中国乌鲁木齐土壤中有机氯的来源、组成与风险评价

Twenty-eight surface soil samples from 5 functional zones (park, traffic roadside, business/residential area, rural area, and industrial area) of Ürümqi, China were collected and analyzed for the concentrations of 14 organochlorine pesticides (OCPs), such as 3 isomers of hexachlorocyclohexane (HCHs) (α-HCH, β-HCH, and γ-HCH), 4 dichlorodiphenyltrichloroethanes (DDTs) (p, p’-DDT and its metabolites p, p’-DDD (1,1-dichloro-2,2-bis(p-chlorophenyl)ethane) and p, p’-DDE (1,1-dichloro-2,2-bis(4-chorophenyl)ethylene), and o, p’-DDT), and methoxychlor, aiming to survey the residue levels and compositions of these 14 OCPs, to identify possible sources of the OCPs, and to assess their potential risks to human health and the environment in surface soils of Ürümqi. The concentrations ranged from non-detected to 30.86 μg kg^-1 for HCHs (sum of α-, β-, and γ-HCH), from non-detected to 40.03 μg kg^-1 for DDTs (sum of p, p’-DDT, p, p’-DDD, p, p’-DDE, and o, p’-DDT), and from non-detected to 11.95 μg kg^-1 for methoxychlor. The total concentrations of the OCPs ranged from 16.40 to 84.86 μg kg^-1, with a mean of 41.89 ± 16.25 μg kg^-1. According to the measured concentrations and occurrence rates of the 14 OCPs, DDTs, HCHs, and methoxychlor were the most dominant compounds. Among the 5 functional zones, the total concentration of OCPs was in the order of rural area > traffic roadside > park > business/residential area > industrial area. The different compositions of DDTs and HCHs indicated that the residues of these compounds in most soil samples originated from historical application, besides slight recent introduction at some sampling sites. The results of Pearson correlation analysis showed that soil total organic carbon played an important role in the residue levels of HCHs, but such relationships were not found with DDTs or other OCPs. The soil quality of Ürümqi was classified as Class I based on the guidelines of the Chinese Environmental Quality Standard for Soil (GB15618-1995), indicating that the residue levels of OCPs have little risks to the environment and human health in the study area.     

运用红边参数估算叶片叶绿素含量

Soil samples collected from several sites along an altitudinal transect on the eastern slope of the Tibetan Plateau were analyzed for hexachlorobenzenes(HCHs) and dichlorodiphenyltrichloroethanes(DDTs).The results showed that HCHs and DDTs were found in the soil samples from the remote high altitude areas away from source regions,which confirmed the long-range atmospheric transport phenomenon of these organochlorine pesticides(OCPs) insecticides.The OCP concentrations in the soils had a significant negative correlation with altitude;they showed a trend to increase with decreasing altitude,but the increase was not continuous,being interrupted at some moderate-altitude sites on the transect.The distances from the source region,landforms,soil properties,and physical-chemical properties of OCPs were more important than total organic carbon content to the distribution of OCPs in soils disturbed by human activities.An analysis of the compositions of HCH isomers and DDTs revealed predominantly low ratios of α-HCH to γ-HCH,ranging from 0.06 to 4.79,which suggested current lindane inputs.On the other hand,low p,p-DDT/p,p-DDE and o,p-DDT/p,p-DDT ratios were observed,indicating mainly aged historical DDT residues in the study area.     

