中国水土保持科学
中国水土保持科学
 
 
 
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2019 Vol.17 No.2  Published 2019-04-30
  
 
Foundamental Studies
1 MENG Min, JING Hang, YAO Xu, WANG Guoliang, LIU Guobin
Effect of nitrogen addition on enzyme activity during fine root decomposition of Pinus tabulaeformis
[Background] Exploring the effect of nitrogen (N) addition on enzyme activity during fine root decomposition is helpful to elucidate the potential mechanism of N addition affecting fine root decomposition, and eventually provides a basis for studying N deposition affecting carbon balance and nutrient cycling in forest ecosystem.[Methods] The Pinus tabulaeformis seedling were treated with N addition (N0, 0 g/(m2·a); N3, 3 g/(m2·a); N6, 6 g/(m2·a); and N9, 9 g/(m2·a)) for 2 years, and then the fine roots were grouped with 3 diameter size classes (< 0.5 mm; 0.5-1.0 mm and 1.0-2.0 mm) and buried using litterbag method in a P. tabulaeformis forest where was treated with N addition for 2 years, respectively. The litterbags were sampled every 2 months, then the enzyme activities (cellobiase, alkaline phosphatase and galactosidase) and carbon (C), N phosphorus (P) concentrations were determined in laboratory.[Results] During fine root decomposition, the activity of cellobiase increased first and then decreased, and then increased in the later stage. The activities of alkaline phosphatase and galactosidase increased first and then decreased, and the activities were the highest in the middle stage of fine root decomposition. N addition significantly affected cellobiase and galactosidase activities (P< 0.05), but had no significant effect on alkaline phosphatase activity. N3 treatment increased cellobiase activity of 0-0.5 mm and >0.5-1.0 mm fine roots, N9 treatment increased cellobiase activity of >1.0-2.0 mm fine root. N addition decreased galactosidase activity of 0-0.5 mm fine root, and N9 decreased galactosidase activity of >0.5-1.0 mm and >1.0-2.0 mm fine roots. At different stages of decomposition, the effect of N addition on enzyme activity varied depending on the enzyme species and fine root diameters. There were significant positive correlations among different enzyme activities, and the correlation between alkaline phosphatase activity and galactosidase activity was the strongest. Correlation analysis showed that enzymes not only had specific influences, but also had common relations among enzyme species. Enzyme activities were significantly positively correlated with fine root C, N, P concentrations, and negatively correlated with fine root N:P ratio. The correlations between enzyme activity and fine root quality were relatively consistent, but the correlations between enzyme activity and temperature, moisture were quite different.[Conclusions] N addition has a variety of effects on the enzyme activity, such as increasing and decreasing, there is an interaction among N addition, decomposition time and fine root diameter to make the effect of N addition on enzyme activity varied during fine root decomposition. N addition increases decomposition enzyme activity by increasing fine root quality, environmental conditions such as temperature and moisture has varied effects on different enzyme activities during this process.
2019 Vol. 17 (2): 1-9 [Abstract] ( 397 ) [HTML 1KB] [PDF 913KB] ( 508 )
10 ZHU Zhijun, NIU Jianzhi, XU Jun
Effects of lower pruning on water interception of trees
[Background] Lower pruning is one mainly method of forest tending. Canopy interception is an important process of forest hydrological cycle. Lower pruning can effectively change the characteristics of canopy interception. Few researches focus on this aspect. In this study, 6 kinds of typical Beijing mountain afforestation tree species Platycladus orientalis, Pinus tabuliformis Carr., Quercus variabilis Blume, Acer elegantulum Bunge, Pinus bungeana Zucc. and Cotinus coggygria Scop. are used to be the research objects, exploring the way of lower pruning treatments for characteristics changes in the canopy interception.[Method] The method of indoor simulated rainfall was adopted in the experiment. An equipment of canopy interception measurement was made to measure the amount of water interception. There are three parts of the equipment, a bench scale to measure the weight, a metal rain cover to block rain drops and barbed wire to put litters. We put the pot with experimental trees on the bench scale and then start raining. We read the weight on bench scale every 30 seconds. After one hour's raining, continue reading the weight until the weight reading was unchanged. In this research we used weight to express the canopy interception. The final weight reading is the minimum interception(Cmin) of the tree. The maximum of bench scale during the raining is called the maximum interception(Cmax). We can get the data of canopy interception with higher precision in this way. After lower pruning, put trees on the equipment under the rainfall device to repeat experiment. After that, tree litters were put on the barbed wire. The thickness was 2 cm. We repeated the rainfall experiment.[Results] 1) Lower pruning treatment influenced the conifer's canopy interception more than that of broad-leaved tree. The maximum interception of coniferous species decreased by more than 50%. However broad-leaved tree species decreased by less than 20%. 2) The interception ability of the lower layer leaves of broad-leaved trees was much stronger than that of the lower branches. While the interception ability of the lower and lower leaves of the coniferous trees was equal. The interception percentage of lower leaves of coniferous species was significantly less than that of broad-leaved species (P<0.05). Therefore, the interception percentage of lower branches was opposite. 3) After laying tree litters of 2cm, the difference of the maximum interception and the minimum interception between before and after lower pruning was below 10%.[Conclusions] The results show that the interception characteristics of coniferous and broad-leaved canopy vary with the intensity of the lower pruning, which is mainly reflected in that the coniferous tree species has stronger response strength than the broad-leaved tree species. Laying litters under the forest may effectively reduce the influence of lower pruning on the flow of trees.
