湿润速率对中性紫色水稻土磷素淋溶动态的影响

为了研究土壤湿润速率对土壤磷素淋溶的影响,以国家紫色土土壤肥力与肥效监测基地的长期定位试验为研究对象,开展了室内磷素淋溶模拟分析以及田间原位监测试验。结果表明:自然存水条件下的水稻土磷素淋溶主要发生在2h快速湿润速率下,有机肥配施氮磷钾肥和单施氮磷钾肥处理最高全磷(TP)浓度相当,比无肥和单施有机肥处理高14.97%,土壤湿润后的微生物生物量碳在2h时出现最低值,且随湿润速率的减缓逐渐升高,但土壤在不同湿润速率下淋洗出的磷浓度与土壤微生物生物量碳含量间无线性负相关,说明该土壤湿润后淋洗出的磷主要来源于土壤胶体,表明吸附的磷或者土壤溶液中的磷淋洗程度主要取决于土壤磷素状况;田间原位监测试验指出,经过48h后田表水TDP、可溶性有机磷(DOP)、钼酸反应磷(MRP)浓度显著降低,MNPK、NPK、M、CK处理的TDP浓度分别降低了32.66%,15.76%,12.83%,57.07%;DOP在室内淋洗液和田间田表水中所占的比例均高于MRP,有机肥配施氮磷钾肥增强了稻田磷素淋失的风险,农业生产过程中应注重有机肥的施用。     

淋洗法测试肥料氮素释放性能研究

分别采用水浸泡法、间歇淋洗法和连续淋洗法测试肥料氮素释放性能,考察了不同模拟土壤介质的淋洗结果,并从介质饱和含水率、水分张力和阳离子交换量等方面综合分析了模拟土壤效果。实验表明:水浸泡法与无介质连续淋洗法结果具有良好的相关性,都符合y=ax+b释放模型;相同介质间歇淋洗法和连续淋洗法结果具有良好的相关性,都符合N=N0/[1+exp(A-kt)]释放模型;蛭石+土壤(体积比1∶1)能更好地模拟土壤性能。模拟土壤连续淋洗法可用于肥料生产企业在线检测。     

土壤中水溶性铜对西红柿的毒害影响因素及预测模型

该文选取17种具有代表性的中国土壤,研究了土壤孔隙水以及0.01mol/LCaCl2浸提态Cu对西红柿生长的毒害,结果发现对于土壤孔隙水中Cu对西红柿生物量10%抑制的毒性阈值(EC10)和50%抑制的毒性阈值(EC50),在17个非淋洗土壤中变化范围分别为0.06～1.47和0.17～3.42mg/L,淋洗土壤变化范围分别为0.05～2.24和0.13～4.37mg/L,最大值与最小值相差为23～41倍;0.01mol/LCaCl2提取态Cu的EC10和EC50,在非淋洗土壤变化范围分别为0.18～2.64和0.57～6.14mg/kg,淋洗土壤变化范围分别为0.18～1.28和0.61～7.11mg/kg,相差从6.9～14.4倍,表明土壤溶液性质影响水溶性Cu对西红柿的毒性阈值。同时,发现土壤孔隙水中Ca2+、溶解性有机碳是影响孔隙水中Cu对西红柿生长毒性的主要因子。当进一步考虑土壤溶液的重要因子(溶解性有机碳、土壤溶液pH值、电导率、全硫含量、Ca2+、Mg2+、K+、Na+),发现基于水溶性Cu的毒性阈值和土壤溶液性质的多元回归系数变化范围为0.75～0.99,说明利用土壤溶液性质能较好的预测土壤中水溶性Cu对西红柿的毒性阈值。该研究可为土壤水溶性Cu的风险评估提供参考。     