漳州土壤中有机氯农药残留研究

A soil survey was conducted in Zhangzhou City,an important agricultural region in south of the Fujian Province,China.93 surface soil samples were collected in the paddy fields,vegetable lands,orchards and tea plantations from Zhangzhou City.An additional soil profile was sampled in a paddy field as previous research had indicated high concentrations of organochlorine pesticides(OCPs) in the paddy fields.Dichlorodiphenyltrichloroethanes(DDTs) ranged from 0.64-78.07 ng g 1 dry weight and hexachlorocyclohexanes(HCHs) ranged from 0.72-30.16 ng g 1 dry weight in the surface soil of the whole study region.Ratios of α-HCH/γ-HCH < 4 and o,p-DDT/p,p-DDT > 1 in all soil samples suggested that lindane and dicofol were widely applied in this region in the past.Concentrations of HCHs and DDTs in soils from the four land use types followed the orders:paddy fields > vegetable lands > tea plantations > orchards and tea plantations > orchards > paddy fields > vegetable lands,respectively.Analyses of the data showed no correlation(r < 0.1) between elevation and OCPs contents in paddy fields,orchards and vegetable lands,indicated no significantly different features in distribution of HCHs and DDTs in the soils from low lying plains and mountains and the unsystematic usage of OCPs,and highlighted the fragmented nature of agricultural production in Zhangzhou,as well as the reemission of OCPs from the soils,where high OCPs concentrations were found,in Longhai of Zhangzhou.In addition,no obvious relationship between the OCPs and total organic carbon(TOC)(r < 0.3) was observed in the soil profile.The mean contribution of dicofol in total DDTs was 66% in the whole Zhangzhou region.The approximate burdens of HCHs and DDTs in the surface layer of 0-20 cm were 0.44 and 1.55 t,respectively.The storage of both HCHs and DDTs in soil surface layer(0-20 cm) accounts for 40% burden of the soil layer of 0-50 cm(1.10 t HCHs and 3.87 t DDTs),in which the highest concentrations of OCPs were observed in soil profile.     

太湖地区农田土壤中氯代持久性有机污染物的残留和输入

Selected persistent organochlorine pesticides (OCPs), including 1,1,1-trichloro-2,2-bis(p-chlorophenyl)ethane (DDT)and its principal metabolites 1,1-dichloro-2,2-bis(p-chlorophenyl)ethylene (DDE) and 1,1-dichloro-2,2-bis(p-chlorophenyl)ethane (DDD), hexachlorocyclohexane (HCH) and its isomers (α-, β, γ-, and δ-HCH), hexachlorobenzene (HCB), endosulfan, dieldrin, and endrin were quantified to determine current levels of organochlorine pesticides, to assess the ecotoxicological potential, and to distinguish previous and current inputs in agricultural soils from the Taihu Lake region.Gas chromatography equipped with a 63Ni electron-capture detector (GC-ECD) system was employed. Thirteen OCPs were detectable in all soil samples, with DDTs being the main residues, and HCHs had the second highest level of OCP residues. Although OCP residual levels were lower than those in 1990s, the residual levels for most of the DDTs and some of HCHs were still higher than the national environmental standards for agricultural soils. The ratios of DDT/DDE and γ-/α-HCH in twelve soils indicated that new inputs could be present in the soils. Thus, efforts should be made to completely ban the production of OCPs and their use in agriculture so as to reduce the threat of OCPs to food quality and human health.     

福建茶园茶叶中六六六和滴滴涕残留水平及来源分析

运用气相色谱-电子捕获检测器（GC-μECD）分析了福建茶园茶叶中六六六（HCHs）和滴滴涕（DDTs）等有机氯农药（OCPs）的分布、组成和来源。结果表明,∑OCPs浓度为0.764～10.561ng.g-1,永泰最高,福鼎最低,一般而言,老叶中∑OCPs浓度高于嫩叶;∑HCHs浓度为0.373～7.427ng.g-1,永泰最高,政和最低,老叶中HCHs浓度显著高于嫩叶;茶叶中HCHs同系物以γ-HCH为主,占总量的51.3%～94.1%;α-/γ-HCH表明所有茶园均存在林丹的使用或输入,β-（/α＋γ）-HCH表明所有茶园均非HCHs历史污染,可能存在HCHs其他新的来源。∑DDTs浓度为0.123～5.168ng.g-1,政和最高,福鼎最低,老叶和嫩叶中无显著差异;与土壤类似,茶叶中DDTs同系物以p,p′-DDT和o,p′-DDT为主,两者之和占总量的67.3%～96.0%;p,p′-DDE/p,p′-DDT表明,除福鼎、永泰和安溪外,其他茶园均存在工业DDTs的使用或输入;o,p′-DDT/p,p′-DDT表明,除政和外,其他茶园均存在大量的三氯杀螨醇的使用或输入,以安溪较为严重。     