2019 Vol. 17 (2): 10-16 [Abstract] ( 391 ) [HTML 1KB] [PDF 1339KB] ( 384 )
17 GAO Siyuan, ZHANG Jianjun, LI Liang, ZHANG Haibo, SUN Ruoxiu
Water storage dynamics and infiltration depth of soil and water conservation forest in the Loess Plateau of western Shanxi province
[Background] In order to explore the dynamic characteristics of water storage in the soil and water conservation forests on the Loess Plateau, the redistribution effects of the level terraces on rainwater and runoff, and the depth of rainwater penetration under different rainfall conditions were analyzed.[Methods] In this study, artificial Platycladus orientalis forest and artificial Pinus tabuliformis forest in the Loess Plateau of western Shanxi province were selected as research objects, the soil moisture content of 0-200 cm soil profile and the precipitation were determined respectively, through the application of EnviroSMART soil moisture monitoring system and HOBO tipping rain gauge. Based on the theory of water balance, the dynamic characteristics of forestland water storage capacity, the rate of forestland water accumulation and the rate of extinction were analyzed, and the effect of precipitation on the depth of rainwater penetration was explored based on the wetting front.[Results] 1) The soil water storage of P. orientalis forest (368.99 mm) was greater than that of P. tabuliformis forest (320.58 mm). 2) The average annual storage water of the level terrace (408.55 mm)> the average annual storage water of the slope (281.01 mm), On the level terraces, the storage is 127.54 mm more on the slope. 3) According to the coefficient of variation of soil water storage capacity, a year could be divided into 4 periods, stabile period of soil moisture (February-April), accumulation period of soil moisture (May-July), fluctuation period of soil moisture (August-October), fading period of soil moisture (November-January of the next year). 4) The average accumulation rate of water storage during the accumulation period is 0.68 mm/d in the P. orientalis forest, 0.64 mm/d in the P. tabuliformis forest, and the average speed of the water in the fading period is 0.34 mm/d in the P. orientalis forest, 0.36 mm/d in the P. tabuliformis forest. 5) The penetration depth of the rainwater in the P. orientalis forest is greater than that in the P. tabuliformis forest. The depth soil water responding to rainfall of the level terrace is deeper than the slope. Under the heavy rain condition, the infiltration depth of the rainwater in the P. orientalis forest is 90 cm (slope)-110 cm (level terrace), and in the P. tabuliformis forest is 60 cm (slope)-70 cm (level terrace).[Conclusions] It is recommended to use level terrace and select P. orientalis when planting soil and water conservation forests on the Loess Plateau.
2019 Vol. 17 (2): 17-26 [Abstract] ( 615 ) [HTML 1KB] [PDF 1024KB] ( 512 )
27 XUE Hao, YU Ruihong, ZHANG Yanxia, DUO Lan, HU Haizhu, HAO Yanling, LU Xixi
Temporal variation of runoff depth in the drainage basin of typical grassland area in Inner Mongolia: A case study of Xilin River Basin
[Background] Most of the existing researches focus on large-scale watersheds and humid regions, but there are few studies on runoff changes in arid grassland basins, especially the systematic study of runoff variation laws at different time scales. The study on the characteristics of runoff changes in the basin of the grassland area has important application value and guiding significance for the reasonable development and utilization of local water resources.[Methods] Located in the southeastern part of Inner Mongolia, the Xilin River Basin is a temperate semi-arid continental monsoon climate. It has the characteristics of less precipitation, more evaporation, and larger temperature difference. The measured flow data from 1968-2015 are from Xilinhot Hydrological Station. Mann-Kendall trend test method was used to analyze the decennary, annual, seasonal, and inter-annual trends of runoff depth from 1968-2015 in the Xilin River Basin. The temporal and spatial variations of river runoff at home and abroad were compared to illustrate the differences between grassland-type rivers and large rivers.[Results] 1)The average runoff in the 1990s was the largest with large fluctuation, and that in the rest of years showed a decreasing trend. 2)The annual runoff during 1968-2015 demonstrated a significant decline over time. 3)The seasonal runoff showed a significant downward trend. Among them, the decline rate in the spring and summer was insignificant, while that in the autumn was significant, and the runoff in the autumn was almost zero after 2005. 4)The inter-annual runoff depth distribution was uneven with "bimodal", which peaked in April and August respectively. 5)According to the Mann-Kendall mutation test, a abrupt change of runoff depth in Xilin River Basin occurred in 1984 and 2000. The period from 1968-1984 was defined as the base period, and the period from 1985-2000 and 2001-2015 was defined as an abrupt change period. Runoff increased during 1985-2000 by 22.84% while compared with the baseline period. The runoff during 2001-2015 showed a significant decrease, by 42.89% compared with the baseline period.[Conclusions] The main factor in the reduction of runoff in the Xilin River Basin is human activities, in which socio-economic factors such as population increases, industry and animal husbandry development affect the runoff of the Xilin River Basin. This study provides scientific basis for the optimal allocation of water resources in the Xilin River Basin. The series of ecological protection measures may reduce the impact of human activities on watershed runoff.
2019 Vol. 17 (2): 27-36 [Abstract] ( 428 ) [HTML 1KB] [PDF 1763KB] ( 412 )
37 CHEN Zhen, YUAN Mutian, CAO Qiqi, LIU Tao, XIAO Huijie
Effects of soil water content on stomatal conductance and leaf water potential of Medicago sativa and Hippophae rhamnoides
[Background] Medicago sativa and Hippophae rhamnoides are two of most important plants in the arid desert areas of northwest China. However, the mechanisms of water-saving and drought resistance of M. sativa and H. rhamnoides remain poorly understood, and the corresponding techniques need to be further studied.[Methods] The potted trials of water stress were carried out to understand the response mechanisms of stomatal conductance (Gs) and leaf water potential (ψL) to water stress for M. sativa and H. rhamnoides at seedling stage. Sufficient water supply (CK), light water stress (LD), moderate water stress (MD), and severe water stress (HD) were set up according to the percentages of soil water contents in field moisture capacity.[Results] Under different stress gradients, the diurnal variation of Gs and ψL for H. rhamnoides was similar with M-shaped and V-shaped curve, respectively, while the counterparts of M. sativa was different. The daily average Gs of H. rhamnoides was higher than that of M. sativa. And the average of Gs and ψL of two plants decreased with the increase of water stress. The correlation between Gs, ψL, and relative humidity (RHL) were significantly positively correlated for two plants. The Gs of H. rhamnoides increased at first and then decreased with the increase of photosynthetic active radiation (PAR). The Gs of M. sativa increased with the increase of PAR only when sufficient water was supplied. However, there was no correlation between Gs and PAR under stress. The ψL and leaf temperature (TL) of H. rhamnoides were significantly correlated with different water stress treatments, but not for M. sativa. The Gs and ψL of H. rhamnoides were 87%~203% higher than that of M. sativa with the change of RHL, TL, and PAR. Therefore, the response of H. rhamnoides to meteorological factors was more sensitive than M. sativa.[Conclusions] It is more adaptable for H. rhamnoides to drought stress environment, while the response mechanism of M. sativa to water stress is more complicated. This study will help to understand the mechanism of H. rhamnoides and M. sativa adapting to drought stress environment at seedling stage and provide a theoretical support for vegetation restoration in desert areas.
