How do hedgerows influence soil organic carbon stock in livestock‐grazed pasture?

Hedgerows have the potential to influence ecosystem function in livestock‐grazed pasture. Despite this, they are often ignored when quantifying farmland ecosystem service delivery. In this study, we assess the contribution of hedgerows to the ecosystem function of carbon (C) storage, with a particular emphasis on soil organic carbon (SOC). We measured SOC stock (kg C m^?2), on an equivalent soil mass basis, at 0–0.15 m depth in pasture adjacent to 38 hedgerows (biotic) and 16 stone walls or fences (abiotic controls) across ten farms in the county of Conwy, Wales, UK. Pasture SOC stock (~7 kg C m^?2) was similar adjacent to biotic and abiotic field boundaries, positively associated with soil moisture and negatively with soil bulk density (BD). For biotic boundaries, two further variables were significantly associated with SOC stock, distance from hedgerow (decrease in SOC stock) and slope orientation (upslope SOC stock greater than downslope). For pasture adjacent to hedgerows, a model combining the aforementioned variables (BD, soil moisture, distance from hedgerow, slope orientation) explained 78% of variation in SOC stock. This study demonstrates that whilst hedgerows do have subtle positive effects on SOC stock in adjacent pasture, SOC storage adjacent to field boundaries is influenced more by soil moisture content and BD than field boundary type.     

我国主要麦区农户施肥评价及减肥潜力分析

【目的】明确我国主要麦区农户小麦施肥存在的问题及减肥潜力,为科学施肥、合理减肥提供依据。【方法】连续3年对我国主要麦区的小麦种植户进行施肥调研和取样,基于农户产量、养分需求量和土壤养分供应水平对其施肥状况和减肥潜力进行评价和分析。【结果】我国主要麦区农户小麦产量和生物量平均为6.0和13.2 t·hm ^-2,二者极显著线性相关。小麦产量与施肥量和土壤养分无显著相关。我国小麦氮（N）、磷（P₂O₅）和钾（K₂O）肥用量平均分别为191.1、112.8和53.4 kg·hm ^-2,春麦区农户氮、磷和钾肥用量平均分别为171.7、108.9和10.6 kg·hm ^-2,旱作区分别为154.3、111.8和32.6 kg·hm ^-2,麦玉区分别为236.4、128.1和74.0 kg·hm ^-2,稻麦区分别为177.5、77.0和71.8 kg·hm ^-2。就施氮量而言,春麦区过量施氮的农户较少,为34%,其次是麦玉区、稻麦区和旱作区,分别为42%、55%和63%;产量较低的农户是氮肥减施的重点,减氮潜力最高达43.6%,平均需减氮2.3—135.5 kg·hm ^-2。过量施磷问题比较突出,各麦区施磷过量的农户分别占63%、87%、68%和57%,即使小麦高产时,仍有超过50%的农户施磷过量;各麦区不同产量等级的农户均需减施磷肥,减磷量平均为3.8—91.1 kg·hm ^-2,旱作区减磷潜力最大,达55.6%。施钾状况因麦区而异,在春麦区,主要问题是施钾不足,占84%,平均需增施钾肥22.8 kg·hm ^-2;旱作、麦玉和稻麦区,减钾潜力分别达43.2%、25.7%和56.0%;产量较低的农户是减钾的重点,平均需减钾31.7—45.9 kg·hm ^-2。【结论】我国农户施肥状况和减肥潜力因农户产量和麦区不同存在差异,中低产农户过量施肥问题较为严重,应注意根据产量适量减少施用氮、钾肥,所有农户均需警惕磷肥过量投入问题,其中旱作区氮、磷肥减施潜力最高,稻麦区减钾潜力最高。     

水分优化对温室葡萄产量及土壤生物学特性的影响

为揭示滴灌不同水分调控下设施栽培葡萄产量与土壤学特性等相关指标的响应关系,在甘肃省永登县设施葡萄试验基地开展葡萄滴灌不同生育期水分调控田间灌溉试验,分析水分调控对设施栽培葡萄土壤积温、蔗糖酶和淀粉酶活性、有机碳(TOC)、微生物量碳(MBC)和微生物熵(qMB)等土壤学特性的影响,基于隶属函数综合分析明确影响葡萄产量及各项土壤生物学特性指标的最佳水分优化处理。结果表明:新梢期水分胁迫的土壤积温、土壤酶、TOC、MBC、qMB均显著(P <0. 05)高于对照;新梢期水分胁迫较对照可增产44. 6%;果实膨大期作为葡萄生长的关键阶段,此时水分胁迫对土壤淀粉酶影响不显著,但对其他土壤学特性指标具有一定的抑制作用,并且可减产9.7%;隶属函数综合分析表明,土壤生物学特性指标及产量综合隶属排名为:PS﹥FS﹥CS﹥CK﹥ES。     

