Long-term application of animal slurries to grassland alters soil cation balance

Abstract. Soil samples from a 32-year grassland field experiment were taken from 0–5, 5–10, and 10–15 cm soil depths in February 2002. Plots received annual treatments of unamended control, mineral fertilizer, three rates of pig slurry and three rates of cow slurry, each with six replicates. Samples were analysed for cation exchange capacity (CEC), exchangeable cations (Na⁺, K⁺, Ca²⁺, Mg²⁺), pH and Olsen P. Exchangeable sodium percentage (ESP) was calculated as a sodicity indicator. Mean ESP was generally greater for slurry treatments than the control, with a trend of increasing ESP with application rate. This was particularly marked for cow slurry. At 0–5 cm depth ESP increased from 1.18 in the control to 1.75 at the highest rate of pig slurry and 5.60 at the highest rate of cow slurry. Similar trends were shown for CEC, exchangeable Na⁺, K⁺ and Mg²⁺, Ca²⁺ and Olsen P. The build-up of soil P due to slurry applications, together with this combination of physical and chemical factors, may increase the risk of P loss to surface waters, particularly from soils receiving high rates of cow slurry.     

2018年春季和夏季莱州湾营养盐结构及限制特征

根据2018年5、8月莱州湾的生态调查资料,采用营养盐限制法则及潜在性富营养化评价模式等方法,对莱州湾无机氮(DIN)、活性磷酸盐(PO34–-P)和硅酸盐(SiO23–-Si)的平面分布、结构及限制特征进行了分析。结果显示,2018年5、8月莱州湾的DIN浓度范围为1.64~106.36 μmol/L,平均值为24.18 μmol/L,5月明显高于8月;PO34–-P浓度范围为0~2.010 μmol/L,平均值为0.182 μmol/L,8月明显高于5月;SiO23–-Si浓度变化范围为0.97~78.93 μmol/L,平均值为18.30 μmol/L,8月明显高于5月。DIN、PO34–-P、N/P高值区主要位于莱州湾西部的小清河口和黄河口附近海域;SiO23–-Si、Si/N、Si/P高值区主要位于湾底部、龙口–莱州近岸海域。对营养盐结构的分析表明,莱州湾存在明显的磷限制和枯水期的硅限制,陆源输入是莱州湾营养盐的主要来源。营养盐结构限制平面分布表明,春季莱州-招远养殖区和夏季东营-潍坊养殖区易引发赤潮,夏季莱州–招远养殖区初级生产力受到一定限制,对养殖业造成一定的影响。     

Soil phosphorus fractions and their availability over natural succession from clear-cut of a mixed broadleaved and Korean pine forest in northeast ChinaOA

To assess phosphorus(P) status of forest soil under naturally restored vegetation, P fractions in the 10-cm soil layer were quantified at different successional stages on the clear-cut site of mixed broadleaved and Korean pine forest. Four communities of shrub, softwood broad-leaved forest, softwood and hardwood broad-leaved forest, and hardwood broad-leaved forest represented different successional stages. A soil sample from a primary broad-leaved and Korean pine stand was the control. A sequen...     

日本北海道北部寒温带森林流域林冠层凋落物及其养分归还量的景观格局(英文)

Within a forested watershed at the Uryu Experimental Forest of Hokkaido University in northern Hokkaido, overstory litterfall and related nutrient fluxes were measured at different landscape zones over two years. The wetland zone covered with Picea glehnii pure stand. The riparian zone was deciduous broad-leaved stand dominated by Alnus hirsuta and Salix spp., while the mixture of deciduous broadleaf and evergreen conifer dominated by Betula platyphylla, Quercus crispula and Abies sachalinensis distributed on the upland zone. Annual litterfall averaged 1444, 5122, and 4123 kg.hm^-2·a^-1 in the wetland, riparian and upland zones, respectively. Litterfall production peaked in September-October, and foliage litter contributed the greatest amount （73.4%-87.6 %） of the annual total litterfall. Concentrations of nutrients analyzed in foliage litter of the dominant species showed a similar seasonal variation over the year except for N in P glehnii and A. hirsuta. The nutrient fluxes for all elements analyzed were greatest on riparian zone and lowest in wetland zone. Nutrient fluxes via litterfall followed the decreasing sequence： N （11-129 kg.hm-2.aq） 〉 Ca （9-69） 〉 K （5-20） 〉 Mg （3-15） 〉 P （0.4-4.7） for all stands. Significant differences were found in litterfall production and nutrient fluxes among the different landscape components. There existed significant differences in soil chemistry between the different landscape zones. The consistently low soil C：N ratios at the riparian zone might be due to the higher-quality litter inputs （largely N-fixing alder）.     

