DOC/DON in soil water were significantly positively related to the C/N ratio in soil at the same depth. Above-ground litter input was the main factor having a significant, negative relationship to DOC/DON in soil water at all depths studied. This might reflect the effect of site conditions on both DOC/DON ratios and litter quantity.     

Changes in Anthocyanin Content as Indicator of Maize Sensitivity to Selenium

The aim of this experiment was to examine the effect of exogenous selenium (Se) on anthocyanin and chlorophyll accumulation, Se content, as well as the growth of maize (Zea mays var. ‘saccharata Kcke’) cv. ‘Zlota Karlowa’ seedlings. Plants were grown hydroponically in Hoagland's nutrient solution at different pH values: 4.5, 6.2, and 7.5. Selenium was added to the solution as either selenate (Na₂SeO₄) or selenomethionine (C₅H₁₁NO₂Se) to a final concentration of: 0 (control), 5, 25, 50, and 100 μ M Se. Generally, the presence of Se in the medium caused an increase in the anthocyanin content and a simultaneous decrease of the total chlorophyll concentration depending on the Se form and dosage. Higher concentrations of anthocyanin were detected in the presence of selenomethionine than selenate, notably at pH 4.5. The effect of individual Se forms on maize seedlings, expressed on the basis of the fresh weight, indicate that selenomethionine was more phytotoxic than selenate. Selenium content both in roots and shoots increased linearly with increasing Se concentration in solution culture. However, a much higher Se level was found in the maize organs when plants were supplied with selenomethionine than selenate. Experimental evidence shows that the changes in anthocyanin content can be used as a test parameter reflecting the degree of Se toxicity in maize plants, and may be potential useful for bioindication of Se phytotoxicity in other higher plants.     

土壤微生物量作为土壤肥力指标的探讨

对不同利用方式19个黑土样品的微生物量和养分进行了分析,结果表明林地的微生物量明显高于玉米地和大豆地,但玉米地和大豆地之间未表现出显著差异,土壤微生物量和土壤养分含量大体上都呈现出林地>大豆地>玉米地的一致的趋势;同时土壤微生物量与土壤有机质、全氮、全磷、速效钾和碱解氮呈现出显著或极显著正相关关系,分析结果还表明土壤微生物量碳作为评价土壤肥力指标比土壤微生物量氮更为灵敏。因此,土壤微生物量可以作为评价不同利用方式的黑土肥力水平的一个生物指标。     

Short-Term Influence of Clinker Dust and Wood Ash on Macronutrients and Growth in Norway Spruce (Picea abies) and Scots Pine (Pinus sylvestris) Seedlings

The effects of clinker dust and wood ash on Norway spruce and Scots pine seedlings were compared in buried pots. Clinker dust (0.5 kg m^?2) and wood ash (0.5 kg m^?2) were applied to the surface of a nutrient-poor mineral soil. In the second year, the increase in soil pH by the dust and ash were larger than in the first year. Both alkaline treatments caused a large increase in the needle potassium (K) concentration. An excess of soil K relative to magnesium (Mg) was observed by decreased Mg concentration in needles shortly after treatment. However, Mg concentration in needles stayed in the sufficiency range. Current results confirmed earlier findings that despite a positive effect on base cation nutrition, wood ash has a low potential for increasing the biomass of forest stands on mineral soils due to the N limitation in these soils.     

Uptake, Deposition and Wash Off of Fluoride and Aluminium in Plant Foliage in the Vicinity of an Aluminium Smelter in Norway

