橡胶园土壤全氮和速效钾养分合理取样位置研究

通过地统计学方法分析了土壤全氮和速效钾空间变异特征,并对其合理取样位置进行探讨,绘制了兼顾土壤全氮和速效钾综合养分的合理取样位置空间分布图.结果表明:橡胶园土壤全氮和速效钾综合养分合理取样位置主要受土壤速效钾含量分布决定;在空间分布上,综合养分的合理取样位置主要位于远离施肥穴的橡胶树行间萌生带和中间树头附近区域.此结果为南方长期经济作物土壤样品取样位置的确定提供一种新的尝试.     

邵阳市植烟土壤速效钾含量分布特征研究

为了解邵阳市植烟土壤速效钾含量分布状况,测试了邵阳市1790个土壤样本的速效钾含量,采用经典统计学和地统计学方法分析了邵阳市植烟土壤速效钾含量及在县域、空间、pH组、有机质组的分布。结果表明：①邵阳市植烟土壤速效钾含量总体上处于偏低水平,平均值为113.75 mg/kg,变异系数为50.40%,处于适宜范围内的样本占12.01%;于邵阳县和新宁县植烟土壤速效钾含量极显著高于隆回县;③植烟土壤速效钾含量总体上呈斑块状分布态势,以植烟土壤速效钾含量100.00~130.00 mg/kg为主要分布面积;榆不同pH组的植烟土壤速效钾含量差异不显著;虞植烟土壤有机质含量在35 g/kg以下时,土壤速效钾含量有随有机质增加而增加的趋势;植烟土壤有机质含量在35 g/kg以上时,土壤速效钾含量有随有机质增加而减少的趋势。     

湘西植烟土壤有效铁含量及变化规律研究

为探明湘西州植烟土壤有效铁含量的分布状况,检测了湘西州主要烟区488个土壤样本的有效铁含量,并采用传统统计学和地统计学方法分析了湘西州植烟土壤有效铁含量适宜样本分布、县域差异、土壤类型差异、海拔高度差异及空间分布。结果表明：①湘西州植烟土壤有效铁含量总体水平高,平均值83.20 mg/kg,变幅10.04～328.89 mg/kg,变异系数82.31%。②不同县之间的植烟土壤有效铁含量差异不显著,从大到小依次为：泸溪县、凤凰县、花垣县、古丈县、永顺县、龙山县、保靖县。③不同土壤类型土壤有效铁含量差异极显著,从高到低依次为：红灰土、石灰土、红壤、黄壤、水稻土、黄棕壤。④不同海拔高度的植烟土壤有效铁含量差异不显著,5个海拔高度组的植烟土壤有效铁含量平均为62.00～192.00 mg/kg。⑤植烟土壤有效铁含量Kriging插值图显示,湘西州植烟土壤有效铁含量总体上呈斑块状分布态势,以有效铁含量89.9～184.0 mg/kg为主要分布面积,主要分布在湘西州的南部和北部地区。     

西瓜根系分泌酸性磷酸酶对有机肥营养的响应

有机肥营养对西瓜品质具有提升效果,但根系对有机肥中养分的吸收机制尚不完全清楚,尤其对磷素的利用机制。本研究关注西瓜根系分泌酸性磷酸酶活性对有机肥施用的响应。采用模拟西瓜根系分泌物的方法研究有机酸对有机肥中可溶性全磷和有效磷含量的影响;采用砂培的方法,研究有机肥中的磷替代化肥磷时西瓜根系分泌酸性磷酸酶活性的响应;采用田间试验研究有机肥替代化肥以及有机肥不同施用量对西瓜根际酸性磷酸酶活性、西瓜磷营养、产量和品质的影响。结果表明,有机肥中水浸提可溶性全磷含量为6.9 g?kg~(-1),可溶性无机磷含量为525.1 mg?kg~(-1),可溶性全磷中无机磷占7.6%,有机磷占92.4%,可溶性有机磷需经过水解后才能被根系吸收。有机肥中磷替代化肥磷时,西瓜根系和根际土壤酸性磷酸酶活性均显著提高,西瓜茎、叶中磷含量提高。施用三倍有机肥时西瓜根际土壤有效磷含量和西瓜产量提高。因此,有机肥中磷替代化肥磷时,西瓜通过提高根系分泌酸性磷酸酶的活性而提高利用有机磷的能力。     

城市不同功能分区草坪绿地土壤有机碳与碱解氮垂直分布特征

为了解城市草坪绿地土壤有机碳与碱解氮垂直分布特征,以长春市为例,选取不同功能分区(公园、道路、居住区、校园)草坪土壤为研究对象,分析了土壤pH值、有机碳(SOC)、碱解氮(AN)的垂直分布特征及相关性。结果表明:草坪绿地类型与土壤剖面对土壤pH值、有机碳(SOC)、碱解氮(AN)含量影响显著(P<0.05)。其中,不同功能区0～30 cm土壤pH值为:校园绿地>道路绿地>居住区绿地>公园绿地;不同功能区0～30 cm土壤SOC含量为:公园绿地>居住区绿地>校园绿地>道路绿地;不同功能区0～30 cm土壤AN含量为:公园绿地>居住区绿地>校区绿地>道路绿地。相关性分析表明:土壤SOC与AN呈正相关,而绿地土壤的pH值与SOC含量呈负相关。由此结论我们可以通过增加土壤中碱解氮含量,调节土壤pH值,来使土壤得到优化,增加固碳能力,减弱温室效应,改善生态环境。     