氮磷减量与液体有机肥配施对膜下滴灌棉田土壤养分的影响

以新疆膜下滴灌棉田为试材,研究氮磷减量与液体有机肥配施对膜下滴灌棉田土壤养分的影响。试验设11个处理:(1)常规施肥(NP);(2)80%常规施肥(80%NP);(3)80%常规施肥+低量氨基酸有机肥(80%NP+LAA);(4)80%常规施肥+中量氨基酸有机肥(80%NP+MAA);(5)80%常规施肥+高量氨基酸有机肥(80%NP+HAA);(6)80%常规施肥+低量黄腐酸有机肥(80%NP+LFA);(7)80%常规施肥+中量黄腐酸有机肥(80%NP+MFA);(8)80%常规施肥+高量黄腐酸有机肥(80%NP+HFA);(9)80%常规施肥+低量沼液有机肥(80%NP+LBS);(10)80%常规施肥+中量沼液有机肥(80%NP+MBS);(11)80%常规施肥+高量沼液有机肥(80%NP+HBS);分别在蕾期、花期、成熟期采集0～20、20～40 cm土层土壤,测定土壤pH值、有机质、氮、磷、钾等有效养分含量。研究结果表明:(1)蕾期时,80%常规施肥配施高量黄腐酸、沼液有机肥显著降低了0～20 cm土层土壤pH值,并对提高土壤速效氮、速效磷含量效果最好。(2)花期时,80%常规施肥配施高量沼液有机肥对提高0～20 cm土层土壤有机质、速效磷含量效果最好。(3)成熟期时,80%常规施肥配施高量沼液有机肥对降低0～20 cm土层土壤pH值、提高土壤有机质含量效果最好。综上所述,新疆滴灌棉田应用80%常规施肥配施高量沼液有机肥效果最好,是新疆滴灌棉田提高土壤肥力和肥料利用率的有效途径。     

基于季节特征的土壤退墒模型建立与率定

利用河南省南阳市2011—2015年12个墒情站的土壤水分监测资料,分析研究了无增墒情况下土壤含水量消退规律,构建出基于不同季节(夏季、春秋季与冬季)的土壤含水量与衰减系数的数学模型,运用规划求解法率定模型参数,并利用2016—2017年资料对模型进行检验。结果表明,不同季节土壤水分衰竭系数模型分别为α=1.023(1-ω~2/4353)~(1/2)(夏季)、α=1.013(1-ω~2/7005)~(1/2)(春秋季)与α=1.008(1-ω~2/9303)~(1/2)(冬季),所建立的数学模型适用于南阳市相应季节壤土与粘壤土小麦、水稻与休闲地土壤旱情预测,但不适用于夏季与春秋季砂土特别是休闲地砂土土壤墒情预测。     

垄畦覆膜种行覆土党参种苗移栽机的设计与试验

针对党参覆膜移栽无机可用的问题,结合西北黄土高原旱区党参垄畦覆膜、种行覆土抗逆栽培模式,设计了一种具有开沟、播苗、起垄、整形、覆膜、种行覆土功能的党参种苗移栽机。对样机关键部件进行了分析与设计,确定了尖角长翼型开沟器、整形镇压、膜上覆土等装置的结构及工作参数,解析了核心部件作业机理。田间试验表明,设计的垄畦覆膜、种行覆土党参种苗移栽机埋苗率为4.1%,露苗率为2.6%,栽植合格率为92.0%,栽植深度合格率为87.5%,膜边覆土厚度合格率为95.9%,膜边覆土宽度合格率为96.3%,生产率约为0.14 hm~2·h~(-1)。田间性能试验指标均达到国家和行业标准要求,试验结果满足设计要求。     

长武塬区苹果园和农田相互转换的深层土壤水环境效应

研究长武塬区苹果园和农田相互转换后0~1 000 cm土壤含水量特征，分析了苹果园土壤干燥化和苹果园转换为农田后土壤水分的恢复效应。结果表明：2、7、17、23、29 a苹果园200~1 000 cm的平均土壤含水量分别为22.8%、21.4%、16.8%、15.4%、14.9%。500~1 000 cm土层中，29 a苹果园平均土壤含水量（14.5%）高于23 a的果园（13.3%）；17~29 a的苹果园均表现为轻度干燥化；基于苹果园和农田转换后土壤水分变化情况估算，苹果园最大种植年限为21 a。苹果园转换为农田1、5、10 a后，农田200~1 000 cm土层土壤含水量分别为：15.3%、15.7%和16.2%，恢复到土壤稳定湿度以上的土层厚度分别为140 cm（1 a）、220 cm（5 a）和400 cm（10 a）。     