Uptake, deposition and wash off of fluoride and aluminium in/on plant foliage were studied in two experiments near an Al smelter by growing different plant species under cover with free wind-flow underneath, and in the open, and by washing the leaves. With an average ambient air concentration of 2.2 μg F m³, the F and Al contents in leaves varied between species from 138 to 665 mg F kg^?1 and from 150 to 1025 mg Al kg^?1when grown under cover. An average of about 60% of the F and nearly 70% of the Al could be washed off covered plants. Uncovered plants had 33–51% lower F content, indicating a considerable precipitation wash off. Precipitation wash off varied with species, probably due to different leaf surface properties. The strong effect of precipitation on plant foliage F has to be taken into consideration when comparing differences in F content between years, localities and species. On average about 40–50% of the F and 55% of the Al could be washed off the leaves of uncovered plants. Washed leaves of plants exposed to precipitation had about 20% lower F content, compared to washed leaves of covered plants, thus indicating leaching of F from leaves exposed to rain. In contrast to fluoride, the Al contents in washed leaves of uncovered plants were about 50–80% higher than in covered washed leaves, thus indicating a significant uptake of Al solved in rainwater through the leaf cuticle.     

Soil Water Chemistry as an Indicator of the Reproducibility of Artificially Contaminated Soil Mesocosms

The simulation of ecosystems by mesocosms might be affected by artefacts due to the scale reduction implied in such experiments. The physico-chemical properties of water leaching out of mesocosms made of only 50 kg of agricultural soil were measured to demonstrate that they constitute reproducible systems. The soils were artificially contaminated with lead, atrazine, benzo(a)pyrene and Phenochlor. Physico-chemical parameters (redox potential, conductivity, pH, dissolved oxygen) and major ions were monitored in the leachates for six months. Even though these changed with time, in each sampling campaign they were similar for all of the mesocosms despite possible independent development of microbial and biological activity.     

Relative Neutralizing Value as an Indicator of Actual Liming Ability of Limestone and Byproduct Materials

Methods used to compare the effectiveness of liming materials (e.g., relative neutralizing value, RNV; effective calcium carbonate equivalent, ECCE) were developed for ground limestone. This method is relatively untested on industrial byproducts that could be used when limestone is expensive or unavailable. The objective was to determine if RNV applies to both ground limestones and industrial byproducts. A 42-d incubation study was performed on three acid soils with 11 ground limestones and 9 different byproducts at four rates based on titration and the modified Adams-Evans buffer method. Overall effectiveness, assessed as RNV compared to Ca(OH)₂, averaged 101.5 ± 0.9% for all the evaluated liming materials, except the paper sludge and dolomitic marble. Thus, RNV was a good estimate of neutralizing ability when particle size was accurate. Addition of RNV to packaging would facilitate the commercial use of byproducts as liming materials allowing consumers to compare products by price and properties.     

Precipitation Chemistry as an Indicator of Urban Air Quality in Mersin, North-Eastern Mediterranean Region

The chemical composition of precipitation in the city of Mersin on the Mediterranean coast of Turkey has been studied. Spatial and temporal variability of rainwater constituents have been determined from samples collected at two central and two suburban stations for the December 2003–May 2005 period. A total of 246 samples covering all precipitation events were analyzed to determine pH, conductivity, as well as major anion (Cl^?, ${\text{NO}}_3^ - $ , ${\text{SO}}_4^{2 - } $ ); major cation (H⁺, Na⁺, K⁺, Ca²⁺, Mg²⁺, ${\text{NH}}_4^ + $ ) and formaldehyde (HCHO) concentrations. The pH varied within a range of 4.8–8.5, with only 8 out of 246 samples being acidic (pH?<?5.6), and the remaining highly alkaline samples being neutralized by either ${\text{NH}}_4^ + $ in rainwater, or by CaCO₃ resulting from wet deposition of atmospheric dust. The volume weighted mean ΣAnion/ΣCation ratio was 0.49. The equivalent concentration of major ionic species followed the order: ${\text{Ca}}^{2 + } > {\text{HCO}}_3^ - > {\text{SO}}_4^{2 - } > {\text{Cl}}^ - > {\text{NH}}_4^ + > {\text{Na}}^ + > {\text{Mg}}^{2 + } > {\text{NO}}_3^ - > {\text{K}}^ + > {\text{H}}^ + $ . Formaldehyde concentrations varied in the range of 0.01–17.9 μM, and was found to be dependent on precipitation volume. Relatively higher ${\text{NH}}_4^ + $ , ${\text{SO}}_4^{2 - } $ , ${\text{NO}}_3^ - $ and HCHO concentrations, mainly of anthropogenic origin, measured near the city center suggest increased pollution from local anthropogenic sources, e.g., residential heating, industrial and/or traffic emissions. In general, the results of this study suggest local precipitation chemistry is more strongly influenced by natural (mineral dust and marine) sources compared to anthropogenic ones.     