不同施肥方式下土中有机氯农药的残留特征

Soil samples with three fertilization treatments (no fertilizer, corn straw and farm manure) collected from a Lou soil (Eum-orthic Anthrosol classfied using Chinese Soil Taxonomy) in northwestern China were analysed for residual levels and their characteristics of organochlorine pesticides (α-HCH, β-HCH, γ-HCH, δ-HCH, HCB, o,p'-DDT, p,p'-DDT, o,p'-DDE, p,p'-DDE, p,p'-DDD, a-endosulfan, dieldrin and endrin). Organochlorine pesticides (OCPs) were detected in all soil samples except δ-HCH and their total concentrations ranged from 159.31 ± 9.00 to 179.77 ± 2.58 ng g^-1 with an order of HCHs > DDTs > (dieldrin + endrin) > HCB > α-endosulfan. Among all the compounds, γ-HCH had the highest concentration followed by p,p'-DDE. The residual levels of HCH isomers and DDT as well as their metabolites in soil with different fertilization treatments were in the order of γ-HCH > β-HCH ≈ α-HCH > δ-HCH and p,p'-DDE > p,p'-DDT > o,p'-DDT > p,p'-DDD ≈ o,p'-DDE, respectively. DDE/DDT ratios ranged from 1.59 ±0.13 to 3.35 ± 0.16 and endrin/dieldrin ratios from 1.40 ± 0.06 to 9.20 ± 4.05, both indicating no new occurrence of these pesticides in these soils, while α-HCH/γ-HCH ratios of 0.04 indicated a new input of lindane (almost pure γ-HCH) in the past several years. The farm manure treatments showed lower DDT residues than samples without fertilizer. Also addition of corn straw and farm manure increased soil organic matter content and decreased the soil pH which could retard the degradation of DDT in the soil.     

福建茶园土壤六六六和滴滴涕残留水平及来源分析

采用现场采样及室内测试方法,分析了福建茶园土壤中六六六（HCHs）和滴滴涕（DDTs）类有机氯农药（OCPs）的分布、组成和来源。结果表明,∑HCHs和∑DDTs浓度分别为0.251-1.120 ng.g^-1和0.210-2.406 ng.g^-1,属于清洁背景范围;漳浦、福鼎和福州茶园土壤∑OCPs浓度显著高于其他样点。除福州外,其他样点HCH同系物中γ-HCH相对含量最高,占HCHs总量的26.3%-76.3%。DDTs中以o,p′-DDT相对含量最高,为34.7%-60.8%。0-15 cm土壤HCHs和DDTs浓度（分别为0.593 ng.g^-1和1.340 ng.g^-1）均高于15-30 cm（0.451 ng.g^-1和0.862 ng.g^-1）。除福州β-（/α＋γ）-HCH和α-/γ-HCH值较高外,其他样点均较低,表明福州HCHs为历史污染,其他样点均存在HCHs新输入,并可能存在林丹的使用或输入;除福鼎p,p′-DDE/p,p′-DDT值较高外,其他样点均较低,表明除福鼎外其他样点均有DDTs的新输入;o,p′-DDT/p,p′-DDT值均较高,表明可能有大量三氯杀螨醇的使用或输入。     

辽东与山东半岛土壤中有机氯农药残留特征研究

2005—2008年在辽东半岛和山东半岛15个市县采集了265个土壤样品,对其10种有机氯农药进行了分析,研究该地区土壤中硫丹、HCH和DDT残留情况及其空间分布特征。结果表明,山东半岛土壤中硫丹残留量为6.30μg kg-1,为辽东半岛的9倍;HCHs残留量为4.82μg kg-1,为辽东半岛的1.3倍;辽东半岛土壤中DDTs残留量为45.70μg kg-1,为山东半岛的2.5倍。山东半岛α-HCH、p,p′-DDE、p,p′-DDT的检出率均高于80%,辽东半岛β-HCH、p,p′-DDE检出率均高于80%。不同种植方式,辽东半岛土壤OCPs残留量:果园玉米地菜地草地水稻田;山东半岛土壤OCPs残留量:果园菜地玉米地麦田棉田。与国内其他地区相比,该地区硫丹残留量相对较低,HCHs和DDTs残留量超过国家《土壤环境质量标准》(GB15618-2008)一级标准的土壤样品分别占样品总数的4.53%和9.05%。     

