基于GlobeLand 30的哈密市2000-2020年土地利用格局变化研究

[目的]研究新疆维吾尔自治区哈密市近20 a的土地利用变化,为该地区土地利用规划及生态环境保护提供有力支撑。[方法]基于2000,2010,2020年的GlobeLand 30数据集,通过利用转移矩阵、坡度分布指数、标准差椭圆以及土地利用重心迁移,分析哈密市2000-2020年土地利用的时空变化特征。[结果]①哈密市2000-2020年土地利用变化比较明显。2020年各土地利用类型面积比例为:未利用地>草地>耕地>林地>建设用地>水域。哈密市虽然面积大但能利用的绿洲面积较小。2020年草地面积为10226.39 km²,水域面积为295.17 km²。2000-2020年土地利用类型变化量中,草地的减少量最大,流失面积为671.48 km²,主要转换成未利用地、林地和少量耕地;建设用地增量最大,面积高达405.60 km²。2000-2020年其他土地利用类型中林地和耕地面积呈增长趋势;未利用地和水域呈减少趋势,其中水域面积的减少量很小,基本保持稳定。②2000-2020年草地在5个坡度梯度上分布比较均匀;而耕地和建设用地基本分布在Ⅰ级和Ⅱ级坡度梯度,耕地在Ⅰ级坡度梯度上显优势分布;林地在Ⅰ级坡度梯度上面积最大;未利用地分布面积随着坡度梯度的增加而减少。③2010-2020年土地利用变化与2000-2010时段的变化相比方向性较明显,范围更广,重心向西北方向迁移。[结论]2000-2020年哈密市的土地利用变化有着明显的时空特征,坡度对各地类分布的影响较为明显。     

2020年通辽市开鲁县气候影响评价

本文采用统计分析方法，对2020年开鲁县国家基准气候站采集的气温、降水、日照等基本气象要素数据和相应历年值进行对比分析，并对局地大风、暴雪等重大灾害性天气进行综合分析，并根据分析结果，作出气候对生产生活影响的综合评价。结果表明，2020年气候条件对全县农业生产及人们的生活有利有弊。     

Performance evaluation of venturi aeration system

The venturi aeration is an effective practice to increase the dissolved oxygen accessibility in the water bodies. This study aims to optimize the various geometrical parameters of the venturi aeration system. A non-dimensional technique was applied to find the optimum performance of various geometric parameters i.e. throat lengths (t_l), number of air holes (N), and converging and diverging angles (α and β). These experiments have been carried out using 1124 L capacity of tank having dimensions of 105 cm long, 105 cm wide and 102 cm deep. The experiments were conducted at a constant flow velocity of water (1.096 m/s) with varying throat length (t_l = 20–100 mm keeping 20 mm as interval between two consecutive length), number of air holes (N = 1–17 at an equal hole to hole distance of 5 mm between them), and converging and diverging angles (α and β = 10°, 15°, 20° and 25°). Multiple non-linear regression equations were also developed from the linear relation with the dependent variable (Non-dimensional form of standard aeration efficiency, NDSAE) and independent variables (t_l and N). With the geometrically optimized venturi aerator the optimum performance was found for t_l =100 mm, N = 17, and α and β = 15°. The maximum value of standard oxygen transfer rate (SOTR) and standard aeration efficiency (SAE) obtained was 0.0216 kgO₂/h and 0.611 kgO₂/kWh respectively. From the non-dimensional study, it was found that the NDSAE is the function Reynolds number (Re) and Froude number (Fr). The simulation equations were developed on the basis of Re and Fr for NDSAE, and subjected to 7.378 × 10⁻⁶ < Re < 3.689 × 10^-5 and 0.163 < Fr < 0.817, respectively.     

岩溶流域典型农业区水体氢氧同位素的空间异质性及形成机制

分别于平水期和枯水期采集了花溪河流域典型农业区地表水和地下水样品。利用氢氧同位素示踪技术,结合土地利用类型对研究区不同水体的补给来源、季节变化及主要影响过程进行了分析,并对不同水体氢氧同位素值进行了空间插值分析,同时对其形成机制进行了分析,阐明了不同土地利用类型影响下的主要水文过程。结果表明:(1)研究区不同水体的主要补给来源为当地大气降水,月亮湖水库受蒸发作用影响明显,地表水和地下水的δD和δ~(18)O整体上呈现平水期高于枯水期的特征。(2)地下水的δD和δ~(18)O在枯水期与平水期均呈现明显的空间分异性特征,西部水田/水库集中区富集,东部旱地集中区贫化,土地利用对研究区环境水文过程影响明显。该研究结果有助于了解不同土地利用方式下地表水对地下水的影响,为流域管理提供科学依据。     

Glacier mass balance in High Mountain Asia inferred from a GRACE release-6 gravity solution for the period 2002–2016

