Geological characteristics and accumulation mechanisms of the "continuous" tight gas reservoirs of the Xu2 Member in the middle-south transition region,Sichuan Basin,China

＂Continuous＂ tight gas reservoirs are those reservoirs which develop in widespread tight sandstones with a continuous distribution of natural gas. In this paper, we summarize the geological features of the source rocks and ＂＇continuous＂ tight gas reservoirs in the Xujiahe Formation of the middle- south transition region, Sichuan Basin. The source rocks of the Xul Member and reservoir rocks of the Xu2 Member are thick （Xul Member： 40 m, Xu2 Member： 120 m） and are distributed continuously in this study area. The results of drilled wells show that the widespread sandstone reservoirs of the Xu2 Member are charged with natural gas. Therefore, the natural gas reservoirs of the Xu2 Member in the middle-south transition region are ＂continuous＂ tight gas reservoirs. The accumulation of ＂continuous＂ tight gas reservoirs is controlled by an adequate driving force of the pressure differences between source rocks and reservoirs, which is demonstrated by a ＂one-dimensional＂ physical simulation experiment. In this simulation, the natural gas of＂continuous＂ tight gas reservoirs moves tbrward with no preferential petroleum migration pathways （PPMP）, and the natural gas saturation of＂continuous＂ tight gas reservoirs is higher than that of conventional reservoirs.

Soil Erosion Spatial Distribution Character of Sloping Field in the Sichuan Hilly Basin:Taking a Cultivated Slope in Neijiang as Example

^137Cs nuclear tracing technique was used to estimate rates of soil redistribution on a sloping field with traditional erosion control measures located near Shangqiao Village, Neijiang City, in the Sichuan Hilly Basin of China. The downslope changes of ^137 Cs inventory and its corresponding soil erosion rates in the sloping field show a rolling trend and have two peak values in two inflexions of the sloping field, these result reflects that the changes of microphysiognomy play a key role on the spatial soil redistribution of the sloping field.

Effects of Land Use Change on Eco-environment in Hilly Area of Central Sichuan Basin——A Case Study of Yanting County, Sichuan Province

With the artificial alder and cypress mixed forest being planted, there has been a marked land use change since 1970s' in Hilly Area of Central Sichuan Basin, China. Data from meteorological observations or posts operated over long time, measurement and calculation of NPP (net primary production) and biomass of biological community, and analysis of soil organic matter content show that the artificial alder and cypress mixed forest has outstanding eco-environmental effect: adjusting local climate, raising soil fertility, alleviating menace of drought, and raising NPP and biomass of biological community. It is very beneficial for improving ecological environment to afforest artificial alder and cypress mixed forest in populous Hilly Area of Central Sichuan Basin, China. Key Words: land use/land cover change (LUCC); eco-environmental effect; Hilly Area of Central Sichuan Basin; the artificial alder and cypress mixed forest

Tectonic paleogeography of Late Sinian and its significances for petroleum exploration in the middle-upper Yangtze region, South China

The paleotectonic pattern,lithofacies paleogeographic features,sedimentary evolution and its controlling effects on hydrocarbon accumulation assemblages during the depositional period of the Sinian Dengying Formation in middle-upper Yangtze region were investigated based on outcrops,drilling,log and seismic data.The study shows that,(1)Affected by the breakup of the Rodinia supercontinent,the middle and upper Yangtze areas were in extensional tectonic environment during the depositional period of Dengying Formation.The carbonate platform was structurally differentiated.Intra-platform depressions controlled by syndepositional faults developed,forming a tectonic-paleogeographic pattern of"three platforms with two depressions".(2)During the depositional period of the first and second members of the Dengying Formation,rimmed platforms and intra-platform fault depressions developed in upper Yangtze area and isolated platform developed in middle Yangtze area,and there was the Xuanhan-Kaijiang ancient land block in eastern Sichuan.The depositional period of the third member of the Dengying Formation is the transformation period of tectonic-paleogeographic pattern,when a set of shallow water shelf sediment rich in mud was deposited due to transgression on the background of the eroded terrain formed in EpisodeⅠof Tongwan Movement.The sediment of the fourth member of the Dengying Formation inherited the paleogeographic pattern of the first and second members of the Dengying Formation in general,but the Deyang-Anyue intra-platform fault depression further expanded,and the middle Yangtze platform evolved into two separated platforms.(3)Tectonic-sedimentary differentiation and evolution of carbonate platform in the Sinian gave rise to two types of accumulation assemblages with wide distribution and great exploration potential,which are platform margin and intra-platform.