碱渣与菜籽饼共施对茶园土壤酸度调控的研究

Rapeseed cake (RC), the residue of rapeseed oil extraction, is effective for improving tea (Camellia sinensis) quality, especially taste and aroma, but it has limited ability to ameliorate strongly acidic soil. In order to improve the liming potential of RC, alkaline slag (AS), the by-product of recovery of sodium carbonate, was incorporated. Combined effects of different levels of RC and AS on ameliorating acidic soil from a tea garden were investigated. Laboratory incubations showed that combined use of AS and RC was an effective method to reduce soil exchangeable acidity and Al saturation and increase base saturation, but not necessarily for soil pH adjustment. The release of alkalinity from the combined amendments and the mineralization of organic nitrogen increased soil pH initially, but then soil pH decreased due to nitrifications. Various degrees of nitrification were correlated with the interaction of different Ca levels, pH and N contents. When RC was applied at low levels, high Ca levels from AS repressed soil nitrification, resulting in smaller pH fluctuations. In contrast, high AS stimulated soil nitrification, when RC was applied at high levels, and resulted in a large pH decrease. Based on the optimum pH for tea production and quality, high ratios of AS to RC were indicated for soil acidity amelioration, and 8.0 g kg-1 and less than 2.5 g kg-1 were indicated for AS and RC, respectively. Further, field studies are needed to investigate the variables of combined amendments.     

An in-situ Technique for Producing Low-Cost Agricultural Biochar

Application of biochar to agricultural soils is effective to sequester atmospheric carbon and improve soil quality, but current pyrolysis and transportation costs are high, making biochar too costly to be used at the field scale. This study developed a new in-situ technique, burning and soil covering(B-SC), which can be used by farmers for production of biochar with crop residue. In this study,the air-dried feedstocks, elephant grass and corn residue, were burnt in situ for biochar production in the field. After approximately 90% of the leaves were combusted, the burning process was dramatically slowed down by covering the feedstock with soil. The biochar yield averaged 18.0 ± 1.3(n = 15) and 13.7 ± 1.3(n = 10) kg per 100 kg air-dried feedstock for the elephant grass and corn residue,respectively. The biochar properties were suitable for soil improvement. The inputs for biochar production of the B-SC process only included low labor force, open field, feedstock(e.g., grass and crop residue), and simple tools. The operation time for processing 10 kg of the corn residue by an individual farmer was 24.4 ± 4.1 min(n = 10). As compared with the conventional field burning process, the B-SC process drastically shortened the time for biomass burning and generated a significantly lower emission of smoke and thermal energy. This simple technique can be particularly practical and effective for farmers to improve the soils of poor quality in China.     

Long-Term Effects of Different Passages of Vehicular Traffic on Soil Properties and Carbon Storage of a Crosby Silt Loam in USA

The passage of vehicles with heavy axle loads causes soil compaction, and this adversely affects soil properties and crop yield.The adverse effects can persist for several years due to significant changes in key soil properties. However, the mechanisms of the aforementioned effects are not well understood for conservation agriculture(CA)(e.g., no-till(NT)) wherein the use of heavy machinery is considerably common. Therefore, known compaction forces(0 Mg load for compaction(NT-0, control), two passages of 2.5 Mg water wagon axle load(NT-2), and four passages of 2.5 Mg water wagon axle load(NT-4)) were applied to all the plots annually for 20 consecutive years. The experiment was established in 1997 at the Waterman Agricultural and Natural Resources Laboratory(WANRL), Ohio State University, Columbus, Ohio. Each treatment was replicated thrice. Soil samples were obtained in November2016 to determine the effects of variations in the axle load and vehicular passages on carbon(C) and nitrogen(N) storage and selected soil properties of a Crosby silt loam soil under NT-based corn-soybean rotation with residue retention in Central Ohio, USA. Three locations were also randomly selected in an adjoining natural woodlot(WL) soil plot and sampled(30 m away from the compaction field) to compare the effects of vehicular traffic on soil under NT with WL soil. Results revealed that soil bulk density(ρb) and total porosity at 0–10 and 10–20 cm depths were not affected by the passages of vehicular traffic for 20 years under the NT system.The penetration resistance(PR)(1.86 and 2.03 MPa at 0–10 and 10–20 cm soil depths, respectively) was significantly higher under NT-4 compared with that under other treatments. Saturated hydraulic conductivity at 0–10 and 10–20 cm soil depths ranged from19.7 to 31.4 and 18.5 to 29.5 mm d~(-1), respectively, across all the treatments. The proportion of macroaggregates( 0.25 mm) and microaggregates( 0.25 mm), mean weight diameter and geometric mean diameter of aggregates, pH, electrical conductivity, and C and N contents and storage did not differ significantly between the treatments at either of the sampling soil depths. The data indicated that 2 to 4 passages of vehicles with 2.5 Mg of axle load did not cause significant compaction of the Crosby silt loam under NT compared with that under natural WL. Therefore, the continuous cultivation of row crops with NT and residue retention is feasible with passages of vehicular traffic for well-drained soils in Central Ohio.     