2019 Vol. 17 (2): 37-43 [Abstract] ( 430 ) [HTML 1KB] [PDF 940KB] ( 451 )
 
Applied Studies
44 KONG Yuhua, HAN Mengjuan, ZHANG Zhihua, XU Xingkai, LAI Yong, YANG Xitian
Seasonal dynamics of dissolved organic matter contents in surface soils of 3 artificial forests
[Background] Soil active carbon and nitrogen are the most important and active components during soil carbon and nitrogen cycling, and their seasonal changes are of great significance to carbon and nitrogen cycling and redistribution within and between different ecosystems, as well as soil formation. To reveal soil carbon and nitrogen turnover mechanism in artificial forest ecosystem, seasonal dynamics of soil active carbon and nitrogen contents and other factors were determined.[Methods] Three typical artificial forests (Platycladus orientalis, Robinia pseudoacacia and Quercus variabilis) in the rocky mountainous area of northern China were selected as the research objects. Two treatments were set up, i.e., Y (with litter return) and W (without litter return). The characteristics and variation trends of dissolved organic carbon (DOC) and dissolved organic nitrogen (DON) and inorganic nitrogen (SIN, including NO3--N and NH4+-N) contents at the depth of 0-10 cm soils were investigated during March, June, September and December.[Results] The DOC, DON, NO3--N and NH4+-N contents in the 3 artificial forests soils all showed general significant seasonal dynamics (P<0.05), with peak values in June. NO3--N was the main form of inorganic nitrogen in soils, and its ratio to SIN in P. orientalis, R. pseudoacacia and Q. variabilis artificial forests were 70.2%, 72.8% and 53.4%, respectively. Artificial forest types had a significant impact on soil DOC and NO3--N contents (P<0.05). The annual average of soil DOC and DON contents with litter return presented as P. orientalis > Q. variabilis > R. pseudoacacia, while soil NO3--N, NH4+-N and SIN contents tended to be as P. orientalis > R. pseudoacacia > Q. variabilis. Litter treatments had a significant impact on soil DOC and DON contents (P<0.05), while no significant impact on soil NO3--N and NH4+-N contents. Further, most of forests soil without litter return showed higher DOC and DON concentrations than those of with litter return. A stepwise regression analysis showed that the main influencing factor of soil DOC in all treatments was soil total nitrogen (TN), which explained 76.4% of its variation. The main influencing factors for soil DON were soil TN, NO3--N, air temperature and NH4+-N, which together explained 86.6% of its variation.[Conclusions] Different artificial forest types significantly affected the seasonal variation of soil active carbon and nitrogen. Litter returns increased soil carbon and nitrogen content and turnover rate. Further, temperature was the main driving factor for soil active carbon and nitrogen turnover in the rocky mountainous areas of North China. Besides, soil DOC and DON turnover were mainly affected by soil TN content in the present artificial forest ecosystem.
2019 Vol. 17 (2): 44-52 [Abstract] ( 497 ) [HTML 1KB] [PDF 856KB] ( 477 )
53 ZHOU Xia, WEI Yang, LI Dongrong, JIANG Jing, ZHANG Chaobo
Strengthening effects of alfalfa roots on soil shear resistance in loess region
[Background] Surface erosion, slope instability and soil-water loss caused by soil erosion have become major ecological and environmental problems in China. Plant measures are commonly used ways in preventing soil erosion, and are also the most effective and fundamental methods for soil and water conservation. Shrub and grass have become priorities for solving the contradiction between water resources and ecological environment and preventing soil erosion.[Methods] Direct shear tests were conducted on loess soil samples with alfalfa roots, using the devices including direct shear box, frame, jack, hydraulic pump, displacement sensor, pressure sensor, recorder etc. The shear strength of alfalfa root-loess samples with various soil water contents and in different soil depth (10, 20, and 30 cm) were measured, the characteristics of shear failure of the soil samples and the distribution of the failure roots in shear plane were determined, and the relationship between shear strength and shear displacement of samples in different soil depth and with different soil water content were analyzed.[Results] 1) The alfalfa roots increased the shear strength of the soil by 43.10%-89.41%, and increased the shear displacement by around 13.16-56.95 mm. 2) The shear strength of both the alfalfa root-loess samples and rootless soil samples decreased with increasing soil water content, and the soil water content presented a negative effect on the shear strength of the soil. When the soil water content was 18.97%, the shear strength of the soil composite sample was 10.02 kPa and the shear displacement was 70.55 mm. The maximum shear strength increased by 89.41% and the shear displacement increased about 25 mm compared with the bare soil sample. 3) When the soil water content was about 30% in the shear depth of 30 cm, the soil reinforcement effect of the root system was very limited. 4) The enhancement effect of alfalfa roots on soil shear strength decreased with the increase of soil shear depth, and the root system had a more significant effect on the shear strength of shallow soil.[Conclusions] The results are of practical importance to the selection of dominant species, to the improvement of slope stability and the prevention of soil and water loss on the Loess Plateau. It can also provide theoretical basis of vegetation measures for slope consolidation and soil and water conservation.