中国西南地区CCUS区域中心建设路径与政策建议

西南地区正在加快推动成渝地区双城经济圈和国家天然气(页岩气)千亿立方米产能基地等国家战略实施,面临能源消费量增长硬需求和碳减排硬约束之间的矛盾,推动CCUS产业发展是解决该问题的必由之路,而建设CCUS区域中心是CCUS产业规模化、集群化发展的必然趋势,其中四川盆地是西南地区打造CCUS区域中心的最佳选择。为了加快建设中国西南地区CCUS区域中心,系统梳理了国外的经验做法,分析了其优势和挑战,结合我国西南地区的CO_(2)排放及分布情况、封存地质条件、源汇匹配关系,针对性提出了建设路径和政策建议。研究结果表明:①打造中国西南地区CCUS区域中心具有企业减碳和增产的需求巨大、高耗能行业企业碳源丰富且较为集中、地质封存潜力大且分布集中、源汇匹配情况较好、地方政府积极支持等5大优势;②当前面临的主要问题是缺乏顶层设计和统一规划、缺乏全产业链协同技术攻关的共享平台、缺乏碳减排的激励和约束政策体系等;③下一步应聚焦CCUS-EGR、CCS、DACCS等3条路径,分启动、扩展、规模化发展3个阶段打造西南地区CCUS区域中心,形成两个千万吨级产业集群和3个百万吨级产业集群,并比选技术路径和商业化路径。结论认为,要重点从完善顶层设计,出台统一的战略规划;强化科技攻关体系建设,加快形成技术成熟、经济可行的CCUS全链条技术;强化政策支持、推动国际合作等3个方面入手,加快推动中国西南地区CCUS区域中心建设。

Characteristics,evolution,and regional differences of biomass burning particles in the Sichuan Basin,China

The Sichuan Basin has experienced serious air pollution from fine particulate matter(PM2.5) in the past few years with biomass burning has been identified as a major source of PM2.5 in this region.We used single particle aerosol mass spectrometer to investigate the characteristics of biomass burning particles in three interacting cities representing different types of urban environment in the Sichuan Basin.A total of 739,794,279,610,and380,636 biomass burning particles were detected at Ya’an,Guang’an,and Chengdu,which represented 42%,69%,and 61%,respectively,of the total number of particles.We analyzed the chemical composition,transportation,and evolution of biomass burning particles.The contribution of K-elemental carbon and K-secondary inorganic particles was highest in Ya’an(36%) and Guang’an(47%),respectively,reflecting the important role of fresh biomass burning particles and long-distance transport in these two cities.Air masses originating from different directions corresponded to different levels of PM2.5 and the contributions of polluted clusters increased significantly on polluted days.Fresh and secondary inorganic biomass burning particles increased pollution at Ya’an and Guang’an,respectively,but dominated different stages of pollution in Chengdu.K-nitrate particles were formed by photochemical reactions,whereas K-sulfate particles were formed by both photochemical and liquid-phase reactions.Investigation of the degree of particle aging showed that there were more fresh particles at Ya’an and more aged particles at Guang’an.These results are useful in helping our understanding of the characteristics of biomass burning particles and evaluating their role in PM2.5 pollution in the Sichuan Basin.

Sediment source identification by using ^(137)_Cs and ^(210)Pb radionuclides in a small catchment of the Hilly Sichuan Basin, China

Double radionuclide tracers of 137Cs and 210Pb were used to investigate sediment sources in the Wujia Gully, a small catchment in the Hilly Sichuam Basin in 2002. Aver-age 137Cs and 210Pb concentrations in the source soils of the steep forest slopes, gentle cultivated terraces and bare slopes were 7.15±0.40 and 162.01±3.86 Bqkg-1, 4.01±0.31 and 70.96±2.65 Bq·kg-1, and 0 and 15.12±1.22 Bq·kg-1, re-spectively, while those concentrations in the recently depos-ited sediments in the reservoir were 3.06±0.23 and 72.66±1.61 Bq·kg-1, respectively. By using the mixing model, the relative sediment contributions from steep forest slopes, gen-tle cultivated terraces and bare slopes (including channel banks) were estimated to be 18%, 46% and 36%, respec-tively. Cultivated terraces and bare slopes (including channel banks) were the first and the second important sediment sources in catchment. Specific sediment yield in the catch-ment was 642 t·km-2·a-1 from the deposited sediment volume in the reservoir since 1956. Soil erosion rates for the forest slopes and cultivated terraces, which accounted for 2/3 and 1/3 of the drainage area in the catchment, were esti-mated to be 173 and 886 t·km-2·a-1, respectively.