Cultivation effects on soil texture and fertility in an arid desert region of northwestern China

In arid desert regions of northwestern China, reclamation and subsequent irrigated cultivation have become effective ways to prevent desertification, expand arable croplands, and develop sustainable agricultural production. Improvement in soil texture and fertility is crucial to high soil quality and stable crop yield. However, knowledge on the long-term effects of the conversion of desert lands into arable croplands is very limited. To address this problem, we conducted this study in an arid desert region of northwestern China to understand the changes in soil physical-chemical properties after 0, 2, 5, 10, 17, and 24 years of cultivation. Our results showed that silt and clay contents at the 17-year-old sites increased 17.5 and 152.3 folds, respectively, compared with that at the 0-year-old sites. The soil aggregate size fraction and its stability exhibited an exponential growth trend with increasing cultivation ages, but no significant change was found for the proportion of soil macroaggregates (>5.00 mm) during the 17 years of cultivation. The soil organic carbon (SOC) content at the 24-year-old sites was 6.86 g/kg and increased 8.8 folds compared with that at the 0-year-old sites. The total (or available) nitrogen, phosphorus, and potassium contents showed significant increasing trends and reached higher values after 17 (or 24) years of cultivation. Changes in soil physical-chemical properties successively experienced slow, rapid, and stable development stages, but some key properties (such as soil aggregate stability and SOC) were still too low to meet the sustainable agricultural production. The results of this long-term study indicated that reasonable agricultural management, such as expanding no-tillage land area, returning straw to the fields, applying organic fertilizer, reducing chemical fertilizer application, and carrying out soil testing for formula fertilization, is urgently needed in arid desert regions.     

Effects of sediment load on the abrasion of soil aggregate and hydraulic parameters in experimental overland flow

The breakdown of soil aggregates under rainfall and their abrasion in overland flow are important processes in water erosion due to the production of more fine and transportable particles and, the subsequent significant effect on the erosion intensity. Currently, little is known about the effects of sediment load on the soil aggregate abrasion and the relationship of this abrasion with some related hydraulic parameters. Here, the potential effects of sediment load on soil aggregate abrasion and hydraulic parameters in overland flow were investigated through a series of experiments in a 3.8-m-long hydraulic flume at the slope gradients of 8.7 and 26.8%, unit flow discharges from 2×10~(–3) to 6×10~(–3) m~2 s~(-1), and the sediment concentration from 0 to 110 kg m~(–3). All the aggregates from Ultisols developed Quaternary red clay, Central China. The results indicated that discharge had the most significant(P0.01) effect on the aggregates abrasion with the contributions of 58.76 and 60.34%, followed by sediment feed rate, with contributions of 39.66 and 34.12% at the slope gradients of 8.7 and 26.8%, respectively. The abrasion degree of aggregates was found to increase as a power function of the sediment concentration. Meanwhile, the flow depth, friction factor, and shear stress increased as a power function along with the increase of sediment concentration at different slope gradients and discharges. Reynolds number was obviously affected by sediment concentration and it decreased as sediment concentration increased. The ratio of the residual weight to the initial weight of soil aggregates(Wr/Wi) was found to increase as the linear function with an increasing flow depth(P=0.008) or Reynolds number(P=0.002) in the sediment-laden flow. The Wr/Wi values followed a power function decrease with increasing friction factor or shear stress in the sediment-laden flow, indicating that friction factor is the best hydraulic parameter for prediction of soil aggregate abrasion under different sediment load conditions. The information regarding the soil aggregate abrasion under various sediment load conditions can facilitate soil process-based erosion modeling.     

松嫩草原盐碱土细菌多样性分析

以松嫩盐碱草原3种不同盐碱程度的盐碱土为材料,应用高通量测序技术,研究了3种不同程度盐碱土壤的细菌群落结构。结果表明:3种盐碱土的理化性质差异显著(P0.05),pH值、碱化度随着盐碱化程度增加而增大,而碱解氮、速效钾和有机质含量随着盐碱化程度增加而降低;3种盐碱土共获得2841个OTU,分属于39个细菌门,其中酸杆菌门、变形菌门等10个菌门是盐碱土中最主要的细菌门类;轻度盐碱土中酸杆菌门占主导地位,相对丰度为32.28%,中度盐碱土中变形菌门占主导地位,相对丰度为19.87%,重度盐碱土中放线菌门占主导地位,相对丰度为22.57%;RDA分析表明,酸杆菌门、硝化螺旋菌门、广古菌门、TM7等的相对丰度与碱解氮、有机质以及速效钾含量呈正相关,疣微菌门的相对丰度与有效磷含量呈正相关,放线菌门、浮霉菌门、拟杆菌门、芽单胞菌门、厚壁菌门的相对丰度与pH值、碱化度呈正相关。