Soil chemical properties and microbial biomass after 16 years of no-tillage farming on the Loess Plateau, China

Data from a 16-year field experiment conducted in Shanxi, on the Chinese Loess Plateau, were used to compare the long-term effects of no-tillage with straw cover (NTSC) and traditional tillage with straw removal (TTSR) in a winter wheat (Triticum aestivum L.) monoculture. Long-term no-tillage with straw cover increased SOM by 21.7% and TN by 51.0% at 0–10 cm depth and available P by 97.3% at 0–5 cm depth compared to traditional tillage. Soil microbial biomass C and N increased by 135.3% and 104.4% with NTSC compared to TTSR for 0–10 cm depth, respectively. Under NTSC, the metabolic quotient (CO₂ evolved per unit of MBC) decreased by 45.1% on average in the top 10 cm soil layer, which suggests that TTSR produced a microbial pool that was more metabolically active than under NTSC. Consequently, winter wheat yield was about 15.5% higher under NTSC than under TTSR. The data collected from our 16-year experiment show that NTSC is a more sustainable farming system which can improve soil chemical properties, microbial biomass and activity, and thus increase crop yield in the rainfed dryland farming areas of northern China. The soil processes responsible for the improved yields and soil quality, in particular soil organic matter, require further research.     

Spatial variability in soil heat flux at three Inner Mongolia steppe ecosystems

Closing the energy budget at flux measurement sites is problematic, even when the fetch extends over flat, homogeneous surfaces with low vegetation cover. We used the residual energy balance and ordinary least square (OLS) linear regression methods to quantify spatial variability in soil heat flux contributing to energy balance closure (EBC), by deploying a mobile energy system within the footprints of three Eddy-covariance towers located in the steppe of Inner Mongolia, China. The EBC at the study sites had a daily average residual of 8–19 W m⁻² with OLS slopes of 0.83–0.96. The EBC was better achieved at the wet site than at the dry site. The spatial variability in soil heat flux was 48 W m⁻² (13% of R_n) during the day and 15 W m⁻² (34%) at night, with an average of 29 W m⁻² (24%) across the three sites. A 9% OLS slope difference due to this variability was recorded from our eight plot measurements. A large amount of missing energy (110 W m⁻² at peak) could occur with decreasing OLS slope of 23% across the three grassland sites when soil heat flux is not taken into account. In particular, heat storage in the top soil layer not only influenced the magnitude of EBC, but also adjusted soil heat flux to match the ‘truth schedule’. Heat storage in the top soil layer comprised half of the soil heat flux when the heat flux plate was deployed at a depth of 30 mm. If this part of heat storage was neglected, the residual of EBC would increase as large as 60 W m⁻² with OLS slope decreasing 9%. Comparing them with the multiple-location soil heat flux measurements, the single-location measurements from near the Eddy-covariance towers obtained a slightly better EBC with the OLS slope increasing by 4%.     

Soil compaction and forest floor removal reduced microbial biomass and enzyme activities in a boreal aspen forest soil

Soil enzymes are linked to microbial functions and nutrient cycling in forest ecosystems and are considered sensitive to soil disturbances. We investigated the effects of severe soil compaction and whole-tree harvesting plus forest floor removal (referred to as FFR below, compared with stem-only harvesting) on available N, microbial biomass C (MBC), microbial biomass N (MBN), and microbial biomass P (MBP), and dehydrogenase, protease, and phosphatase activities in the forest floor and 0–10 cm mineral soil in a boreal aspen (Populus tremuloides Michx.) forest soil near Dawson Creek, British Columbia, Canada. In the forest floor, no soil compaction effects were observed for any of the soil microbial or enzyme activity parameters measured. In the mineral soil, compaction reduced available N, MBP, and acid phosphatase by 53, 47, and 48%, respectively, when forest floor was intact, and protease and alkaline phosphatase activities by 28 and 27%, respectively, regardless of FFR. Forest floor removal reduced available P, MBC, MBN, and protease and alkaline phosphatase activities by 38, 46, 49, 25, and 45%, respectively, regardless of soil compaction, and available N, MBP, and acid phosphatase activity by 52, 50, and 39%, respectively, in the noncompacted soil. Neither soil compaction nor FFR affected dehydrogenase activities. Reductions in microbial biomass and protease and phosphatase activities after compaction and FFR likely led to the reduced N and P availabilities in the soil. Our results indicate that microbial biomass and enzyme activities were sensitive to soil compaction and FFR and that such disturbances had negative consequences for forest soil N and P cycling and fertility.     

放牧强度对高寒混播草地土壤养分含量的影响

垂穗披碱草/星星草混播草地三个放牧季的牦牛放牧试验结果表明:①放牧强度和土壤层深度对有机质含量的影响均达到极显著的水平(P<0.01),且土壤有机质含量随放牧强度的增加呈下降趋势;②放牧强度对土壤速效氮和速效磷的影响不显著(P>0.05),对速效钾的影响显著(P<0.05);不同土壤层速效氮和速效钾含量之间的差异显著(P<0.05),速效磷含量之间的差异不显著(P>0.05)。     

电感耦合等离子体原子发射光谱(ICP-AES)测定土壤中有效硅

利用ICP-AES测定土壤中有效硅含量,经分析可得出ICP-AES测得的数据在精确度和准确度上均能满足实验的要求;说明ICP-AES可以作为一种快速、简捷的测试手段。