黑龙滩水库消落带植被恢复模式对土壤水稳性团聚体组成及其稳定性的影响

[目的]为阐明水库消落带不同植被恢复模式对土壤水稳性团聚体组成及其稳定性的影响。[方法]以川中丘陵区黑龙滩水库消落带人工恢复与自然恢复植被下的土壤为研究对象,利用湿筛法测定分析土壤水稳性团聚体组成特征及其稳定性指标。[结果]消落带土壤>0.25 mm水稳性大团聚体含量与未淹水对照相比降低4.21%,其中,自然恢复植被下土壤水稳性大团聚体含量较对照下降12.27%,人工恢复植被下大团聚体含量较对照增加3.84%;不同植被恢复模式下土壤水稳性团聚体组成差异显著(p<0.05),人工恢复植被下土壤大团聚体含量(69.48%)显著高于自然恢复模式(43.20%);消落带土壤水稳性团聚体稳定性随水位高程增加而升高,团聚体稳定性指标>0.25 mm水稳性团聚体含量(R_(0.25))、平均重量直径(MWD)、几何平均直径(GMD)人工恢复模式下均大于自然恢复模式,团聚体分形维数(D)、土壤可蚀性因子(K)与团聚体破坏率(PAD)人工恢复模式小于自然恢复模式,表明人工恢复模式下土壤水稳性团聚体稳定性、土壤抗蚀性高于自然恢复模式。[结论]黑龙滩水库消落带在淹水后土壤团聚体稳定性下降,但人工恢复模式能有效改善土壤团粒结构,研究结果可为黑龙滩水库消落带土壤结构稳定性评价及植被恢复提供科学依据。

三维地震速度建模技术在川南页岩气随钻地质导向中的应用

四川盆地川南地区地质构造复杂,地层变形强度不一,精细三维地震速度建模难度较大。以往地震速度建模更多侧重于深层目的层水平段的迭代校正,但丛式平台井在浅层非目的层段复杂工况(气侵、溢流、漏失、掉块等)频频发生,严重影响了钻井时效和施工安全,亟需建立深、浅层兼顾的精细地震速度模型进行时深转换。基于三维时间域地震数据,通过精细人工合成地震记录标定,结合层位数据和井数据,建立初始地震速度模型,并参考实钻邻井数据设置虚拟控制井,采用最小曲率插值和反距离加权插值相结合的方法,对初始地震速度模型进行优化,可快速实现深、浅层同时迭代校正,最终得到符合构造沉积特征的精细三维地震速度模型。在川南地区现场随钻地质导向过程中应用校正后的三维地震速度模型可以及时、准确地为钻井工程提供全层系风险预警和地质导向建议,效果显著,可推广应用。

Response of remotely sensed Normalized Difference Water Deviation Index to the 2006 Drought of eastern Sichuan Basin

One of the most serious droughts in last century occurred in eastern Sichuan Basin in the summer of 2006 (hereinafter called the Drought). The response of Moderate Resolution Imaging Spectroradiometer (MODIS, boarding on NASA satellites of Terra and Aqua) to the Drought was analyzed in order to reach one practicable monitoring solution for regional soil moisture. Temporal process and spatial extension of the Drought were firstly estimated with ground meteorological and hydrological observations. Then, for the whole region of Sichuan and Chongqing, the remotely sensed Normalized Difference Water In- dex (NDWI) for the summers of 2001―2006 were calculated based on 8-day composite MODIS products, which were further used to construct a new water index (Normalized Difference Water Deviation Index, NDWDI) to examine the sensitivity of remote sensing in the Drought. The study showed that the NDWDI is more sensitive to regional drought than other absolute-soil-moisture-based indices. With the new index, the study extracted the spatial-temporal characteristics of the 2006 Drought, and explored its developing and withdrawing processes, which agreed with related statistics. Compared with ground method of drought observation, the NDWDI-based remote sensing solution of this paper is more pref- erable and practicable in that the local soil properties of water consumption and supply are implicitly taken into account, and the spatial representativity limit of ground observation is circumvented to a degree as satellite remotely senses the earth surface in a way of two-dimensional pixel matrix. So, the NDWDI-based method can be used to monitor regional soil water stress situation more practically and efficiently.