2019 Vol. 17 (2): 53-59 [Abstract] ( 409 ) [HTML 1KB] [PDF 1686KB] ( 555 )
60 PENG Ruidong, BI Huaxing, GUO Mengxia, SUN Yubo, DUAN Hangqi, WANG Jingjing
Temporal and spatial distribution of the shading intensity of apple-soybean intercropping system in the loess area of western Shanxi
[Background] Agroforestry system is one of the important soil and water conservation measures in the loess hilly area of western Shanxi. Apple-soybean intercropping system is one of the most common agroforestry systems. Agroforestry can take into account economic benefits and benefits of soil and water conservation. Quantitative analysis of shading intensity of apple-soybean intercropping system and its spatial-temporal dynamic distribution characteristics may provide a theoretical basis for the configuration model of fruit-crop intercropping system based on light environment, and contribute to soil and water conservation and agricultural sustainable development in the loess region of western Shanxi.[Methods] An intercropping system of 5-year-old apple-soybean on the loess area of western Shanxi was studied. The spatial and temporal distribution of shading intensity and its impact on soybean were studied through a method combined by positional monitoring and mathematical analysis. The diurnal variation chart and the growth season variation diagram of the shading intensity were plotted based on the photosynthetically active radiation measured value, from which the correlation between the temporal and spatial distribution of shading intensity and soybean yield was analyzed.[Results] 1) The shading intensity of the apple-soybean intercropping system decreased from the center to the periphery. The average shading intensity on the north and south sides of the tree were 0.29 and 0.22, respectively; and the average shading intensity on the west and east sides of the tree were 0.26 and 0.24, respectively. 2) The average daily shading intensity of intercropped crops in pod-forming period, flowering and seedling period were 0.28, 0.17 and 0.14, respectively. 3) The biomass and yield distribution of soybean showed an increase from the position of the surrounding fruit trees to the center of the study area. The shading intensity of the fruit trees was significantly negatively correlated with the biomass and yield of soybeans, and also the shading intensity during the pod-forming stage had the greatest impact on yield.[Conclusions] To effectively mitigate the interspecific competition in apple-soybean intercropping systems, soybean should be planted in the central area of the intercropping system, and the planting amount in the north and west of the apple tree rows should be slightly less than that in the South and east of the apple tree rows. In addition, in the podding stage of soybeans, agronomic measures such as laying reflective film can be used to increase photosynthetic active radiation (PAR) under the forest to increase soybean yield.
2019 Vol. 17 (2): 60-69 [Abstract] ( 458 ) [HTML 1KB] [PDF 4412KB] ( 565 )
70 WANG Xiuli, LIU Yumin, GAO Runmei
Effects of ectomycorrhizal fungi on the growth of Pinus tabulaeformis seedlings under drought stress
[Background] It researched the effect of ectomycorrhizal fungi on Pinus tabulaeformis seedlings to increase the survival rate of seedlings, promote the regeneration of tree species, and prevent soil erosion.[Methods] Potted water was used to simulate drought stress, and four water treatments were designed:control(CK),light drought(LD),moderate drought(MD),severe drought(SD). Inoculating the seedlings of Pinus tabulaeformis with Trichoderma spp. was to study the effect of growth which ectomycorrhizal fungi had on P. tabulaeformis seedling under drought stress. To each treatment,It selected seedlings whose growth was basically the same, and measured the morphological and physiological indexes. The specific operation refered to Principles and Techniques of Plant Physiological and Biochemical Experiments written by Li Hesheng.[Results] The plant height and needle length of P. tabulaeformis seedlings were significantly affected by inoculation with Trichoderma spp. and drought stress treatment (P<0.01), but the interaction was not significant (P>0.05).The effects of inoculation with Trichoderma spp. and drought stress on the soluble protein, soluble sugar and starch content of P. tabulaeformis seedlings were significant (P<0.01). However, the interaction to the soluble protein and starch content of Pi. tabulaeformis seedlings was not significant (P>0.05), and the interaction to the soluble sugar content was significantly affected (P<0.01). The detailed analysis results to the morphological and physiological indexes of P. tabulaeformis seedlings were as follows:(1) After inoculation with Trichoderma spp., the biomass and root-shoot ratio of P. tabulaeformis seedlings were significantly increased (P<0.05).The mycorrhizal dependence on Trichoderma spp. was moderately dependent. Under drought stress, the plant height and needle length of P. tabulaeformis seedlings showed a decreasing trend. However, after inoculation with Trichoderma spp., the decrease of plant height and needle length was weakened, and the drought resistance of seedling was significantly enhanced (P<0.01). (2) With the increase of drought stress, the soluble protein and starch content of needles in P. tabulaeformis seedlings continued to decrease. After inoculation with Trichoderma spp., the corresponding index showed a decreasing trend with increasing stress, but the trend of inoculated Trichoderma spp. seedlings was weaker than that of uninoculated seedlings. (P<0.01). (3) Under drought stress, the soluble sugar content of needles in P. tabulaeformis seedlings showed a trend of "first rise and then fall". The soluble sugar content of seedlings uninoculated and inoculated Trichoderma spp. reached the highest value in LD and MD, respectively. In other words, the drought tolerance threshold of the seedlings increased.[Conclusions] The results showed that under drought stress, ectomycorrhizal fungi promoted the growth of P. tabulaeformis seedlings. Under moderate drought stress, Trichoderma spp. had the most significant effect on the growth of P. tabulaeformis seedlings. Under the same water treatment, the mycorrhizal seedlings had stronger drought resistance than non-mycorrhizal seedlings.
2019 Vol. 17 (2): 70-76 [Abstract] ( 444 ) [HTML 1KB] [PDF 1177KB] ( 427 )
77 HAO Shanshan, LI Menghua, MA Yongqiang, SHI Yun
Significance analysis of soil erosion factors in loess hilly gully region
[Background] The terrain of loess hilly gully region is complex and varied, and soil erosion is serious. Soil erosion is a nonlinear system, influenced by various uncertain factors, such as soil, vegetation, terrain and others, the result of erosion is very complicated.[Methods] In order to explore the effects of land use types, topography, rainfall and other soil erosion factors in the loess hilly gully region, take Pengyang county as an example, based on the data source in 1995, 2005, 2015, such as land use, annual rainfall, DEM (5 m), etc. In the ecological zoning of Pengyang county, 11 small watershed areas such as Gaojianpu and Hugou were selected as experimental zones. Firstly, the revised universal soil loss equation (RUSLE) was adopted to calculate the soil erosion modulus and five influence factors, such as rainfall erosion force, slope and slope length in each small watershed. Then the BP neural network method was applied to construct the relational model. The five influence soil erosion factors in various small watershed as input variables, soil erosion modulus as the output variable, and finally the validity of the model was predicted and verified.[Results] 1) BP neural network model effectively predicted the significance of soil erosion influencing factors. 2) In the small watershed scale of the study area, topographic factors had the strongest significance to soil erosion, while soil erodibility factors had the weakest significance to soil erosion. 3) On the time scale, there was a slight difference between soil erosion influnence factors in small watershed. The rainfall erosion factor was reflected by rainfall, the significance of soil and water conservation measures factor and the vegetation cover and management factor were related to the implementation of ecological construction projects such as the project of returning cultivated land to forest (grass). In 2005, soil and water conservation measures factor and vegetation cover and management factors showed the inhibition of soil erosion. 4) The significance prediction results of 2015 were applicable to the study area with ecological natural restoration, and the significance of soil erosion influencing factors was as follows:SL > P > R > C > K.[Conclusions] The results show the method based on BP neural network model to predict the significance of soil erosion impact factor is applicable to loess hilly region, and it can provide scientific basis for the follow-up comprehensive governance of small watershed.