广州城郊菜地土壤磷素特征及流失风险分析

通过化学分析和土壤淋洗试验对广州城郊菜地土壤磷素特征和流失风险进行了研究和分析。结果表明，广州城郊菜地土壤全磷含量极高；与自然土壤相比较，菜园土壤无机磷比例增大，有机磷比例降低；无机磷中的Al-P、Fe-P比例增加，O－P比例降低，Ca-P比例基本一致；土壤Olsen P、Bray-1 P、Mehlich-1 P、0.01mol/L CaCl2和H2O提取的磷含量相当高；土壤淋洗液中溶解态磷和总磷持续保持很高的浓度，土壤磷供应强度大。菜园土壤中磷进入水体引起水体磷浓度增加，导致水体富营养化风险大；土壤磷的测定值可作为土壤磷流失风险和对水环境影响程度的评估依据。菜地作为农业非点源污染的优先控制区，应通过严格控制磷肥的投入和合理施肥等控制磷的流失。     

杭州市城市土壤重金属的潜在可淋洗性研究

研究了杭州市城市土壤 8个重金属元素 (Cd、Co、Cr、Cu、Ni、Pb、Zn、Mn)的含量、形态和潜在可淋洗性。结果表明 ,该城市土壤中Cd、Cr、Cu、Ni、Pb、Zn和Mn均有明显的积累 ,其中Cd、Co、Cr和Ni主要以稳定的残余态为主 ,而Cu、Pb、Zn和Mn则以可提取态为主 ,因此在强还原、强酸性或有利于有机质分解条件下Cu、Pb、Zn、Mn的释放潜力较高。用荷兰能源研究中心的淋洗方法 (pH4 0 )测试表明 ,该市城市土壤的重金属可淋洗性较低 ,在一般条件下该城市土壤重金属不会有较大的释放 ,这与该城市土壤中酸可提取态重金属比例较低并含有较高的有机质及粘粒含量有关     

植物残体分解液淋洗对土柱 Ca2+ 淋失量的影响

选取紫花苜蓿、羊草、冷蒿3种北方草原代表性的草本植物,通过土柱淋洗试验,研究植物残体分解液淋洗对土壤溶液Ca2+ 含量的影响.结果表明,不同的植物残体种类和分解期对淋洗后土柱中溶液相Ca2+ 总量的影响不同,其中羊草初期分解液导致的降低量最大,促进土壤碳酸盐的溶解,而紫花苜蓿初期分解液的降低量最小,有利于土壤碳酸盐的稳定.因此,植被自然更替(草场退化)或人为更替(退耕还草)时会影响到土壤溶液中Ca2+ 的浓度,进而影响土壤中碳酸盐的沉淀-溶解平衡,最终导致土壤无机C库的增减.     

有机无机肥配合对土壤磷素吸附、解吸和迁移特性的影响

通过32P示踪、薄层层析和土柱淋洗研究了经过四季不施磷肥、施用纯无机磷肥以及有机无机磷肥3种处理对土壤磷素迁移的影响。结果表明:有机无机肥配合处理的土壤磷吸附亲和力常数和最大吸附量显著低于化肥处理,磷累积解析量高于化肥处理,而32P在薄层板的迁移距离显著高于化肥及对照处理;淋洗试验中有机无机肥配合处理土壤中的32P最先在淋洗液达到13.1mL时出现,而化肥及对照的32P则分别在淋洗液达19.0和19.8mL时出现;在淋洗液体积达到50mL时,对照、化肥及有机无机肥配合处理淋出的32P总量分别为总加入量的1.6%、8.4%和9.8%。有机无机肥配合可以减少土壤磷素的固定,增强磷在土壤中的移动,提高磷的有效性。     

