不同土地利用方式下紫色土中铵的容量和强度（Q/I）关系

研究了4种土地利用方式下(水田、旱地、林地、菜地)紫色土(紫色湿润雏形土)和紫色水稻土(紫色水耕人为土)NH4+的容量和强度(Q/I)关系。结果表明:紫色土和紫色水稻土NH4+Q/I曲线的曲线部分均出现在NH4+的活度比(ARNH4)较低时,表明土壤存在非交换性NH4+(或专性吸附的NH4+)的释放。紫色土和紫色水稻土NH4+的潜在缓冲容量(PBC)为71.47～203.7 cmol kg-1(mol L-1)-1/2;土壤活性NH4+(-ΔNH40)为0.029 5～0.089 7 cmol kg-1,NH4+的平衡活度比(AR0NH4)为0.187×10-3～1.255×10-3(mol L-1)1/2;土壤专性吸附位点(NH4-sas)为0.010 6～0.118 5 cmol kg-1。相关分析和通径分析表明,土壤小于0.002 mm黏粒含量与NH4+PBC及NH4-sas均呈极显著正相关(p<0.01),小于0.002 mm黏粒对PBC的影响主要是间接作用(间接通径系数为0.585),但对NH4-sas则有强烈的直接作用;有机碳与-ΔNH40和AR0NH4均呈极显著正相关(p<0.01),但是有机碳对-ΔNH40有较大的直接效应(直接通径系数为0.966),而对AR0NH4的影响主要以间接效应为主。土壤-ΔNH40与交换性NH4+数值接近且呈极显著相关(r=0.876 4,n=8,p<0.01),而AR0NH4与交换性NH 4+亦呈极显著相关(r=0.983 7,n=8,p<0.01)。土壤小于0.002 mm黏粒和有机碳的差异是导致不同土地利用方式下紫色土交换性NH4+以及Q/I参数的差异的主要原因,交换性NH4+标志的NH4+有效性指标与由Q/I关系得到的NH4+有效性指标类似。     

土壤沉积物样品中有机碳含量的快速测定

采用微波密闭消解样品的方法来测定土壤／沉积物中有机碳的含量。与重铬酸钾氧化法的结果相比，微波消化法具有操作简单、污染小、快速准确的优点。经F检验法及t检验法检验，两种方法的分析结果无明显差异。     

钾肥对优质面包专用型小麦产量及品质的影响

本文研究了在江苏淮北地区不同钾肥用量对优质面包专用型小麦苏徐1号产量的影响,同时通过长期定位试验研究了增施钾肥对苏徐1号产量及品质的影响。钾肥用量试验结果表明,施用钾肥可增加产量8.3%～13 7%,适宜的钾肥用量为90～135kgK2O/hm2,最佳经济钾肥施用量为135.6kgK2O/hm2,其产量为5056.1kg/hm2,长期定位试验结果表明,施用钾肥可提高苏徐1号的商品品质,在长期不施有机肥(厩肥)的情况下,增施钾肥可改善面粉的加工品质,提高其评价值。     

Phytolith‐associated potassium in fern: characterization,dissolution properties and implications for slash‐and‐burn agriculture

In recent time, phytoliths (silicon deposition between plant cells) have been recognized as an important nutrient source for crops. The work presented here aims at highlighting the potential of phytolith‐occluded K pool in ferns. Dicranopteris linearis (D. linearis ) is a common fern in the humid subtropical and tropical regions. Burning of the fern D. linearis is, in slash‐and‐burn regions, a common practice to prepare the soil before planting. We characterised the phytolith‐rich ash derived from the fern D. linearis and phytolith‐associated potassium (K) (phytK), using X‐ray tomographic microscopy in combination with kinetic batch experiments. D. linearis contains up to 3.9 g K/kg d.wt, including K subcompartmented in phytoliths. X‐ray tomographic microscopy visualized an interembedding structure between organic matter and silica, particularly in leaves. Corelease of K and Si observed in the batch experiments confirmed that the dissolution of ash phytoliths is one of major factors controlling K release. Under heat treatment, a part of the K is made available, while the remainder entrapped into phytoliths (ca. 2.0–3.3%) is unavailable until the phytoliths are dissolved. By enhanced removal of organic phases, or forming more stable silica phases, heat treatment changes dissolution properties of the phytoliths, affecting K release for crops and soils. The maximum releases of soluble K and Si were observed for the phytoliths treated at 500–800 °C. For quantitative approaches for the K provision of plants from the soil phytK pool in soils, factors regulating phytolith dissolution rate have to be considered.     