2019 Vol. 17 (2): 77-86 [Abstract] ( 542 ) [HTML 1KB] [PDF 934KB] ( 485 )
87 XUE Lingyu, LI Qingdian, LI Jinhua, XIAO Mao, SHI Ge, WANG Yanping, LI Chuanrong, SHEN Weixing, GUO Huiling, ZHANG Yikun
Effect of different mixed proportion on soil quantity in mixed Robinia pseudoacacia and Pinus tabulaeformis plantations
[Background] Robinia pseudoacacia is nitrogen-fixing pioneer tree, which has been extensively naturalized in the temperate regions of North America, Europe, and Asia and can improve soil quality and alter soil microbial community. Due to its root-sucker reproduction, R. pseudoacacia formed specific plant communities, whose herb layer is markedly different from that in forest dominated by native trees, resulting in the ecological risk. It causes both plant richness loss and shifts in species composition. In order to lift the reasonable utilization of R. pseudoacacia and let it play a greater role, the appropriate proportion of R. pseudoacacia was explored in Mount Tai.[Methods] The main soil types are crude brown soil and common brown soil. The elevation range of the sample in this study are 580-700 m and the slope are southeast. The sampling sites were determined based on the mixed proportion of R. pseudoacacia and Pinus tabulaeformis. Four types and three repeats for each type were set:type Ⅰ:pure R. pseudoacia (100%); type Ⅱ (70% R. pseudoacia+ 30% P. tabulaeformis); type Ⅲ (40% R. pseudoacia + 60% P. tabulaeformis); type Ⅳ:pure P. tabulaeformis(100%). The four types presented continuous patch distribution in this scenic spot, and the habitat characteristics were relatively consistent. Soil microorganisms, soil enzyme activities and soil nutrients for four types were analyzed. Soil quality of these forest stands was further assessed with principal component analysis (MDS-PCA).[Results] 1) Soil microorganisms, soil enzyme activities and soil nutrients increased with the increasing of proportion of R. pseudoacia. The soil microorganisms, NO3-N, available N, available P and catalase were significantly higher than type Ⅳ when the proportion of R. pseudoacia reached 40%. Acid phosphatase and urease were significantly higher than type Ⅳ when the proportion of R. pseudoacia reached 70%. 2) The pH, NO3-N, acid phosphatase and fungi were selected as the minimum data set (MDS). The soil quality index (SQI) of typeⅠ, type Ⅱ, type Ⅲ, type Ⅳ was 0.99, 0.78, 0.67 and 0.01, respectively. In general, all three types of plantations improved soil quality compared to type Ⅳ. With the increasing of the proportion of R. pseudoacacia, the soil quality was significantly better than that of pure P. tabulaeformis forest. When the proportion of R.pseudoacia reached 40%, the soil quality was improved significantly. But the soil quality was not improved significantly when the proportion of R. pseudoacacia continued to increase.[Conclusions] Comprehensive analysis shows that increasing the proportion of R. pseudoacacia can significantly improve the soil quality. Therefore, adjusting the proportion of R. pseudoacacia and maintaining the proportion at 40%-70% are suggested to improve the general fertility quality of forest stands.
2019 Vol. 17 (2): 87-93 [Abstract] ( 329 ) [HTML 1KB] [PDF 797KB] ( 484 )
94 WANG Xiong
Characteristics and potential ecological risk assessment of heavy metals in reclaimed land of a bauxite mine
[Background] The quality of reclaimed land restricts the value and use models of land. Ecological risk assessment is an important basis for the control and prevention of heavy metal contamination. The object of this paper is to study the content characteristics and potential ecological contamination risk of 6 heavy metals elements in farming soil of Xiaoyi bauxite reclaimed land, which have reclaimed for 10 years in 3 terrains of plain, gentle slopeland, and steep slopeland.[Methods] The soil samples in 0-20 and >20-40 cm layers from plain, gentle slopeland, and steep slopeland were collected. The contents of 6 heavy mental (As, Cd, Cr, Cu, Ni, and Pb) in both 0-20 and >20-40 cm of soil layers were measured using ICP-AES after acid digestion, and further the contents and distribution characteristics were analyzed. Finally, the contamination degrees and potential ecological risks of heavy metals were assessed using Hakanson potential ecological risk index. The data of heavy metal contents were mean values of three repetitions, and the calculation and analysis were conducted using software Excel 2010 and SPSS 13.0.[Results] 1) The concentrations of Cd and Pb presented that plain > gentle slopeland > steep slopeland in both of 0-20 cm and >20-40 cm layers, while the other 4 metals sbowed no certain change pattern in 0-20 cm. 2) At 3 different terrains and 2 soil layers, the degree of contamination ranged in 13.18-14.92, with an average 13.88, which was at medium contamination level. The potential ecological risk index ranged in 239.05-275.57, and average was 255.35, which were at a medium risk level. At 0-20 cm soil layer, the degree of contamination and potential ecological risk demonstrated as plain > gentle slopeland > steep slopeland, and as steep slopeland > plain > gentle slopeland in >20-40 cm soil layer. The Cd was the major contamination element and Pb was the second, while Cd at a high and Pb at a medium contamination level. The other 4 elements did not show contaminations and at a low potential ecological risk.[Conclusions] The contamination degree of heavy metals is higher in plain and gentle slopeland than in steep slopeland. As more human impact on plain land and gentle slopeland while steep slopeland is at a nature state, the slope effect on the heavy metal concentrations, contamination degree and potential ecological risk, and the influence gradually decreases with the reduction of slope.