施用聚合果属废弃物与生物炭后砂质石灰性土壤二氧化碳排放及生物化学性质的动态

Biochar is a carbon-rich product obtained by biomass pyrolysis and considered a mean of carbon sequestration. In this research, a sandy calcareous soil from the Farm of the College of Food & Agriculture Sciences, King Saud University, Saudi Arabia, was amended with either woody waste of Conocarpus erectus L.(CW) or the biochar(BC) produced from CW at rates of 0(control), 10, 30 and 50 g kg-1. The effects of the amendments on soil p H, dissolved organic carbon(DOC), microbial biomass carbon(MBC), CO2 emission and metabolic quotient(q CO2) of the sandy calcareous soil were studied in a 60-d incubation experiment. The results showed that the addition of CW led to a significant decrease in soil p H compared to the control and the addition of BC. The CO2-C emission rate was higher in the first few days of incubation than when the incubation time progressed. The cumulative CO2-C emission from the soil amended with CW, especially at higher rates, was higher(approximately 3- to 6-fold) than that from the control and the soil amended with BC. The BC-amended soil showed significant increases in CO2-C emission rate during the first days of incubation as compared to the non-amended soil, but the increase in cumulative CO2-C emission was not significant after 60 d of incubation. On the other hand, CW applications resulted in considerably higher cumulative CO2-C emission, MBC and DOC than the control and BC applications. With the exception of 0 day(after 1 h of incubation), both CW and BC applications led to lower values of q CO2 as compared to the control. The power function kinetic model satisfactorily described the cumulative CO2-C emission. Generally, the lowest values of CO2 emission were observed in the soil with BC, suggesting that the contribution of BC to CO2 emission was very small as compared to that of CW.     

滇池周边大棚土壤中六六六和滴滴涕残留特征

采用气相色谱(ECD)对滇池周边不同年限大棚土壤中六六六(HCHs)和滴滴涕(DDTs)残留量进行了测定, 探讨其残留分布特征。结果表明: (1)大棚种植年限对土壤中残留量影响显著, 种植年限长于10 年的大棚土壤中HCHs 和DDTs 的残留量显著高于年限短于10 年的大棚, DDTs 是有机氯农药(OCPs)的主要组成成分;短于10 年的大棚间, 土壤中HCHs 和DDTs 残留量差异不显著。(2)不同土层中, HCHs 残留量在土壤剖面上的变化趋势不明显, 而DDTs 在表层土壤(0~20 cm)中残留量显著高于下层。(3)从HCHs 和DDTs 的同系物组成来看, HCHs 以β-HCH 残留量最高, 部分样点中p,p′-DDT/(DDD+DDE)比值大于1。可判断HCHs 残留主要是过去施用的残留物, 而DDTs 仍有新的污染输入, 有待进一步调查研究。     

从土壤悬浮液的Wien效应推断阳离子与电渗析粘粒组分的相互作用

The electrical conductivities (ECs) of suspensions containing 25 and 30 g kg-1 solids prepared from theelectrodialyzed clay fraction (＜ 2 μm in diameter) of latosol, yellow-brown soil, and black soil, dispersed invarious nitrate solutions having concentrations of 1 × 10-4/z mol L-1, where z is the valence, and in distilledwater, were measured at field strengths ranging from 14 kV cm-1 to 210 kV cm-1. On the basis of analysesof the charge density and exchangeable ion composition on the surfaces of soil particles in the suspensions,and of the characters of the EC-field strength curves of the various suspensions, it was inferred that theincrement of EC (△EC) and/or relative electrical conductivity (REC) can indicate the bonding strengthbetween cations and soil particles. The bonding strengths of various cations with the soils diminished in theorder: K+ ＞ Zn2+ ＞ Mg2+ ＝ Ca2+ ＞ Na+ for latosol, Ca2+ ＞ Zn2+ ＞ Mg2+ ＝ K+ ＞ Na+ for yellow-brownsoil, and Zn2+ ＞Ca2+ ＞ Mg2+ ＞ K+ ＞ Na+ for black soil.     