We provide estimates of glacier mass changes in the High Mountain Asia (HMA) area from April2002 to August 2016 by employing a new version of gravity solutions of the Gravity Recovery and ClimateExperiment (GRACE) twin-satellite mission. We find a total mass loss trend of the HMA glaciers at a rateof –22.17 (±1.96) Gt/a. The largest mass loss rates of –7.02 (±0.94) and –6.73 (±0.78) Gt/a are found forthe glaciers in Nyainqentanglha Mountains and Eastern Himalayas, respectively. Although most glaciers inthe HMA area show a mass loss, we find a small glacier mass gain of 1.19 (±0.55) and 0.77 (±0.37) Gt/a inKarakoram Mountains and Western Kunlun Mountains, respectively. There is also a nearly zero massbalance in Pamirs. Our estimates of glacier mass change trends confirm previous results from the analysisof altimetry data of the ICESat (ICE, Cloud and Land Elevation Satellite) and ASTER (AdvancedSpaceborne Thermal Emission and Reflection Radiometer) DEM (Digital Elevation Model) satellites inmost of the selected glacier areas. However, they largely differ to previous GRACE-based studies which weattribute to our different post-processing techniques of the newer GRACE data. In addition, we explicitlyshow regional mass change features for both the interannual glacier mass changes and the 14-a averagedseasonal glacier mass changes. These changes can be explained in parts by total net precipitation (netsnowfall and net rainfall) and net snowfall, but mostly by total net radiation energy when compared to datafrom the ERA5-Land meteorological reanalysis. Moreover, nearly all the non-trend interannual masschanges and most seasonal mass changes can be explained by the total net radiation energy data. The massloss trends could be partly related to a heat effect due to increased net rainfall in Tianshan Mountains, QilianMountains, Nyainqentanglha Mountains and Eastern Himalayas. Our new results for the glacier mass changein this study could help improve the understanding of glacier variation in the HMA area and contribute tothe study of global change. They could also serve the utilization of water resources there and in neighboringareas.     

水肥调控对滴灌马铃薯生长、品质及水肥利用的影响

研究生育期土壤水分下限调控和施肥对陕北榆林地区滴灌马铃薯生长、品质和水肥利用的影响,以期探寻马铃薯优质高产的水肥调控模式。以马铃薯紫花白为材料,分别在苗期、块茎形成期、块茎膨大期、淀粉积累期、成熟期设置3个土壤水分调控下限水平:W1(55%、60%、65%、55%、55%)、W2(65%、70%、75%、65%、65%)、W3(75%、80%、85%、75%、75%),4个施肥水平N-P_2O_5-K_2O (kg·hm~(-2))分别为F1(100-40-150 kg·hm~(-2))、F2(150-60-225 kg·hm~(-2))、F3(200-80-300 kg·hm~(-2))、F4(250-100-375 kg·hm~(-2)),共12个处理,在生育期内对马铃薯生长、产量及品质等指标进行观测,分析马铃薯各指标对水肥的响应机制。结果表明:(1)在同一施肥水平下,W2灌水处理的马铃薯生长、产量、品质、水肥利用效率(WUE)均显著高于W1和W3处理。W2处理的平均产量为43 187.15 kg·hm~(-2),比W1和W3分别增加了24.59%和5.26%,淀粉和维生素C含量分别增加了15.32%和6.37%,8.04%和4.66%,WUE分别增加了15.53%和7.54%,肥料偏生产力(PFP)分别增加了21.65%和4.41%。(2)在同一灌水水平下,F3施肥处理的马铃薯生长、产量、WUE均显著高于F1、F2和F4处理,淀粉含量和维生素C含量在F2处理最高。F3处理的平均产量为44 691.32 kg·hm~(-2),比F1、F2和F4处理分别增加了41.79%、10.98%和6.34%。WUE随施肥量的增加均呈抛物线变化趋势,PFP随施肥量增加呈减小趋势,F1处理的PFP平均为108.69 kg·kg~(-1),比F2、F3和F4处理分别显著增加了17.41%、41.06%和87.50%。(3)运用主成分分析法评价马铃薯品质表明,F3W2处理排名第一,是榆林地区马铃薯优质高产的最优水肥组合。     

Change features of time-series climate variables from 1962 to 2016 in Inner Mongolia,China