2019 Vol. 17 (2): 94-102 [Abstract] ( 541 ) [HTML 1KB] [PDF 775KB] ( 460 )
103 WANG Zhen, WANG Keqin, ZHAO Yangyi, WANG Shuaibing, PENG Shuxian
Relation between plant community and soil factors of degraded woodland in hillslope: A case study of the Yizhe Watershed in the water resource area of Songhua dam
[Background] The water resource area of Songhua dam is an important drinking water source in Kunming City, 13 km northeast of the main city, located at 102°45'-102°59' east longitude, 25°08'-25°27' north latitude, and the drainage area is 629.8 km2, which guarantees more than 50% of the daily water supply in major cities in Kunming. The area is located in the eastern plateau, and 93.5% of the land area is mountainous and semi-mountainous, with an altitude of over 2,000 meters. The water conservation forests in mountainous areas are mostly single forest structures, built in the mid-1980s. The degradation of woodland area in protected areas now seriously affects the function of water resources protection. The contour reverse-slope terrace is an important manual intervention to regulate slope runoff. Then, under the long-term influence of this kind of artificial intervention, how will the secondary forest community structure and soil factors change? How will their relationship change? Understanding the relationship between the two under long-term manual intervention will help us evaluate the role of contour reverse-slope terraces scientifically, prevent water and soil loss and restore water conservation functions effectively in water resources.[Methods] This study was carried out in degraded woodland of Yizhe watershed in the Songhua dam. Three plots with contour reverse-slope terrace and three plots as a comparison were selected. Vegetation surveys were carried out on six plots at the end of the rainy season in 2017. The plant community characteristics of the plots were analyzed, after the plant community diversity was calculated and the important values of the species were sorted by model fitting method. At the same time, the soil samples of 0-40 cm surface soil were collected by three-point random sampling method according to the slope position. The canonical correspondence analysis (CCA) method were used to analyze the changes of soil environmental factors and plant community composition, and the corresponding qualitative relation.[Results] 1) Under the condition of long-term artificial intervention, the plant species Margalef richness (1.09), Pielou evenness index (0.87), Shannon-Wiener index (1.67) and Simpson index (4.49) were 2.51% to 9.00% higher. Among them, the important value of the best species increased to 25.49, and the herbaceous dominant species changed from Gramineae to Compositae, resulting in an increase in niche. 2) The presence of contour reverse-slope terrace resulted in the increasing of total soil porosity (50.48%), water content (20.45%), total nitrogen (4.47 g/kg), total phosphorus (3.99 g/kg) and available potassium (67.64 mg/kg). 3) Soil bulk density, total porosity, water content, organic matter, total nitrogen and total phosphorus were key environmental factors affecting the plant community structure of degraded forest land. Seven years of completing the contour reverse-slope terrace, the changes in soil bulk density and total porosity may be one of the reasons for the changes in plant community structure.[Conclusions] In general, the active artificial intervention measure may increase the vegetation diversity and the important plant value by improving soil bulk density and total porosity under the time scale, thereby promoting the degraded ecosystem to positive succession.
2019 Vol. 17 (2): 103-111 [Abstract] ( 514 ) [HTML 1KB] [PDF 879KB] ( 401 )
 
Development Studies
112 LI Yiran, ZHANG Xinggang, CHENG Tiantian, ZHANG Yongtao
Optimization of SCS model to estimate runoff in the mid-southern hilly region of Shandong province and evaluation of applying it
[Background] Runoff prediction is the basis of soil and water loss monitoring and prediction, and selecting suitable runoff prediction models for different regions can provide convenience for better soil and water conservation work in the river basin.[Methods] Based on the principle of SCS model, this study discussed the method of forecasting runoff for different land use types in the mid-southern hilly region of Shandong province. This study selected the runoff plots of four land use types (sloping farmland, level terrace, bare land and grassland) in the small watershed as the research object. Based on the data of runoff and rainfall observed in 2012-2015 years in the Yaoxiang small watershed, the initial loss rate and runoff curve number of the standard SCS-CN model and its modified form (MS model) in this area were calibrated by using the particle swarm optimization (PSO), then the optimized parameters were taken into the original model for runoff prediction, and the application results of initial model was compared with the optimized model. The measured runoff and other data in 2016 year were used to verify the models. Then the pass percent of model, the Nash-Sutcliffe efficiency coefficient (NSE), RMSE and the coefficient of determination (R2) were selected for evaluation indicators, and the model evaluation system was established based on the principle of TOPSIS method to quantitatively evaluate the application effect of different models.[Results] The application effect of standard SCS-CN model in four land use types was not applicable, and all evaluation indexes were deviated to a greater degree. The particle swarm optimization in 1stOpt software was used to optimize the standard SCS-CN model and MS model, forming the SCS-CNLes model and MSLes model, and the initial loss rate and runoff curve number in the optimized model had certain validity. In the model rate period and the model validation period, the application results of SCS-CNLes model and MSLes model were all fine, and the evaluation indexes of each model were higher than that of standard SCS-CN model. The TOPSIS comprehensive evaluation system was established for analysis. The result showed that the application effect of the MSLes model in the level terrace was the best, the qualified rate of the model was 100%, the NSE value was 0.70, the coefficient of determination was 0.77, and the RMSE value was 0.87. And followed by was the SCS-CNLes model in the grassland, the qualified rate of the model also was 100%, the NSE value was 0.53, the coefficient of determination was 0.83, and the RMSE value was 1.03.[Conclusions] The results show that MSLes model may be applied to forecast the actual runoff to some extent in the level terrace in the mid-southern hilly region of Shandong province, and relevant results can provide theoretical reference for follow-up research of runoff prediction in this area.