淡水养殖对长江氮磷输出的贡献及其河口环境效应

本研究利用集成式环境评估模式—营养盐模型(IMAGE-GNM),计算了2003—2018年长江流经主要省份淡水养殖引起的总氮(TN)和总磷(TP)年排放量。结果显示,长江流域淡水养殖产生的TN和TP释放量具有一致的空间分布,由湖北、湖南和江西省组成的中游占淡水养殖TN和TP总排放量的60%以上;2003—2018年长江流经的主要省份淡水养殖的TN和TP负荷均呈增长趋势,且TP的增长幅度略高于TN;长江流域淡水养殖TN和TP的年排放量分别占2010年长江N、P输送量的7.93%和13.65%,是长江水体N、P营养盐重要的来源;淡水养殖污染的N/P介于6.35～12.53之间(质量比),也对长江水体N/P失衡起到了一定的缓解作用。本研究估算与观测结果一致性较高,相关估算在一定程度上反映了长江流域养殖污染的现状;随着淡水养殖过程中N、P释放通量的增加,河流—河口富营养化的程度可能会加剧,值得进一步的关注。     

过量施用磷肥和有机肥对土壤磷渗漏的影响

采用土柱培养的模拟试验方法,研究在不同磷水平土壤上大量施用磷肥和有机肥对土壤测试磷、土壤磷渗漏的影响及机理。结果表明,不同磷水平土壤施用磷肥和有机肥后,土壤CaCl2-P、Olsen-P和土壤渗漏液中可溶性磷均显著增加;单位量磷肥或有机肥所增加土壤各形态磷量随土壤磷水平的增加而增大;随着磷肥和有机肥用量的增加,单位量磷肥或有机肥所增加各形态磷量也逐渐增大,差异均达到显著和极显著水平;施用磷肥和有机肥土壤磷的最大吸磷量（Qm）和土壤磷吸持指数（PSI）逐渐减少,土壤磷的吸附饱和度（DPS）逐渐增加;单位量磷肥或有机肥所增加的土壤磷的吸附饱和度随着土壤磷水平的增加而增加。随磷肥和有机肥用量的增加,不同磷水平土壤磷的吸附饱和度逐渐增加、土壤磷的吸持指数下降、土壤磷的渗漏量逐渐增大;土壤磷渗漏量与土壤测试磷呈显著正相关;单位量磷肥或有机肥所增加的土壤测试磷随着磷肥或有机肥用量以及土壤磷水平的增加而增加。     

中国稻田土壤有效磷时空演变特征及其对磷平衡的响应

以农业农村部始于1988年的全国稻田土壤监测数据库为基础,将稻作区划分为东北、长江三角洲(简称"长三角")、长江中游、华南和西南五个区域,分析近30 a各稻作区土壤有效磷含量、磷肥回收率及农学效率和磷素的表观平衡,揭示各区域间稻田土壤磷素时间演变和空间差异特征,为稻田土壤磷素科学管理提供理论依据.结果表明,全国主要稻作...     

低磷胁迫下玉米幼苗生理响应及相关基因表达研究

以玉米品种合344为试验材料,对低磷胁迫下玉米幼苗叶片生理表型指标与玉米叶片转录组差异基因表达数据联合分析,探究低磷胁迫下与玉米幼苗叶片生理表型变化相关的关键响应基因及其调控规律.结果表明,低磷胁迫下玉米叶片的叶绿素荧光参数(FV/FM)以及叶绿素含量均有不同程度的降低,并且叶绿素合成相关基因大部分为下调表达,叶绿素降...     

柑桔配施氮、磷、钾肥效应研究初报

本试验研究了在同一施氮水平下，不同水平磷、钾配施及施用不同种类钾肥对柑桔营养、产量及品质的效应。结果表明，紫色黄泥土锦橙园采用适当氮、磷、钾肥配合施用对提高单产及改善果实品质具有明显作用，以株施Ｎ４６０９、Ｐ_２Ｏ_４００ｇ、Ｋ_Ｏ５６０ｇ效果最佳，经济效益也最大。在一定范围内，叶片中的磷、钾养分含量都随磷、钾化肥用量的增加而提高。     

Long term fertilization effects on ‘Rio Red’ grapefruit yield and shape on a heavy textured calcareous soil

Fertilizer recommendations for citrus production on heavier textured, calcareous soils increase with the age of the tree up to 168 kg N ha⁻¹ year⁻¹ from a soluble source in one or two applications. Such practices may be inefficient and could cause detrimental effects on fruit quality. A variety of fertilization practices are used in South Texas, and additional evaluation is needed. Rates and sources of nitrogen (N), phosphorus (P), and a commercial program consisting of both a soil component containing organic acids and a foliar component were evaluated on grapefruit production for 6 years. Increasing rate of N application increased leaf nutrient concentration, grapefruit yield, and affected fruit shape as indicated by a decrease in the equatorial:polar diameter (E:P) ratio. Since the response to increasing N application by the E:P ratio was linear while grapefruit yield was quadratic, high N application has a negative effect on fruit shape beyond the level of increasing total yield. Phosphorus application had no effect on any parameter measured, even though soil testing indicated soil P levels were below those at which a P response would be expected. Comparisons between granular 21-0-0 applied broadcast and liquid N-32 injected in a band in the soil at the drip line showed an increase in the number of fruit per tree, but no differences in yield. The ‘Actagro’ program greatly improved available soil P levels and increased the juice brix:acidity ratio, but did not affect grapefruit yield. Phosphorus availability may therefore be a factor in improving grapefruit juice quality. The soil profile within the citrus root zone was found to contain large amounts of inorganic N, but availability of this residual N was limited since yield responses occurred at the N application rates applied in this study. The amount of N contained in the fruit harvested was a small fraction, roughly 5–10%, of the residual amount in the soil. While N uptake in the fruit increased with N fertilizer application, the increase in N taken up relative to the amount applied averaged 42%.