Natural Abundance of Foliar 15N as an Early Indicator of Nitrogen Deficiency in Fertilized Cotton

Information on the contribution of various soil nitrogen (N) sources to plant N uptake is often needed for the implementation of sustainable or site-specific management practices in agriculture. Considering the limitations of traditional methods in meeting these needs, this study investigated the potential of leaf δ¹⁵N as an early indicator of nutrient deficiency in cotton. The spatial and temporal natural abundance of ¹⁵N was measured in the soil and leaves of a fertilized cotton field located near the village of Moschochori (Larissa, Greece). The isotopic signal of the leaves was interpreted in the context of the relative contribution of fertilizer to cotton N uptake,as has been demonstrated in the past for other agricultural crops such as wheat (Triticum aestivam L.) and corn (Zea mays). Spatial variability of leaf δ¹⁵N was high early in the growing season (June), reflecting differences in fertilizer N availability and uptake between the east and west side of the field, as well as differences resulting from soil denitrification in depressions. The west side of the field appears to have lost significant amounts of fertilizer N, due to leaching during the rainy period in May, that accumulated in depressions near the waterway. In the subsequent months, the isotopic signal of the leaves was consistently high and indicated reduced fertilizer N uptake on the west side that resulted in deficiencies of N as well as of phosphorus (P) and potassium (K). The significant correlations of mid-square leaf δ¹⁵N with late-season nutrient content and soil elelctrical conductivity(EC) provided evidence that the natural abundance of ¹⁵N was a sensitive indicator of soil and plant nutrient status in this fertilized cotton field.     

Phenolic Pattern of Bean (Phaseolus vulgaris L.) as an Indicator of Chronic Ozone Stress

From sowing till emergence of the fourth trifoliolate leaf, beans were exposed for seven hr a day to four ozone concentrations in open-top chambers: filtered air (FA), non-filtered air (NF), non-filtered air plus 30 ppb ozone (NF+) and non-filtered air plus 60 ppb ozone (NF++). Controls in ambient air of open plots (AA) were also available. The free polyphenolic pool of the first trifoliolate leaf was systematically investigated using HPLC. The groups of phenolics to which the three main chromatographic signals belonged were identified as hydroxycinnamic acid derivative for peak No 1 and flavonoids for peaks Nos 4 and 6. The metabolic regulation of phenolic accumulation could be recognized as different clusters based on specific phenolic patterns that reflected some of the tested atmospheric conditions. The comparison of AA and NF conditions revealed a ‘chamber effect’. FA and NF atmospheres gave rise to almost the same phenolic equilibriums dominated by a hydroxycinnamic acid derivative (about 53% of the total phenolics). Ozone addition was associated with a regular reduction of the percentage of peak No 1: about 40% for NF+ and 19% for NF++. Therefore, the significant decrease of the vacuolar storage of this phenolic compound (from 23 mg g^-1 dry weight for NF to about 3 mg g^-1 dry weight for NF++) can be regarded as a useful tool for monitoring long-term exposure to elevated ozone concentrations.     

Use of Fura 2 Fluorescent Dyes as Indicator for Studying Calcium Distribution in Several Plant Tissues