Interruption of schistosomiasis transmission in mountainous and hilly regions with an integrated strategy:a longitudinal case study in Sichuan,China

Background:Schistosomiasis remains a major public health concern in China.Since 2004,an integrated strategy was developed to control the transmission of Schistosoma japonicum in China.However,the long-term effectiveness of this integrated strategy for the interruption of schistosomiasis transmission remains unknown in the mountainous and hilly regions of China until now.This longitudinal study aims to evaluate the effectiveness of the integrated strategy on transmission interruption of schistosomiasis in Sichuan Province from 2005 through 2014.Methods:The data regarding replacement of bovines with machines,improved sanitation,access to clean water,construction of public toilets and household latrines,snail control,chemotherapy,and health education were captured from the annual report of the schistosomiasis control programmes in Sichuan Province from 2005 to 2014,and S.japonicum infection in humans,bovines and snails were estimated to evaluate the effectiveness of the integrated strategy.Results:During the 10-year period from 2005 through 2014,a total of 536568 machines were used to replace bovines,and 3284333 household lavatories and 15523 public latrines were built.Tap water was supplied to 19116344 residents living in the endemic villages.A total of 230098 hm2 snail habitats were given molluscicide treatment,and 357233 hm2 snail habitats received environmental improvements.There were 7268138 humans and 840845 bovines given praziquantel chemotherapy.During the 10-year study period,information,education and communication(IEC)materials were provided to village officers,teachers and schoolchildren.The 10-year implementation of the integrated strategy resulted in a great reduction in S.japonicum infection in humans,bovines and snails.Since 2007,no acute infection was detected,and no schistosomiasis cases or infected bovines were identified since 2012.In addition,the snail habitats reduced by 62.39%in 2014 as compared to that in 2005,and no S.japonicum infection was identified in snails since 2007.By 2014,88.9%of the endemic counties achieved the transmission interruption of schistosomiasis and transmission control of schistosmiasis was achieved in the whole province in 2008.Conclusion:The government-directed and multi-department integrated strategy is effective for interrupting the transmission of schistosomiasis in the mountainous and hilly regions of China.

Seismic motion attenuation relations in Sichuan and adjacent areas

The Sichuan and adjacent areas is divided into southwest China region （SWCR） and Sichuan Basin region （SCBR） according to tectonic backgrounds and seismic damage distribution features. 96 modem destructive earthquakes in SWCR and 40 in SCBR are gathered respectively. All their magnitude parameters are checked. Based on the statistic relations between epicentral intensity and magnitude as well as relation between sensible radius and magnitude, the near and far field seismic intensity attenuation features are represented and controlled. And then the seismic intensity attenuation relations along major axis, minor axis and mean axis are established separately. The system-atic deviations of surface wave magnitude between China seismograph network and U.S. seismograph network are considered in this paper. By making use of the new attenuation relations of bedrock horizontal ground acceleration response spectrum in west U.S., the attenuation relations of bedrock horizontal ground acceleration response spec- trum in SWCR and SCBR are digital transformed based on the attenuation model considering acceleration saturation of distance and magnitude in near field.

川中丘陵区典型小流域旱地地温数据集(1997-2021年)

下垫面温度(地表温度)和不同深度的土壤温度统称地温,它的变化和变化规律是大气与陆地表面能量和物质交换的综合表征,因此地温是土壤热力状况的重要参量。四川盐亭农田生态系统国家野外科学观测研究站(简称盐亭站,代码YGA)位于亚热带四川盆地农业生态区,是中国生态系统研究网络(Chinese Ecosystem Research Network,CERN)和国家科技基础条件平台布局在该生态区域的农田生态系统试验观测与研究平台。本数据集是基于盐亭站综合气象观测场长期的自动站观测数据和人工观测数据整理计算而成,共包括4个数据文件,分别是自动站每日逐时地温数据(1997–2021)、自动站逐日地温统计数据(2004–2021)、自动站地温度月值统计数据(2004–2021)和人工观测地表温度日值与月值数据(2004–2021),数据量约8.85 MB。地温为野外台站联网观测指标,其观测仪器、数据获取过程和数据质控执行统一的相关规范和标准,确保地温数据的可靠性和可比性。长时间序列、多层次地温数据的积累,可为生态系统的能量物质交换、环境变化响应科学研究以及盆地农业主体区域在耕地质量评估和粮食安全方面的应用研究提供科学数据支撑。

