Effect of the addition of Chaetoceros calcitrans,Navicula sp. and Phaeodactylum tricornutum (diatoms) on phytoplankton composition and growth of Litopenaeus vannamei (Boone) postlarvae reared in a biofloc system

The aim of this study was to evaluate the effect of the addition of Chaetoceros calcitrans, Navicula sp. and Phaeodactylum tricornutum (diatoms) on phytoplankton composition and the growth of Litopenaeus vannamei postlarvae reared in a biofloc system . Four treatments were used: BFT (biofloc system without feed and no addition of diatoms); BFT‐F (biofloc system with feed and no addition of diatoms); BFT‐D (biofloc system with the addition of diatoms and no feed); and BFT‐FD (biofloc system with the addition of feed and diatoms), all in triplicate. The shrimp (16 ± 0.02 mg) were stocked at 2500 postlarvae m^?3 and fed a commercial feed. Diatoms were added on the 1st, 5th, 10th and 15th day at a density of 5 × 10⁴ cells mL^?1 for each species. No significant differences (P > 0.05) between treatments were observed for gross primary production, net ecosystem production and water column respiration rate. However, significant differences (P < 0.05) were observed for nitrite, orthophosphate, alkalinity, final weight, weight gain, yield, feed conversion ratio (FCR), phytoplankton and cyanobacteria composition. The BFT‐FD treatment had better performance parameters for final weight (270 mg), weight gain (254 mg), yield (0.67 Kg m^?3) and FCR (0.61), indicating the benefits of the diatoms C. calcitrans, Navicula sp. and P. tricornutum for decreasing cyanobacteria and improving growth of L. vannamei postlarvae reared in biofloc systems.     

氢氧化镁对水质、底质改良的研究与应用

近年,沿海各地区水产养殖业发展迅速。由于内湾海区海水循环交换能力较弱,黑臭底泥的长期堆积,导致养殖水体水质和底质进一步恶化,然而这种问题普遍存在于封闭式或半封闭式水域环境中。对此,氢氧化镁作为水质、底质改良剂被应用于水环境的治理。本文概述了氢氧化镁的作用机理,包括氢氧化镁与悬浮颗粒物的静电、对氮磷的降解及对硫化氢的降解等作用;同时介绍了氢氧化镁在海水养殖场、淡水湖泊和水库、水华防控、赤潮防控及废水处理中的研究与应用;展望了氢氧化镁和纳米级氢氧化镁在水体环境领域的应用前景。     

基于UHPLC-Q-TOF/MS的不同产地普洱生茶化学成分差异研究

为了更加全面地了解产地对普洱生茶品质与化学成分的影响,本研究选取来自临沧市、普洱市、西双版纳州三大产区12个茶山(自然村)的普洱生茶样品,采用超高效液相色谱-四级杆-飞行时间质谱(UHPLC-Q-TOF/MS)对不同产地普洱生茶的非挥发性代谢物表型进行了研究。结果表明:不同产地普洱生茶的化学成分在含量上具有较大差异,且具有明显的产地特征。采用主成分分析,可以对来自西双版纳自治州(包括勐腊县、勐海县、景洪市)、普洱市、临沧市3个地级行政区的普洱生茶进行有效区分,也可以对来自普洱茶产区的东南、西南、西北3个区域的普洱生茶进行有效区分。进一步鉴定了普洱生茶中79种主要成分,并对其在12个茶山(自然村)的普洱生茶中的含量分布,以及与不同产地普洱生茶滋味品质的关系进行了分析。本研究表明,基于UHPLC-Q-TOF/MS的茶叶非挥发性化学成分轮廓可以作为普洱生茶产地判别的依据。     

Soil water response to precipitation in different microtopographies on the semi-arid Loess Plateau,China

Soil water is an important factor restricting afforestation on the semi-arid Loess Plateau.The microtopography of the loess slope has changed the distribution pattern of soil water on the slope.To improve water utilization efficiency and optimize afforestation configuration patterns,the relationship between soil water and precipitation at micro-topographic scale must be studied.We used time series analysis to study the temporal variation of soil water and its response to precipitation in four kinds of micro-topographies and undisturbed slope on loess slopes.Micro-topographies significantly influenced soil water distribution and dynamics on the slopes.Soil water stored in the platform,sinkhole,and ephemeral gully influenced subsequent soil water for 4 weeks,whereas soil water stored in the scarp and undisturbed slope could influence soil water for 2 weeks.It took 12 weeks,10 weeks,18 weeks,6 weeks,and 12 weeks for precipitation to reach the deeper soil layer in the platform,sinkhole,scarp,ephemeral gully,and undisturbed slope,respectively.These soil water characteristics in different micro-topographies are vital factors that should be taken into consideration when undertaking afforestation on the Loess Plateau.     