不同施磷量下稻田土壤磷素平衡及其潜在环境风险评估

【目的】对南方赤红壤区不同施磷量下稻田土壤的磷素平衡及其潜在环境风险进行评估,为该地区合理施磷、 减轻农业面源污染提供依据。【方法】采用大田定位监测试验,3个不同年份(2011~2013年)早、 晚稻分别设置4个施磷水平(施磷范围为P2O5 0、 63~81、 126~162、 252~324 kg/hm2,分别用P0、 P1、P2、P3表示),连续3年测定早、 晚稻的稻谷和稻秆产量,分析其磷养分含量,以施磷水平与水稻地上部磷素累积量间的差值表示土壤磷素表观盈余量。同时,采集施基肥和穗肥后1、 2、 3、 5、 7和9 d的田面水,测定总磷含量,利用Split-line模型对2011~2012年每造水稻收获后小区耕层土壤Olsen-P含量和所有监测时间点的田面水总磷平均浓度进行分段回归,并对二者之间的相关关系进行分段回归拟合。【结果】 施磷量P2O5 63~81 kg/hm2的处理稻谷产量显著提高,但磷肥施用量增至2倍时,稻谷产量无明显增加,继续增至4倍时,前3造水稻稻谷的产量增加也不明显。施磷可不同程度地提高水稻地上部的磷素累积量、 土壤表观磷素盈余量和Olsen-P含量,且三者均随施磷量的增加而增加。在施肥后1~3 d内无磷处理田面水总磷浓度较高,是磷素流失的高危险期; 施磷量P2O5 63~81 kg/hm2的处理显著提高了施肥后2 d内田面水的总磷浓度,而P2O5 252~324 kg/hm2的处理在监测期间田面水总磷浓度均显著高于无磷处理。 Split-line模型模拟土壤Olsen-P与田面水总磷的关系,得出在本试验区土壤环境条件下,可能导致田面水中磷激增的土壤Olsen-P临界含量为19.0 mg/kg,对应的施磷量为P2O5 63 kg/hm2,与土壤磷素持平的施磷量一致。【结论】综合考虑水稻产量效应、 土壤磷素表观平衡和磷素环境风险,在本研究区域目前的土壤环境条件下,P2O5 63 kg/hm2为水稻产量较高、 环境风险较小的推荐施磷量。     

柠檬酸/柠檬酸钠淋洗铬污染土壤效果及弱酸可提取态铬含量的变化

研究了用0.2 mol.L-1柠檬酸/柠檬酸钠（摩尔比为1∶1）复合淋洗剂对污染土壤中铬的淋洗效果,及淋洗过程中C（rⅥ）和C（rⅢ）以及弱酸可提取态的含量随淋洗时间的变化,污染土壤取自于沈阳市沈北新区铬渣堆放场地污染土壤。结果表明,在该复合淋洗剂的解吸附与络合的双重作用下,总铬的短时间去除效率较高,淋洗8 h和24 h的去除率分别为33.6%和36.0%,其中淋洗24h时C（rⅥ）和C（rⅢ）的去除率分别达到38.5%和30.0%。淋洗过程中土壤中铬的形态发生了重新分配,弱酸可提取态占总铬比例增加,从而有利于铬在土壤中的迁移。     

生物有机无机复混肥的养分释放特征研究

通过好气培养间歇淋洗法和室内培养法,研究了生物有机无机复混肥的养分释放和氮素在土壤中的矿化规律。结果表明,生物有机无机复混肥的氮磷钾淋洗累积量呈现"S"型曲线,氮素淋洗释放量在第21 d达到最高峰,磷素在第28 d养分释放量达到高峰,钾素在28~35 d出现养分释放高峰,养分释放更加平缓;氮素在土壤中矿化率2.8%~3.2%,0~18 d表现为净固定过程,18 d以后开始矿化释放无机氮,第35 d达到高峰,硝化作用进行比较缓慢,硝化率表现为前期弱,后期强。     

异丙隆在土壤中的淋溶迁移及其影响因素研究

采用室内土壤淋洗柱法,以黄褐土、砂姜黑土和水稻土为供试土壤,研究了异丙隆在土壤中的淋溶迁移行为,探讨了淋溶水量、淋溶水pH值、施药量和添加外源木炭等因素对异丙隆在土壤中淋溶迁移的影响。结果表明,不同土壤中异丙隆淋出率为黄褐土〉砂姜黑土〉水稻土;淋溶水量与异丙隆的淋出率呈正相关,且对淋溶后异丙隆在土层中的分布有明显影响;用不同pH值的淋溶水时,异丙隆的淋出率为pH5〉pH9〉pH7;施加不同药量时,异丙隆的淋出率为10mg〉5mg〉20mg;异丙隆的淋出率随外源木炭添加量的增大而减小,而异丙隆在土壤柱中的滞留量则随着木炭添加量增大而增大,提示添加外源木炭可明显减少异丙隆在土壤中的淋出率,降低异丙隆在土壤中的淋溶深度。     