川中丘陵区典型小流域地表水环境特征数据集(2005-2019)

基于中国科学院盐亭紫色土农业生态试验站(简称盐亭站)对川中丘陵区典型小流域地表水环境状况的长期常规监测,集成2005–2019年川中丘陵区典型小流域地表水环境特征数据集。本数据集涉及典型小流域内布设的4个监测点,分别位于小流域的沟头池塘、中游汇水沟渠、集水区出口处的田面和堰口;2005–2006年,每3个月采集1次水样,2007–2009年,加采8月和9月的水样,2010–2019年则每月采集1次,采集样品时间均为每月20日,数据包含反映地表水环境的酸碱度、总氮、总磷、矿化度、电导率、化学需氧量、钙离子、镁离子、钾离子、钠离子、碳酸根离子、重碳酸根离子、氯化物、硫酸根离子、磷酸根离子和硝酸根离子等16个理化指标。监测样点布设、采集水样过程、实验室分析和数据分析均遵照中国生态系统研究网络(CERN)和国家科技基础平台要求的规范和标准进行,数据质量可靠,并与网络其他野外台站同类数据具有可比性。可为环境科学研究、生态清洁小流域以及水环境综合评价、管理和规划提供重要数据支持。

四川盆地中西部区域性超压特征与天然气大规模聚集的关系

四川盆地近20年来持续发现大型、超大型气田,其天然气大规模聚集的成藏机理却众说纷纭,尤其是地层超压如何有效促进大气田形成的机理已经成为地质学家研究的重点。为此,基于实测地层压力与钻井液密度等开展了地层压力系数与视地层压力系数的计算与分析,并结合天然气成藏地质条件与气藏发育规律,探讨了四川盆地中西部重点地区超压体系基本特征及其与天然气富集的关系。研究结果表明:①四川盆地中西部地区除山前破碎带、西南部地区喜马拉雅期隆升破裂带外,其他大部分地区普遍存在超压现象,超压地层的厚度介于4000~8000 m;②超压普遍发育,天然气大规模聚集的区域性直接盖层变得模糊与不重要,导致岩性气藏的大规模、大面积、多层系发育成为可能;③巨厚超压层及其内部断裂的发育,促进了气源充足、构造相对稳定区天然气多层系与多区带规模成藏。结论认为,四川盆地中、西部地区构造相对稳定区巨厚层超压的形成,是现今天然气得以多层位与多区带大规模聚集的重要机制,巨厚超压层内部与其下部地层压力系数较低的区域是最有利于大型气田形成的区域。

基于地理探测器的环四川盆地地质公园空间分布的影响机制分析

为了探索环四川盆地区域内地质公园空间分布的影响因素,以及量化研究各影响因素对地质公园空间分布的影响程度,基于环四川盆地2000—2019年的地质公园数据,采用地理统计的方法研究该区域地质公园的时空分布特征。研究表明:环四川盆地的地质公园空间分布表现为两个特征:(1)在2005—2019年间,环四川盆地地质公园的空间分布类型为离散分布,总体具有“东多西少”的分散分布状态。(2)在时间变化上呈现出明显的阶段特征,即2005—2010年为空间分布较为分散的缓慢发展期和2010—2019年为多核形成的快速发展期。在此基础上,结合地理探测器模型和Pearson相关系数法进一步量化研究地质公园空间分布的影响机制。(3)各影响因子的影响强度大小依次为:年降水量>高程值>土壤类型>地质环境分区>公路里程>人均GDP>地貌类型。(4)各影响因子的相关性大小排序为:年降水量、人均GDP和公路里程数对地质公园的建设与发展有促进作用,高程值与地质公园的发展存在负相关关系。