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。     

浑善达克沙地杨树水分利用特征

为探究浑善达克沙地杨树的水分利用特征。本文利用氢和氧同位素示踪技术,测定了降雨、土壤水与地下水的δ18O值,利用多元线性混合模型定量计算了杨树对不同土层土壤水分的利用比例。结果表明:①浑善达克沙地大气降雨方程线为:δDLWML=7.84δ^18OLWML+9.12,斜率比全国降雨方程偏小,体现了研究区降雨少,蒸发大的气候特征;②土壤含水量与地下水位埋深、降雨量、植物生长期的变化有着显著的相关关系。降雨量较大与地下水位埋深较浅的时期,土壤含水量明显增大,在植物生长前期和中期,土壤含水量明显较低;③杨树在雨季,利用了大量的浅层土壤水(0~40 cm),在较为干旱的旱季,利用了大量的深层土壤(160~200 cm)水与少量的地下水。     

幼龄期压砂地枸杞产量和品质多指标耦合灌溉制度优化

为提高宁夏中部干旱带幼龄期压砂地枸杞灌水效率,保障枸杞产量和品质,进行了3水平灌水定额(300、225 m~3·hm~(-2)和150 m~3·hm~(-2))的田间对比试验,采用综合指标增量最优方法对灌溉制度进行了优化。研究发现:枸杞5月上旬萌芽期耗水以土壤蒸发为主,日耗水量0.6～1.2 mm,6月中旬进入夏果花期耗水量增大,日耗水量2.5～3.7 mm,7月中旬枸杞夏果期耗水量继续增大,达2.4～4.3 mm,7月下旬日耗水量最大,为3.2～4.7 mm,8月中旬耗水量下降,日耗水量3.0～4.2 mm。灌水定额对枸杞产量影响显著(P0.05),灌水定额300 m~3·hm~(-2)时产量最高,为1 402.65 kg·hm~(-2);灌水定额225 m~3·hm~(-2)时枸杞多糖、β-胡萝卜素和黄酮较高,含量分别为4.56%、0.15%和0.41%;灌水定额150 m~3·hm~(-2)时枸杞甜菜碱含量较高,为0.77%。进一步通过综合指标增量最优方法进行优化,结果表明β-胡萝卜素含量最高时得到综合指标增量最大,为-5.4%,总耗水量为450 mm。枸杞夏果花期进入需水关键期,阶段耗水量达70 mm以上,进入6月中旬枸杞需水量增大,旬耗水量达29 mm以上。可见,幼龄期压砂地枸杞产量及品质指标均达到最优的耗水量较难获得,但是在β-胡萝卜素含量最高时可以获得产量和品质多指标耦合的最优耗水量,据此进行灌溉制度优化,可以一定程度上实现幼龄期压砂地枸杞优质高产。     

基于Google Earth Engine平台的关中冬小麦面积时空变化监测

以关中地区为研究区,基于Google Earth Engine(GEE)平台,根据冬小麦生育期内归一化植被指数(NDVI)时序曲线和物候特征,采用NDVI重构增幅算法和光谱突变斜率,构建了关中地区冬小麦提取模型并实现了冬小麦种植面积的提取。用农业统计面积验证提取结果表明:在市级和县级尺度上,决定系数R~2分别为0.82和0.62,一致性指标d分别为0.95和0.84,提取结果与实地调查数据的空间一致性精度为93.4%。结果显示:关中地区冬小麦主要分布在中部关中平原,冬小麦种植面积在2011—2017年呈下降趋势,减少了83.22×10~3 hm~2(8.47%)。综合考虑冬小麦NDVI时序曲线的"峰""谷"特征,具有一定的普适性,可为大面积连续年份冬小麦种植面积时空监测提供参考。     

基于主成分分析和Copula函数的灌溉水利用系数影响因素研究

以新疆生产建设兵团第十二师中型灌区为研究对象，采用首尾法测算2018年和2019年4个样点灌区的灌溉水利用系数，在采用主成分分析法对指标体系降维处理的基础上，用Copula函数构建PCA-Copula评价分析方法，对灌溉水利用系数各影响因素的影响程度和影响规律进行计算分析。结果表明：两年测算数据表明，4个样点灌区灌溉水利用系数都在0.63以上，且最大值达到0.668，分别高于同期全疆、全国平均水平5.05%、10.15%；主成分分析得出，渠道衬砌率（0.944）、滴灌灌溉面积比（0.746）、作物需水量（0.635）、实际灌溉面积（0.734）等都具有超过60%的正贡献率，而葡萄种植比（-0.586）和灌区毛灌溉用水量（-0.645）等具有超过58%的负贡献率。利用PCA-Copula分析评估方法得出，作物种植比例和节水灌溉工程状况对十二师中型灌区灌溉水有效利用系数影响显著（P<0.05），其中葡萄净灌溉定额和灌区毛灌溉用水量对灌溉水有效利用系数的影响极其显著（P<0.01），相关系数分别为0.875、0.742，同时利用Spearman等级相关系数检验法和线型回归来检验PCA-Copula评价法与熵值法的密切程度，检验结果其相关系数分别为 0.87（P＜0.05）和0. 52（P＜0.001），表明PCA-Copula评价方法适用于研究灌溉水利用系数影响因素。     

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.