Mobilization of Cu and Zn in contaminated soil by nitrilotriacetic acid

Batch and upflow column leaching experiments were used to evaluate the nature and extent of Cu and Zn solubilization from contaminated soil by nitrilotriacetic acid (NTA) in 0.025 M NaClO₄. In batch soil suspensions, NTA levels of 10^?5 to 10^?3 M substantially promoted Cu and Zn release from the metal-enriched soil. The ability of NTA to enhance Cu and Zn solubility decreased with increasing solution acidity probably due to competitive binding of NTA by protons and Fe released by hydrous oxide dissolution. However, in the pH range typically encountered in northeastern U.S. soils, soluble metal levels were nearly constant for a given NTA concentration. Leaching soil columns with NTA solutions enhanced Cu release more than Zn, as the enrichment ratio (cumulative metal leached by NTA compared to the 0.025 M NaClO₄ control leachate) after 85 pore volumes displacements was 23.6 and 4.3 for Cu and Zn, respectively. While Cu release by 0.01 M CaCl₂ differed little from the control, 0.01 M CaCl₂ was substantially more effective than 10^?5 M NTA in displacing bound Zn. The data reflect different retention mechanisms for Cu and Zn in this soil.     

Solubility and Leaching of Boron from Borax and Colemanite in Flooded Acidic Soils

Boron (B) is a micronutrient essential for adequate plant growth. Borax (Na₂B₄O₇·10H₂O) and colemanite (Ca₂B₆O₁₁·5H₂O) are common B fertilizer materials, the former being widely used worldwide. Boron is completely water soluble and subjected to leaching. In this study, the dissolution kinetics of both borax and colemanite in deionized water and at pH 3.8, 5.2, 6.5, and 8.2 were determined. Soils incubated with minerals for 40 days and 80 pore volumes of leachates from repacked soil column treated with either surface-applied borax or colemanite (powdered and granular) were collected and analyzed for B contents. Two different soils, Chempaka (Typic paleudult) and Tepus (Typic Kandiaquult) series, taken from paddy-growing areas were used in leaching and incubation studies. Dissolution rate of borax was greater than that of colemanite, and complete dissolution was observed after 100 min, whereas complete dissolution of colemanite was not reached even after 300 min. There was no effect of pH on dissolution rate of borax and colemanite. Boron released from borax was hasty, and after 5 weeks no more B was released. In the case of colemanite, B released was steadily increased until the end of the incubation study. At the end of the study, there was no significant difference in B levels of both borax- and colemanite-applied soils. Particle size had a significant effect on the solubility and dissolution rate of colemanite. Boron dissolution rate and solubility from colemanite powder were significantly greater than those from granular colemanite. Leaching losses from borax were much greater than from colemanite as indicated by the breakthrough curves, which were earlier for borax than colemanite. After 60 pore volumes, no more B was leached out from borax, and in the leachates of colemanite some concentration was detected even after 80 pore volumes. Boron content in soil of columns after the completion of the experiment was greater in case of colemanite. Borax and colemanite fertilizers showed the same trend of leaching and B releasing in both Tepus and Chempaka soil series.     

Soil pH on mobility of imazaquin in oxisols with positive balance of charges

The influence of soil pH on the leaching potential of the ionizable herbicide imazaquin was assessed on the profile of two highly weathered soils having a net positive charge in the B horizon, in contrast to a soil having a net negative charge in the whole profile, using packed soil column experiments. Imazaquin leached to a large extent and faster at Kd values lower than 1.0 L kg(-1), a much more lenient limit than usually proposed for pesticides in the literature (Kd < 5.0 L kg(-1)). The amount of imazaquin leached increased with soil pH. As the soil pH increased, the percentage of imazaquin in the anionic forms, the negative surface potential of the soils, as well as imazaquin water solubility also increased, thus reducing sorption because of repulsive electrostatic forces (hydrophilic interactions). For all surface samples (0-0.2 m), imazaquin did not leach at soil pH values lower than pKa (3.8) and more than 80% of the applied amount was leached at pH values higher than 5.5. For subsurface samples from the acric soils, imazaquin only began to leach at soil pH values > zero point of salt effects (ZPSE > 5.7). In conclusion, the use of surface K(oc) values to predict the amount of imazaquin leached within soil profiles having a positive balance of charges may greatly overestimate its actual leaching potential.     