基于NIR和GIS的甘蔗含糖量与种植条件关系研究

为监测较大区域内甘蔗产量及含糖量的时间、空间变化情况,了解地区、环境及土壤成分与甘蔗含糖量的关系,为甘蔗栽培提供指导,以日本琉球群岛南大东岛甘蔗栽培区为对象,用NIR方法测定甘蔗含糖量及其他成分含量,采用GIS技术建立地块位置、甘蔗产量、含糖量及P、K含量和土壤K含量数据库。在此基础上,建立3个栽培年度甘蔗含糖量、单产与甘蔗汁P、K含量的空间分布图,发现甘蔗含糖量与降水量及种植区水环境密切相关。对甘蔗含糖量及P、K含量和土壤K含量的相关分析表明,甘蔗含糖量与甘蔗汁P含量呈正相关,而与甘蔗汁和土壤K含量均呈负相关。     

基于GIS的长江中游油菜种植区土壤养分及pH状况

为了掌握长江中游油菜种植区土壤养分状况,在湖北、湖南、江西三个省份调查和取样分析5 463份土壤数据的6个指标(土壤有机质、全氮、有效磷、速效钾、有效硼和pH),基于Arc GIS平台,采用Kriging插值法分析4个不同油菜种植区域(二熟制山地区、二熟制平原区、三熟制山地区、三熟制平原区)的土壤养分状况。结果表明,长江中游油菜种植区土壤有机质、全氮和有效磷均处于适宜/丰富的含量水平,基本没有5级和6级水平的有机质、全氮、有效磷分布。从不同区域来看,以上3个养分指标总体均表现为三熟制地区养分含量高于二熟制地区。长江中游仍有1.82×10~5 hm~2区域土壤速效钾处于缺乏的水平(30~50 mg kg~(-1))。土壤有效硼含量仍有待提高,尤其是在三熟制地区,土壤有效硼缺乏(5级和6级)的比例仍高达13.6%~20.4%。土壤pH多集中在6.0左右,但是三熟制地区仍然有较高比例(约35.7%)的土壤pH处于4.5~5.5。综上所述,长江中游不同种植区域土壤养分性状存在差异,尤其是三熟制地区仍有相当比例需要提高土壤有效硼和改良酸性土壤。     

钾用量与灌溉方式互作对土壤-烤烟系统钾素及烟叶品质的影响

旨在探究钾用量与灌溉方式互作对土壤-烤烟系统钾素变化及烟叶质量的影响问题。采用大田裂区设计,研究了不同灌溉方式与钾用量互作对土壤-烤烟系统钾素及烟叶内在化学成分的影响。同一灌溉方式下,增施钾肥显著提高土壤钾素含量,土壤速效钾和缓效钾含量随钾肥用量的增加而增加;与不施钾相比,施钾显著提高烟叶钾含量,但常规施钾与高量施钾处理间烟叶钾含量差异不显著。相同施钾量下,3种灌溉方式相比,以交替对1/2区域灌水处理土壤速效钾和缓效钾含量最低,烟叶钾含量以固定对1/2区域灌水处理最高,但与交替对1/2区域灌溉处理差异不显著。烟叶采收结束时,9个处理的土壤速效钾含量均随土层深度的增加,呈先降低再增加的趋势,至60~100 cm土层趋于稳定。灌水方式和钾用量互作对烟叶化学成分有一定影响,以常规施钾与固定1/2区域灌水处理组合的烟叶化学成分协调性最佳。在常规施钾量下,固定1/2区域灌水处理不仅改变了钾素在不同土层的分布,而且提高了烟叶钾含量,且减少了灌溉用水,建议可在黄淮烟区进行示范应用。     