黄土高原某些耕作土壤中土壤微生物生物量C、N与矿化N的关系

The chloroform fumigation-incubation method was used to measure the soil microbial biomass C (SMBC) and N (SMBN) in 16 loessial soils sampled from Ansai, Yongshou and Yangling in Shaanxi Province. The SMBC contents in the soils ranged from 75.9 to 301.0 μg C g^-1 with an average of 206.1 μg C g^-1, accounting for 1.36%~6.24% of the total soil organic C with an average of 3.07%, and the SMBN contents from 0.51 to 68.40 μg N g^-1 with an average of 29.4 μg N g^-1, accounting for 0.20%~5.65% of the total N in the soils with an average of 3.36%. A close relationship was found between SMBC and SMBN, and they both were positively correlated with total organic C, total N, NaOH hydrolizable N and mineralizable N. These results confirmed that soil microbial biomass had a comparative role in nutrient cycles of soils.     

红壤稻田土壤理化及生物学性状的动态变化特征

Rice production plays a crucial role in the food supply of China and a better understanding of the changes in paddy soil fertility and the management effects is of practical importance for increasing rice productivity. In this study, field sampling in a typical red soil region of subtropical China, Jiangxi Province, was used to observe changes in the soil physical, chemical, and biological properties in a cultivation chronosequence of paddy fields. After cultivation, clay (< 0.002 mm) content in the soil, which was 39% in the original uncultivated wasteland, decreased, to 17% in the 80-year paddy field, while silt (0.02--0.002 mm) content increased. Additionally, macroporosity increased and pore shapes became more homogeneous. Soil Ph generally increased. Soil organic C and total N content of the 0-10 cm layer increased from 4.58 and 0.39 g kg-1 to 19.6 and 1.62 g kg-1, respectively in the paddy fields after 30-year cultivation and then remained stable. Soil total P content increased from 0.5 to 1.3 g kg-1 after 3 years of rice cultivation, indicating that application of phosphate fertilizer could accelerate phosphorous accumulation in the soil. Total K content in the 0--10 cm soil layer for the 80-year paddy fields decreased by 28% compared to that of the uncultivated wasteland land. Total Fe and free Fe contents declined with years of cultivation. The bacterial population increased and urease activity noticeably intensified after years of cultivation. In this chronosequence it appeared that it took 30 years to increase soil fertility to a relatively constant value that was seen after 80 years of cultivation.     

黑土不同土地利用方式下受水分有效性调节的土壤CO2排放的温度敏感性

The quantification of soil CO2 efflux is crucial for better understanding the interactions between driving variables and C losses from black soils in Northeast China and for assessing the function of black soil as a net source or sink of atmospheric CO2 depending upon land use.This study investigated responses of soil CO2 efflux variability to soil temperature interactions with diferent soil moisture levels under various land use types including grassland,bare land,and arable(maize,soybean,and wheat)land in the black soil zone of Northeast China.The soil CO2 effluxes with and without live roots,defined as the total CO2 efflux(FtS)and the root-free CO2 efflux(FrfS),respectively,were measured from April 2009 to May 2010 using a static closed chamber technique with gas chromatography.The seasonal soil CO2 fluxes tended to increase from the beginning of the measurements until they peaked in summer and then declined afterwards.The mean seasonal FtS ranged from 20.3±7.8 to 58.1±21.3 mg CO2-C m-2h-1 for all land use types and decreased in the order of soybean land>grassland>maize land>wheat land>bare land,while the corresponding values of FrfS were relatively lower,ranging from 20.3±7.8 to 42.3±21.3 mg CO2-C m-2h-1.The annual cumulative FtS was in the range of 107-315 g CO2-C m-2 across all land uses types.The seasonal CO2 effluxes were significantly(P<0.001)sensitive to soil temperature at 10 cm depth and were responsible for up to 62% of the CO2 efflux variability.Correspondingly,the temperature coefcient Q10 values varied from 2.1 to 4.5 for the seasonal FtS and 2.2 to 3.9 for the FrfS during the growing season.Soil temperature interacting with soil moisture accounted for a significant fraction of the CO2 flux variability for FtS (up to 61%) and FrfS (up to 67%) via a well-defined multiple regression model,indicating that temperature sensitivity of CO2 flux can be mediated by water availability,especially under water stress.     