Effect of two moisture regimes on P-release from P treated soils

Understanding phosphorus (P) release under different climatic or moisture regimes will facilitate effective management of plant nutrition. The objective of this study is to evaluate the effect of two soil moisture regimes on P release from Ogun rock phosphate (ORP) and Sokoto rock phosphate (SRP) in two soil types. Soil was poured into soil columns to form lower and top layers. Top layer was mixed with 400 kg ha^?1 P from ORP, SRP, single super phosphate (SSP) and leached with 35.4 cm³ water representing low moisture regime (LMR; 400 mm rainfall) and 106.1 cm³ water for high moisture regime (HMR; 1200 mm rainfall). P concentrations of leachates, available P in soil and soil pH were determined. Cumulative P leached was higher under HMR than LMR in both soils. There was more leaching with SSP (0.41–0.97 mg P) than both phosphate rocks (0.008–0.19 mg P) indicating leaching potential of SSP. Cumulative P leached from SSP treated Olokemeji soils was twice that of acidic Sapoba under LMR while they were similar (Olokemeji, 0.97 mg P; Sapoba, 0.94 mg P) under HMR suggesting that LMR enhances fixation of P in acidic soils. Irrigation of P fertilized soils may reduce P sorption in acidic soils.     

Phosphorus leaching in a calcareous soil treated with plant residues and inorganic fertilizer

Column experiments were conducted over 45 d to determine the degree of P mobility. The sandy loam soil was spiked with 200 mg P kg^–1 and 5% organic residues. The treatments included: control without any water‐soluble P and plant residues, potato, wheat, water‐soluble P fertilizer, wheat + water‐soluble P, and potato + water‐soluble P. Each column was leached with distilled water, and leachates were collected and analyzed for P, K⁺, Ca²⁺, Mg²⁺, along with pH and EC. Sequential extraction was performed on soil samples at the end of leaching column experiments. The relatively high initial concentration of P in the leachates decreased to more stable values after 15 d which can be attributed to the colloid‐bound P. The P concentrations in the leachates fluctuated between 8 and 220 mg L^–1 in the water‐soluble–P fertilizer treatment, between 0.80 and 230 mg L^–1 in the potato + water‐soluble‐P treatment, and between 0.90 and 214 mg L^–1 in the wheat + water‐soluble P treatment. Leaching loss of P mainly occurred in the 15 d of leaching, accounting for 94%, 88%, and 65% of total P leached in wheat + water‐soluble‐P, potato + water‐soluble‐P, and water‐soluble‐P treatments, respectively. Maximum amount of P leached was found from an exponential kind model and was in the range 0.45 mg kg^–1 to 125.4 mg kg^–1 in control and potato + water‐soluble‐P treatments, respectively. Sequential extraction results showed that in control and amended soils the major proportion of P was associated with Ca. The leachate samples in all treatments were saturated with respect to hydroxyapatite, β‐tricalcium phosphate, and octacalcium phosphate up to 20 d of leaching, whereas they were undersaturated with respect to Mg‐P minerals through the entire leaching experiment.     

Flow-associated precipitation reactions in saline-sodic soils and their significance

A saline-sodic soil (pH 10.0, ESP 100.0, total soluble salts 10.0 mequiv./100 g) rich in soluble sodium carbonate (7.8 mequiv./100 g) was leached in the laboratory with calcium-containing water. The effect of varying flow velocities and concentration of calcium in the leaching water on the extent of carbonate precipitation was studied by following the composition of leachate in one set of experiments and the redistribution of soluble carbonates in the soil column in another experiment. The results showed that precipitation of soluble carbonates in the soil increased with increasing flow velocity and concentration of calcium in the leaching solution. The results have been discussed in terms of actual flow processes occurring at the wetting front. It is suggested that by controlling the extent of carbonate precipitation, the quantity of amendments containing calcium necessary for the reclamation of sodic soils rich in soluble carbonates can be considerably reduced. The results also suggest that the usual method of determining the gypsum requirement of soils is likely to overestimate the gypsum needs of these soils because a large portion of the soluble carbonates is leached out without reaction with the added gypsum.     