2019 Vol. 17 (2): 112-120 [Abstract] ( 344 ) [HTML 1KB] [PDF 2525KB] ( 557 )
 
Engineering Studies
121 YAN Shiyu, WANG Xiuru, WANG Xiao, HAN Xiaoliang
Accuracy analysis of model processing UAV remote sensing data: A case study of soil and water conservation monitoring for the Yellow River-to-Baiyangdian Water Transfer Project
[Background] The Unmanned Aerial Vehicle(UAV)remote sensing technology has provided a new technical mean for soil and water conservation monitoring in construction projects, especially in terms of the calculation of the area and volume of disposal ground, also greatly improved the efficiency and accuracy of monitoring. However, the accuracy of different models processing UAV remote sensing data varies a lot. Based on the Yellow River-to-Baiyangdian Water Transfer Project, this study selected 5 disposal grounds in Puyang, a city located in the plain area, as the research object. Since these 5 disposal grounds are similar in location and natural conditions, it is convenient for conducting comparative experiments and comparing the calculation accuracy of different models processing remote sensing data.[Methods] In this study, PhotoScan and Pix4D were used to process the UAV remote sensing data to obtain DOM and DSM images of each disposal ground. Global Mapper, LocaSpace Viewer and Context Capture were used to extract information from DOM and DSM images to calculate the area and volume of disposal grounds. Then 6 sets of models processing UAV remote sensing data were structured:Pho-Glo, Pho-Loc, Pho-Con, Pix-Glo, Pix-Loc and Pix-Con. Based on the actual value of construction organization, we quantified the errors of the area and volume of each disposal ground calculated by different models.[Results] 1) Using these 6 models:Pho-Glo, Pho-Loc, Pho-Con, Pix-Glo, Pix-Loc and Pix-Con, the calculation errors of disposal area were 5.57%, 5.05%, 4.84%, 1.69%, 3.06% and 1.23% respectively, and the errors of disposal volume were, 9.06%, 10.28%, 4.76%, 5.73%, 6.52% and 2.97% respectively. 2) When calculating the disposal area, using Pix4D for preliminary processing significantly reduced the error. There was no significant difference among Global Mapper, LocaSpace Viewer and Context Capture as for the information extraction. 3) When calculating the disposal volume, using Pix4D for preliminary treatment significantly reduced the error. There was no significant difference between Global Mapper and LocaSpace Viewer to calculate the volume of disposal grounds, while the accuracy of Context Capture was significantly higher than that of the others. 4) PhotoScan processed images more accurately when there was water on the surface and the DSM images were more consistent with the actual situation.[Conclusions] The accuracy of the 6 models are quite different, though all of them meet the requirements of relevant regulations. UAV has a bright application prospect in soil and water conservation monitoring for construction projects, which is more efficient and accurate than traditional monitoring methods when calculating the area and volume of disposal grounds. It is suggested that Pix-Con model processing UAV remote sensing data should be popularized in monitoring of construction projects.
2019 Vol. 17 (2): 121-131 [Abstract] ( 543 ) [HTML 1KB] [PDF 5603KB] ( 553 )
132 ZHOU Maorong, WANG Xijun
Influence of photovoltaic power station engineering on soil and vegetation: Taking the Gobi Desert Area in the Hexi corridor of Gansu as an example
[Background] During the construction of photovoltaic electric field, the excavation, dumping and rolling of the original surface inevitably destroy the soil and vegetation of the construction area. Through the study on the disturbance of soil environment and vegetation caused by the construction of photovoltaic power station, this paper tried to provide technical support for the ecological protection during the construction of photovoltaic power plant in the Gobi Desert Area in the Hexi corridor of Gansu.[Methods] The study took 6 typical photovoltaic power stations in Wuwei, Zhangye and Jiayuguan cities from east to west in the Gobi Desert Area in the Hexi corridor in Gansu as the research object. The disturbances of photovoltaic power station construction on soil environment and vegetation were studied by using the methods of field observation, inspection, and soil and water conservation monitoring data.[Results] 1) There was little difference in soil pH value, total nitrogen, total phosphorus, total potassium, organic matter and available phosphorus in the disturbed area between photovoltaic panels and the undisturbed area outside the photovoltaic power station, and the disturbance to the influence of soil nutrient was not obvious. 2) During the construction of photovoltaic electric field, the original vegetation and the surface crust were destroyed greatly, and the surface crust was damaged, which aggravated soil erosion and dust, and even caused dust storms. The destruction of vegetation reduced the coverage of vegetation and caused the deterioration of ecological environment and the decrease of plant population diversity. 3) During the operation period, the photovoltaic panel collected rainwater and the abandoned water for cleaning the photovoltaic panel, which increased the soil moisture content of the disturbed land between the photovoltaic panels and was conducive to vegetation restoration.[Conclusions] It is suggested that photovoltaic power station construction should give priority to photovoltaic modules with high photoelectric conversion efficiency, and spiral steel pipe pile foundation should be selected as the support foundation under geological conditions to reduce the disturbance range and intensity to the surface. The consciousness of environmental protection must be established in achieving the civilization construction.