四川盆地东部寒武系油气跨层成藏及天然气勘探意义

四川盆地东部发育下寒武统筇竹寺组泥页岩烃源岩,其生成的油气向上能否穿越中下寒武统膏盐岩区域盖层,并在中上寒武统洗象池群储层聚集成藏(即油气跨层成藏),一直缺乏清晰的认识。为此,开展了洗象池群储层固体沥青和中下寒武统膏盐岩区域盖层封盖性等研究,探讨了油气跨层成藏及其天然气勘探意义。四川盆地东部洗象池群储层固体沥青主要来源于筇竹寺组泥页岩烃源岩;中下寒武统膏盐岩区域盖层封闭性良好,但在中二叠世至中三叠世,复活的基底断裂和新形成的规模较大的断裂使其封盖完整性遭受一定程度的破坏,为寒武系油气跨层成藏提供了重要的垂向运移通道。该区寒武系油气成藏经历了盐下早期古油藏(S_(3)—P_(1))、油气跨层成藏(P_(2)—T_(2))和古气藏(T_(3)—K_(1))等演化阶段;油气跨层成藏是多旋回叠合盆地油气成藏的重要特征,中二叠世至中三叠世复活的基底断裂和新形成的规模较大的断裂是寻找洗象池群原生古气藏的重要线索。确定和评价原生古气藏将是今后研究区洗象池群天然气勘探的重点和难点。

长江流域四川区域城市水生态环境问题解析及治理对策

以长江流域四川区域18个城市为研究对象,分析了近5年区域内长江干流(四川段)、支流岷沱江和嘉陵江流域典型城市建成区的水环境质量变化趋势及主要污染指标,估算流域内城镇生活源、工业源和城市面源化学需氧量(COD)、氨氮、总氮(TN)和总磷(TP)污染排放负荷,解析城市水生态环境问题及成因。结果表明:近5年长江流域四川区域城市水体水质逐年向好,TP、氨氮、TN和COD是区域内水体的主要污染指标;城镇生活源为区域城市的主要污染源,城市基础设施建设不足、部分城市工业污染问题突出、丰水期城市面源负荷较大、资源型和水质型缺水并存等导致了城市水生态环境问题。在此基础上,提出通过推进城镇污水收集和处理系统提质增效、实施典型工业废水专项治理、建设溢流污水处理设施、开展城市水体生态修复等措施进一步提升长江流域四川区域城市水生态环境质量。

山丘区留空库容削峰调洪系统的设计及应用

山丘区建设项目受地形及工程造价影响,需尽可能减小围墙外排洪沟断面的过水流量,但通常建设项目围墙外山洪沟低洼处已有或拟建塘坝库容较小且难以扩容,常规方法无法满足减小排洪沟断面设计流量的要求。因此,提出一种建设项目防排洪设小水库留空库容削峰调洪技术方案,较传统水库调洪可大大节省库容,同时满足下游减小排洪沟流量的要求,并结合实际工程实例,详细阐述了留空库容削峰调洪系统的功能和设计要点,可为山丘区建设项目特小流域防排洪工程提供重要的技术支撑和经验借鉴。

不同改造模式对柏木人工林土壤团聚体粒径分布及稳定性的影响

土壤团聚体是土壤结构的基本单元,对改善土壤质量和提升养分含量具有重要作用.为研究不同改造模式下川中丘陵区柏木人工林土壤团聚体特征,以绵阳市盐亭县林山乡柏木人工林为研究对象,基于干筛法和湿筛法比较分析疏伐改造(ET)、林窗改造(FG)、林带改造(SF)和柏木纯林(PC)4种模式0~40 cm土层深度下土壤团聚体粒径分布特征和稳定性指标.结果表明:(1)在干筛处理下,4种模式的柏木人工林土壤机械性团聚体以>2 mm为主,含量为48.07%~74.74%,而0~20 cm土层表现为疏伐改造显著高于林带改造,20~40 cm土层表现为柏木纯林显著高于林窗改造和林带改造.(2)在湿筛处理下,0~20 cm土层>2 mm粒径土壤水稳性团聚体表现为林带改造显著高于柏木纯林与林窗改造,0.053~0.25 mm粒径团聚体表现为林窗改造显著高于疏伐改造与林带改造.(3)平均重量直径(MWD)和几何平均直径(GMD)0.56~1.77,土壤水稳性团聚体MWD和GMD在0~20 cm土层表现为疏伐改造显著高于林窗改造.这表明,改造模式能够显著影响柏木人工林土壤团聚体粒径分布和稳定性特征,本研究为川中丘陵区柏木人工林的经营管理提供基础数据.