添加生物炭对酸性红壤中玉米生长和氮素利用率的影响

Biochar added to soil can improve crop growth through both direct and indirect effects, particularly in acidic, highly weathered soils in subtropical and tropical regions. However, the mechanisms of biochar improving crop growth are not well understood. The objectives of this study were i） to determine the crop responses to biochar addition and ii） to understand the effect of biochar addition on N use efficiency. Seven acidic red soils varying in texture, p H, and soil nutrient were taken from southern China and subjected to four treatments： zero biochar and fertilizer as a control（CK）, 10 g kg-1biochar（BC）, NPK fertilizers（NPK）, and 10 g kg-1biochar plus NPK fertilizers（BC＋NPK）.15N-labeled fertilizer was used as a tracer to assess N use efficiency. After a 46-d pot experiment,biochar addition increased soil p H and available P, and decreased soil exchangable Al3＋, but did not impact soil availabe N and cation exchange capacity（P 〉 0.05）. The N use efficiency and N retained in the soil were not significantly affected by biochar application except for the soil with the lowest available P（3.81 mg kg-1） and highest exchanageable Al3＋（4.54 cmol kg-1）. Greater maize biomass was observed in all soils amended with biochar compared to soils without biochar（BC vs. CK, BC＋NPK vs. NPK）. This agronomic effect was negatively related to the concentration of soil exchangeable Al3＋（P 〈 0.1）. The results of this study implied that the liming effect of biochar improved plant growth through alleviating Al toxicity and P deficiency, especially in poor acidic red soils.     

基于Century模型和1:500 000土壤数据库的华东旱地土壤有机碳动态模拟

Changes in soil organic carbon (SOC) in agricultural soils influence soil quality and greenhouse gas concentrations in the atmosphere. Dry farmland covers more than 70% of the whole cropland area in China and plays an important role in mitigating carbon dioxide (CO2) emissions. In this study, 4109 dry farmland soil polygons were extracted using spatial overlay analysis of the soil layer (1:500000) and the land use layer (1:500000) to support Century model simulations of SOC dynamics for dry farmland in Anhui Province, East China from 1980 to 2008. Considering two field-validation sites, the Century model performed relatively well in modeling SOC dynamics for dry farmland in the province. The simulated results showed that the area-weighted mean soil organic carbon density (SOCD) of dry farmland increased from 18.77 Mg C ha1 in 1980 to 23.99 Mg C ha1 in 2008 with an average sequestration rate of 0.18 Mg C ha1 year?1. Approximately 94.9% of the total dry farmland area sequestered carbon while 5.1% had carbon lost. Over the past 29 years, the net SOC gain in dry farmland soils of the province was 19.37 Tg, with an average sequestration rate of 0.67 Tg C year1. Augmentation of SOC was primarily due to increased consumption of nitrogen fertilizer and farmyard manure. Moreover, SOC dynamics were highly differentiated among dry farmland soil groups. The integration of the Century model with a fine-scale soil database approach could be conveniently utilized as a tool for the accurate simulation of SOC dynamics at the regional scale.     

麦根酸的分泌及其对土壤中铁的有效性的影响

Large amounts of phytosiderophore are detected from both the solution and the rhizosphere soil when cereal crops are under Fe deficiency stress.The extension of phytosiderophore in the rhizosphere soil is found only within 1 mm apart from the root surface.The rate of phytosiderophore secretion is negatively related to chlorophyll content in young leaves and positively related to the Fe-solubilizing capacity.Results from in vitro experiments whow 10 μmoles mugineic acid can dissolve 501 μg Fe from iron hydroxide and 146 ug from strengite.Thus,phytosiderophore can considerably enhance the soil iron availability by increasing the solubility of amorphous iron hydroxide and iron phosphate,and active Fe is consequently accumulated in the plant rhizosphere,43% higher than in the bulk soils There is evidence to support that mugineic acid chelates with Fe%3 at a rate of 1:1 in the acid condition.In addition,we observe mugineic acid has certain effects on mobilization of P as well as Fe by dissolving the insoluble iron phosphate,And phytosiderophore seems to be an effective remedy for the chlorosis of dicotyledonous plants.