The practice of leaching boron and soluble salts from fly ash-amended soils

The leachability of B and salts from two fly ash-amended soils was conducted in a column leaching experiment. Fly ash was applied to the surface 3 cm of a Baywood (acid) sand and an Arizo (calcareous) sandy, loam at 5% by weight; the columns were continously leached with Colorado River water at two different pH's. Boron from fly ash was solubilized more readily in the Baywood than in the Arizo soil. Addition of fly ash increased B levels in the leachates from 0.25 to 2.35 μg ml^?1 (Baywood) and 0.93 μg ml^?1 (Arizo). Acidified leaching water had no significant effect on B leaching patterns but resulted in leaching higher soluble salts. Approximately 348 and 161 cm of water for the Arizo and the Baywood soils respectively, would be required to reduce the B concentration below a critical limit for B sensitive crops. It is suggested that crops planted when fly ash is applied for disposal/recycling on land should be both salt and B tolerant.     

Relationship between Metals Leached and Soil Type from Potential Acid Sulphate Soils under Acidic and Neutral Conditions in Western Australia

Metal contaminants are likely to be mobilised from soil when in contact with acidic drainage. Soils containing sulphide are often associated with significant quantities of trace metals. Understanding the source of metal pollution is of significant concern for management because sulphide-containing soils are found in close proximity to estuaries, lowland rivers and lakes. This study focuses on Western Australian soils, which are typically sandy and well weathered. Two leachate trials, a batch and a column method, investigated the possibility of characteristic leachate signatures with respect to future traceability of metal contamination from soil drainage. Leaching signatures were assessed for four soil types (grey sand (GS), iron-rich sand (FeRS), silty sand (SS) and peat) found coastally between Perth and Albany, in Western Australia. Trace metals leached from the four soil types showed significant differences for both the metals leached and the concentrations for the column leaching trial. No nickel (<1.0 µgL^?1) but relatively high concentrations of arsenic were leached from the peat site. The FeRS leachates contained chromium, copper, high aluminium and relatively high iron. The GS leached extremely high iron and relatively high manganese concentrations. In comparison, only small concentrations of nickel, iron, aluminium, arsenic and manganese leached from the SS columns. Selenium did not leach above reporting limits (<1.0 µg L^?1) from any of the soil types. This work suggests that leachate signatures from different soil types exist and that soil type should be considered when determining the risk of aquatic impact associated with acidic drainage.     

Sorption and mobility of 14C-labeled imazaquin and metolachlor in four soils as influenced by soil properties

Aqueous batch-type sorption-desorption studies and soil column leaching studies were conducted to determine the influence of soil properties, soil and suspension pH, and ionic concentration on the retention, release, and mobility of [14C]imazaquin in Cape Fear sandy clay loam, Norfolk loamy sand, Rion sandy loam, and Webster clay loam. Sorption of [14C]metolachlor was also included as a reference standard. L-type sorption isotherms, which were well described by the Freundlich equation, were observed for both compounds on all soils. Metolachlor was sorbed to soils in amounts 2-8 times that of imazaquin, and retention of both herbicides was related to soil organic matter (OM) and humic matter (HM) contents and to herbicide concentration. Metolachlor retention was also related to soil clay content. Imazaquin sorption to one soil (Cape Fear) increased as concentration increased and as suspension pH decreased, with maximum sorption occurring in the vicinity of pK(a1) = (1.8). At pH levels below pK(a1) imazaquin sorption decreased as hydronium ions (H3O+) increased and competed for sites. NaCl was more effective than water in desorption of imazaquin at pH levels near the pK(a1). Mechanisms of bonding are postulated and discussed. The mobility of imazaquin through soil columns was in the order Rion > or = Norfolk > Cape Fear > or = Webster, whereas for metolachlor it was Rion > or = Norfolk > Webster > or = Cape Fear. Imazaquin was from 2 to 10 times as mobile as metolachlor.