Detecting change features of climate variables in arid/semi-arid areas is essential for understanding related climate change patterns and the driving and evolution mechanism between climate and arid/semi-arid ecosystems.This paper takes Inner Mongolia of China,a unique arid/semi-arid ecosystem,as the study area.We first detected trend features of climate variables using the linear trend analysis method and then detected their trend-shift features using the breaks for additive seasonal and trend method based on the time-series of monthly precipitation and monthly mean temperature datasets from 1962 to 2016.We analyzed the different change features of precipitation and temperature on a regional scale and in different ecological zones to discover the spatial heterogeneity of change features.The results showed that Inner Mongolia has become warmer-wetter during the past 54 years.The regional annual mean temperature increased 0.4°C per decade with a change rate of 56.2%.The regional annual precipitation increased 0.07 mm per decade with a slightly change rate of about 1.7%,but the trend was not statistically significant.The warmer trend was contributed by the same positive trend in each season,while the wetter trend was contributed by the negative trend of the summer precipitation and the positive trend of the other three seasons.The regional monthly precipitation series had a trend-shift pattern with a structural breakpoint in the year 1999,while the regional monthly mean temperature series showed an increasing trend without a periodical trend-shift.After the year 2000,the warmer-wetter trend of the climate in Inner Mongolia was accelerated.The late 20th century was a key period,because the acceleration of the wetter trend in some local zones(I and II)and the alleviation of the warmer trend in some local zones(Ⅶ,Ⅷand IX)occurred simultaneously.Moreover,the change features had a strong spatial heterogeneity,the southeastern and southwestern of Inner Mongolia went through a warmer-drier trend compared with the other areas.The spatio-temporal heterogeneity of the climate change features is a necessary background for various types of research,such as regional climate change,the evolution of arid/semi-arid ecosystems,and the interaction mechanisms between climate and arid/semi-arid ecosystems based on earth-system models in Inner Mongolia.     

不同氮效率型苜蓿氮素吸收差异与根系形态的关系及其对氮的响应

以高效型苜蓿（‘龙牧806’‘肇东苜蓿’）和低效型苜蓿（‘公农1号’‘陇东苜蓿’）为试验材料，采用营养液砂培法，在4个供氮量下（2.1，21，210和420 mg·L^-1），研究紫花苜蓿苗期氮素吸收、分配的氮效率型差异及其与根系形态之间的关系。结果表明高效型苜蓿品种的株高、地上生物量、根重、总根长和根体积均显著高于低效型品种（P<0.05）；供氮量较低时（2.1和21 mg·L^-1），高效型向根系分配了较大比例的氮素，而低效型则向地上部分配了较大比例的氮素，根系形态参数与总氮量呈显著正相关（P<0.05），且根重对氮素吸收的直接作用较大，直接通径系数是1.230和1.102。因此，在氮胁迫下，根系形态对氮吸收效率起重要作用，尤其是根系形态中的根重对其影响较大。     

Screening and identification of soybean varieties with high phosphorus efficiency at seedling stage

In order to simplify the workload and find a reliable method for screening soybeans with different phosphorus(P)efficiencies,47 soybean varieties were screened from 90 varieties according to yield under normal phosphorus,and 10 indicators including root phenotype,phosphorus utilization efficiency at the seedling stage and yield were measured.Through single-index cluster analysis,the performance value and relative value of the abovementioned indexes under low-phosphorus conditions were analyzed,and then,the combined indexes were analyzed by principal components method.The membership function method and the cluster analysis method was used to calculate and analyze the comprehensive score value.Three indexes of root P utilization efficiency(X₁),relative value of root P utilization efficiency(X₂),and root volume(X₃)under low P at the seedling stage were selected as the most consistent with the yield screening results under low P condition,and the mathematical model of the comprehensive score value was obtained:D=1.218X₁t 0.320X₂t 0.007X₃-0.664(P=0.000,R²=1.000).The comprehensive score can screen and identify the P efficiency of soybeans with fewer indexes in the early growth stages,which provides a more rapid and reliable mathematical model for screening and identifying a larger number of germplasm resources for P efficiency.     

不同氮效率油菜种质苗期氮吸收转运与利用差异研究

氮效率研究是油菜营养性状遗传改良的前提,为探究不同氮效率油菜种质苗期氮吸收、转运和利用的异同,以2个氮效率差异油菜种质H6（氮高效）和L18（氮低效）为供试材料,利用水培营养液设置正常氮（CK）和低氮（LN）2个氮浓度处理,培养14d后检测植株氮含量,计算氮累积量、氮转运系数和氮利用效率。结果显示,不同氮浓度处理对油菜苗期氮的吸收、转运和利用效率影响的差异达到极显著水平（P＜0.01）。与CK相比,LN处理的油菜生物量、氮含量和氮累积量均显著降低,而氮利用效率和根冠比显著提高;氮高效油菜种质H6的生物量、氮累积量、氮转运系数和氮生理利用效率均显著大于氮低效种质L18,分别为L18的2.07、1.42、3.23和1.56倍。从氮的吸收、转运和利用3个方面探讨了低氮胁迫处理下油菜种质苗期氮效率差异的原因,对深入开展油菜氮高效机理研究及油菜品种氮效率改良具有一定的指导意义。