2019 Vol. 17 (2): 132-138 [Abstract] ( 607 ) [HTML 1KB] [PDF 760KB] ( 565 )
 
Research Review
139 WANG Shanshan, LI Zhanbin, ZHANG Letao, MA Bo
Review on the off-site erosion effect of up-slope runoff and sediment
[Background] Up-slope runoff and sediment play an important role in energy deliver and sediment transport between the adjacent section. The change of up-slope runoff and sediment will affect the soil erosion process of down-slope. Thus, it is the vital content of soil erosion to study the up-slope runoff and sediment. However, previous studies mainly focused on the sediment sources of small watershed and the off-site depositional effects of up-slope runoff and sediment, while less studies focused on the off-site erosional effect of up-slope runoff and sediment.[Methods] This paper reviewed the study methods of the off-site erosional effect of up-slope runoff and sediment. Based on the previous research, the "off-site erosion" was firstly proposed in this paper. And then, it summarized the research achievements of predecessors. In terms of the characteristics of off-site runoff and sediment yield, the paper summarized the off-site erosional effect of up-slope runoff and sediment on the bare slope, and the research progress of the influence of soil and water conservation on the off-site erosional effect. Furthermore, it discussed the hotspots, challenges, and the future research directions of the off-site erosional effect.[Results] "Off-site erosion" refers to the change of downslope runoff characteristics and the sediment yield caused by up-slope runoff and sediment. The up-slope runoff and sediment joined into the down-slope and increased the runoff energy of down-slope. Besides, the runoff velocity, hydraulic radius, Reynolds number and Froude number increased, while resistance coefficient decreased. Based on the analysis of observed data and simulation experiments, the up-slope runoff and sediment would increase the sediment yield of down-slope. However, when the sediment concentration of runoff came to the sediment carrying capacity of runoff, the runoff with sediment couldn't erosive the down-slope soil, and even to deposit. The soil and water conservation measures on slope decreased runoff amount and sediment yield entering the down-slope. Some scholars thought soil and water conservation on slope decreased the off-site sediment yield, while others drew the opposite conclusion. Engineering measures, such as dams, drastically cut the runoff erosional energy, thus they had the decreased effect on off-site.[Conclusions] "Off-site erosion" is a relatively spatial concept, but how to reasonably define the up-slope and down-slope regions, there is still no clear definition. Up-slope runoff and sediment, erosion pattern evolution process and erosion process interacted with each other. Meantime, off-site erosional effect of up-slope runoff and sediment would be impacted by the dynamic change, such as rainfall intensity, underlying surface, sediment concentration and sediment carrying capacity. Further research of the off-site erosional effect of up-slope runoff and sediment could be conducted in confirming the concept of "off-site erosion", exploring the influence factors and mechanism of off-site erosion, illuminating the transfer characteristics of sediment and runoff energy during the off-site erosional process of up-slope runoff and sediment, as well as quantitating the off-site less erosional effect of soil and water conservation.
2019 Vol. 17 (2): 139-145 [Abstract] ( 459 ) [HTML 1KB] [PDF 745KB] ( 431 )
146 YE Luping, TAN Wenfeng, FANG Linchuan, ZHAO Wei
Research advances in spatial variability of soil aggregate by using geostatistics
[Background] Soil aggregate is to soil what cell is to organism. They have profoundly impacts on soil fertility and plant growth, and play important roles in soil resistance to erosion, soil remediation, and global carbon cycling, etc. The aim of this review is to find out the main issues in current researches, and provide an outlook of the potential for GIS and geostatistics application in spatial variability of soil aggregate.[Methods] We collected all relevant literature for this review. Based on these references, we reviewed the current development of spatial variability of soil aggregates by using GIS and geostatistics, analyzed spatial quantification methods and scale effects, summarized the factors influencing the spatial variation of soil aggregate, and the modeling of spatial variability prediction of aggregate stability.[Results] Current researches about geostatistics have made some progress in the spatial variability of soil aggregate. However, due to the spatio-temporal variability of soil properties, climate, topography, vegetation and human activities, the relevant researches need to be further studied. 1) At different spatial scales, the contribution of soil properties, natural factors, and human activities to the spatial variability of aggregate stability are unclear. 2) Some studies have used remote sensing data, DEM and other readily available data for spatial prediction of aggregate stability. The low spatial resolution cannot reflect the spatial variation in detail. Therefore, it is necessary to further improve the resolution of remote sensing data and predict the spatial variability of aggregate stability with a higher precision.[Conclusions] Previous studies placed emphasis on the formation process and stabilization mechanisms of soil aggregates at micro-scale. However, these micro-scale analyses cannot fully reveal the roles and functions of soil aggregates in ecosystems due to the fact that the eco-role of soil aggregate is affected by a combination of factors, such as soil properties, natural environment, and human activities, etc. In addition, the spatial heterogeneity in the aggregate structure and stability raises the difficulty in deriving the spatial pattern of soil aggregates with traditional classical statistics under real conditions, which makes geostatistics gradually be introduced in soil aggregates analysis. A large number of new methods and the continuous improvement of geostatistics are being applied to soil science. We should try to introduce the new analytical methods and models to analyze the spatial variability of soil aggregate. It is of great significance to study the formation process of aggregate, the influence factors of aggregate stability and the contribution of influence factors to aggregate stability, to understand the formation mechanism of aggregate, and to accurately explore the factors affecting the formation and stability of soil aggregate.
2019 Vol. 17 (2): 146-153 [Abstract] ( 616 ) [HTML 1KB] [PDF 2920KB] ( 420 )
中国水土保持科学
 
Notice on the Recruitment of Youth Editorial Board Members for the Journal of SSWC
Theme on Spreading Spirits of Great Scientists: LIANG Xi, the Founder of Forestry Education in China
ZHENG Fenli, CHEN Liding and LEI Tingwu in the list of Highly Cited Chinese Researchers by Elsevier
SSWC Indexed in the 2020 edition of “A Guide to the Core Journals of China”
Science of Soil and Water Conservation Accepted for Inclusion in Scopus
2020 Editor-in-Chief Meeting of Science of Soil and Water Conservation Held in Beijing, Concurrently
SSWC Selected to Be in Core Library of Source Journals of CSCD during 2019-2020
SSWC Indexed in the 2017 edition of “A Guide to the Core Journals of China”
Appreciation for peer reviewer of SSWC Editorial Board
2017 Editor-in-Chief Meeting of Science of Soil and Water Conservation Held in the Yangling of Shaan
Professor Wang Lixian, Former Editor-in-Chief of SSWC Won Norman Hudson Memory Award
Calls for Papers in English
Deputy Editor-in-Chief Cui Peng Elected as a Member of 9th National Committee of CAST
Three Members of SSWC Editorial Board Rewarded as NOSTW in 7th Session Assessment
Election of 4th Editorial Board and First Meeting of New Board Held in Beijing
Deputy Editor-in-Chief of SSWC, Academician Cui Peng elected as a member of the IRDR SC
Notice About The 5 Not-Allowed Rules While Publishing Academic Articles by 7 Organizations
SSWC Indexed in “A Guide to the Core Journals of China”
Science of Soil and Water Conservation Calls for Papers
SSWC Selected to Be in Core Library of Source Journals of Chinese Science Citation Database During
On the Home Page of the Journal Science of Soil and Water Conservation
Five Papers of Science of Soil and Water Conservation Determined as Excellent in 5th Assessment
Congratulations to Deputy Editor-in-Chief Cui Peng Elected as Academician of Chinese Academy of Scie
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