Calcium (Ca) is an essential plant nutrient and is important in determining quality of fruits in storage. The analytical method presently known to determine Ca concentration in vegetables measures total Ca, and there is a need to develop methods that can determine the distribution of Ca within vegetable tissues. The objective of this study was to determine the ability of fluorescent probes to visualize Ca location and distribution in vegetable tissues. We examined three protocols using fluorescent dyes developed to detect Ca. The first tested Fura 2 acetoximetil (AM) probe in fresh cuts from grapes at different combinations of temperatures and incubation times. The second protocol was developed with the aim of lowering the natural autofluorescense. In the third protocol, the Fura 2 probe was used in tissues previously fixed in formalin, acetic acid, and alcohol solution (FAA). Tissues were observed under an epifluorescence microscope and, to compare and complement the observations, under a scanning electron microscope (SEM). No sign of fluorescence was observed in fixed and fresh tissue using the Fura 2 AM. In fresh cuts, there was autofluorescent interference, provoked mainly by chlorophyll, but also from the vascular system and tannins. The Fura 2 probe was introduced to vegetable tissues by utilizing a pH of 4.5, and a more intense signal was observed in tissues with greater Ca concentration. This signal was also associated with Ca crystals, which might have had some degree of hydrolysis at low pH. Under a SEM microscope, Ca oxalate crystals were clearly observed in those tissues. Our results show that Fura 2 probe can be used to detect Ca and its distribution in vegetable tissues.     

Injury Symptoms and Releasing Rates of Inorganic Ions from Pine Needles as Indicators of Atmospheric Pollution in the Canary Islands Forests

Pinus canariensis Chr, Sm. ex DC. samples showing severe damage produced by atmospheric pollution were taken from three locations under the possible influence of the emissions of a fuel-fired power plant in Tenerife. Other samples were taken at four control locations in Tenerife, La Palma and El Hierro (Canary Islands, Spain), distant from local sources of pollution. Injury symptoms were evaluated by visual examination of the needles, and the data were correlated with the releasing rates of inorganic anions and cations from the needles when sonicated under water. For this purpose, the samples were sonicated 4-times during 10 min successive periods while renewing the water layer in between, and the leachates were analyzed by capillary zone electrophoresis. Measurable amounts of K⁺, Na⁺, Ca²⁺, Mg²⁺, Cl^- and SO₄ ^2- were detected. Potassium ions were released in approximately constant or increasing amounts along the sonication series in the control samples, whereas the samples damaged by pollution released larger amounts during the first sonication treatment, and much lower amounts afterwards. Indices which estimated the initial releasing rate of the cations were examinated as possible indicators to evaluate atmospheric pollution. Only the K⁺ index showed a large positive correlation with the brown-reddish decoloration and tip necrosis of the needles. The correlation of the K⁺ index with flecking and steepling of the needles was much lower. After principal component analysis of the autoscaled data, the sampling sites and the variables were projected on the plane of the first and second eigenvectors. Using the visual examination parameters as variables, both without and with addition of the cation indices, the sampling sites appeared in the order of increasing damage along the first eigenvector. Evidence of the effects of long-range transported pollutants was obtained, and no relationship was demonstrated between damage of pine needles and emissions from the power plant.     

The Importance of Sr Isotopic Compositions as an Indicator of Acid-Soluble Minerals in Arid Soils in China

Aeolian particles originating from arid areas in China, termed Kosa, are considered to be a major source of non-sea-salt Ca, a dominant base cation, in acid precipitation in northeastern Asia. We extracted evaporite minerals (halite, gypsum, and carbonate) from the surface soil collected at eight desert and loess areas in northern China with water and acetic acid. Most ⁸⁷Sr/⁸⁶Sr ratios of the extracted fractions fell in a restricted range (0.7115 ± 0.0015) and differed from those of bulk soils and acid-insoluble minerals (0.712–0.717). The selective dissolution of the soil carbonates in the atmosphere is consistent with two facts: (1) their ⁸⁷Sr/⁸⁶Sr ratios are close to the maximum ⁸⁷Sr/⁸⁶Sr ratios of spring precipitation in Japan, when Kosa activity is marked; and (2) their mole ratios of Mg/Ca (0.15) and Sr/Ca (0.001) are almost identical to those of precipitation in China and Japan when Kosa activity is marked. The ⁸⁷Sr/⁸⁶Sr, Mg/Ca, and Sr/Ca ratios in the acid-soluble components can be used as indexes of Kosa aerosols in the precipitation of the northwestern Pacific.