几株高效溶磷解钾药用稻内生固氮菌的筛选与鉴定

从药用稻(Oryza officinalis)中筛选具有高效溶磷解钾的内生固氮菌,在农业生产上具有很大的潜在应用价值.本研究以药用稻为材料,采用两种选择性无氮培养基结合乙炔还原法进行内生固氮菌的分离,利用平板筛选法从所分离的内生固氮菌中筛选出高效溶磷解钾菌,应用全细胞蛋白SDS-聚丙烯酰氨凝胶电泳(sodium dodecyl sulfate-polyacrylamide gel electrophoresis,SDS-PAGE)对所筛选到的菌株进行快速聚类.选取每个类群的代表菌株进行16S rRNA基因序列测定及生理生化鉴定.通过钼锑抗比色法和四苯硼钠法测定其溶磷解钾量,同时通过接种水稻对其促生作用进行分析.结果表明,从药用稻中筛选到了4株具有高效溶磷解钾能力的内生固氮菌,其固氮酶活性在8.78～8.88 μmol C2H4/(mL·h)之间.SDS-PAGE全细胞蛋白电泳将4株菌聚为1个类群.16S rRNA基因序列相似性分析及理化鉴定表明,代表菌株yy01为久留里伯克霍尔德菌(Burkholderia kururiensis,菌株yy01发酵培养5d后,溶无机磷量达116.28mg/L,是参比菌株变栖克雷伯氏菌(Klebsiella variicola)的2.73倍;解钾量达268.31 mg/L,是参比菌株变栖克雷伯氏菌的4.67倍.此外,yy01还具有分泌生长素等特性,接种水稻之后能明显的促进水稻的生长,其中水稻叶长增加了25.90％,根增长了42.30％,分蘖数增加了79.64％,鲜重增加了166.90％,氮、磷、钾的含量分别增加了61.54％、41.18％和54.05％.因此,从药用稻中筛选到的4株具有高效溶磷解钾能力的内生固氮菌是一类对农业生产有着重要意义的菌株.     

Potassium Dynamics in US Coastal Plain Soils

ABSTRACT

Potassium (K) deficiency in crops in southern US Coastal Plain soils has been documented since the l880s. Long-term soil fertility studies such as Alabama’s “Cullars Rotation” experiment (circa 1911) have been conducted with K since 1911. Other Alabama long-term experiments on several Coastal Plain and related Hapludults, Paleudults, and Kandiudults also contain K variable treatments which have been monitored since 1929. Soil test data from these long-term experiments have allowed us to answer some practical questions regarding K dynamics in Coastal Plain soils. Potassium movement through the soil profile is dependent on the soil’s cation exchange capacity (CEC) but relative accumulation is greater in the plow layer regardless of soil CEC. While subsoil K testing may be useful for identifying situations where subsoil K has been depleted, this extra effort and expense is not necessary for most cropping situations. A crop will remove most of its K from the plow layer if it is present in sufficient quantity based on soil test. Crop depletion of plow-layer K to the point where yield may be reduced is gradual and may take 10–15 years or more depending upon soil CEC and initial soil K concentration. Depletion is most rapid in low CEC soils as would be expected. However, soil test K can vary considerably during the course of a crop season with the lowest soil test K concentrations occurring immediately after harvest.     

Is air-drying of soil samples an appropriate step in determining plant available potassium for corn?

Potassium (K) fertilizer recommendations are mainly based on air -dried soil samples which can lead to over- or under-estimation of plant available soil K. Three on-farm trials were conducted in North Dakota and Minnesota to determine the variation of soil test-K between air-dried (K_Dry) and field moist (K_Moist) soil samples. The differences between K_Dry and K_Moist decreased exponentially as soil K increased, but increased linearly with increasing soil moisture. Soil drying influenced the plant available soil K-test value, producing higher K values compared to the moist soil K. It is unclear based on these initial experiments which method might produce a more predictable K critical value to aid in directing K application for corn in this region.