Effect of time resolution of rainfall measurements on the erosivity factor in the USLE in China

Rainfall erosivity, one of the factors in the Universal Soil Loss Equation, quantifies the effect of rainfall and runoff on soil erosion. High-resolution data are required to compute rainfall erosivity, but are not widely available in many parts of the world. As the temporal resolution of rainfall measurement decreases, computed rainfall erosivity decreases. The objective of the paper is to derive a series of conversion factors as a function of the time interval to compute rainfall erosivity so that the R factor computed using data at different time intervals could be converted to that computed using 1-min data. Rainfall data at 1-min intervals from 62 stations over China were collected to first compute the ‘true’ R factor values. Underestimation of the R factor was systematically evaluated using data aggregated at 5, 6, 10, 15, 20, 30, and 60-min to develop conversion factors for the R factor and the 1-in-10-year storm EI₃₀ values. Compared with true values, the relative error in R factor using data at fixed intervals of ≤10min was <10% for at least 44 out of 62 stations. Errors increased rapidly when the time interval of the rainfall data exceeded 15 min. Relative errors were >10% using 15-min data for 66.1% of stations and >20% using 30-min data for 61.3% of stations. The conversion factors for the R factor, ranging from 1.051 to 1.871 for 5 to 60-min data, are higher than those for the 1-in-10-years storm EI₃₀, ranging from 1.034 to 1.489 for the 62 stations.     

基于InVEST模型的祁连山国家级自然保护区土壤保持现状与功能

运用InVEST模型,对甘肃祁连山自然保护区土壤保持现状与功能进行了定量评估,分析了不同土地利用、海拔高度、坡度以及土壤类型下的保土状况。结果表明:2015年甘肃祁连山自然保护区土壤侵蚀量与土壤保持量分别为1. 67×10^8t、4.21×10^8t。从侵蚀面积来看,保护区以微度和轻度侵蚀为主,占总面积的63.95%;虽草地的土壤保持能力弱于其他自然植被类型,但草地是土壤保持总量最高的土地利用类型;不同海拔梯度下的土壤保持总量随海拔增加呈现先增后减的趋势,保护区内海拔2 500~3 500 m的土壤保持功能最好;栗钙土的土壤保持量最高,黑毡土在草原土壤类型中土壤保持强度较低;坡度为15°~25°的区域土壤保持量最大,占土壤保持总量的31.93%;甘肃祁连山保护区生态系统减少泥沙淤积和减少土地废弃的价值分别为5. 76×10^8元和1. 44×10^8元,保护区内林草地保肥价值为9. 03×10^10元。     

Assessing the effects of vegetation and precipitation on soil erosion in the Three-River Headwaters Region of the Qinghai-Tibet Plateau,China

Soil erosion in the Three-River Headwaters Region (TRHR) of the Qinghai-Tibet Plateau in China has a significant impact on local economic development and ecological environment. Vegetation and precipitation are considered to be the main factors for the variation in soil erosion. However, it is a big challenge to analyze the impacts of precipitation and vegetation respectively as well as their combined effects on soil erosion from the pixel scale. To assess the influences of vegetation and precipitation on the variation of soil erosion from 2005 to 2015, we employed the Revised Universal Soil Loss Equation (RUSLE) model to evaluate soil erosion in the TRHR, and then developed a method using the Logarithmic Mean Divisia Index model (LMDI) which can exponentially decompose the influencing factors, to calculate the contribution values of the vegetation cover factor (C factor) and the rainfall erosivity factor (R factor) to the variation of soil erosion from the pixel scale. In general, soil erosion in the TRHR was alleviated from 2005 to 2015, of which about 54.95% of the area where soil erosion decreased was caused by the combined effects of the C factor and the R factor, and 41.31% was caused by the change in the R factor. There were relatively few areas with increased soil erosion modulus, of which 64.10% of the area where soil erosion increased was caused by the change in the C factor, and 23.88% was caused by the combined effects of the C factor and the R factor. Therefore, the combined effects of the C factor and the R factor were regarded as the main driving force for the decrease of soil erosion, while the C factor was the dominant factor for the increase of soil erosion. The area with decreased soil erosion caused by the C factor (12.10×10³ km²) was larger than the area with increased soil erosion caused by the C factor (8.30×10³ km²), which indicated that vegetation had a positive effect on soil erosion. This study generally put forward a new method for quantitative assessment of the impacts of the influencing factors on soil erosion, and also provided a scientific basis for the regional control of soil erosion.     

超高效液相色谱-质谱/质谱法同时测定蔬菜中7种磺胺的残留量

为建立超高效液相色谱-质谱/质谱法(UPLC-MS/MS)同时测定蔬菜中7种磺胺残留量的方法。样品用1%乙酸乙腈提取，以C18色谱柱分离待测物，采用多反应监测(MRM)离子扫描模式，外标法进行定量，线性良好，相关系数均大于0.999。结果显示：7种磺胺的检出限为0.000 4～0.000 6 mg/kg，样品添加回收率为67.5%～94.1%，相对标准偏差均少于5.3%(n＝6)。该方法简单快捷、定量准确，可满足多种蔬菜中7种磺胺的残留检测要求。     

An investigation into the grazing efficiency of perennial ryegrass varieties

The objective of this study was to compare the grazing efficiency of 30 perennial ryegrass varieties, differing in ploidy and heading date. Plots were grazed by lactating dairy cows and managed under a rotational grazing system with 19 grazing events occurring over two years. Pre-grazing and post-grazing compressed sward heights were measured with a rising plate meter. A mixed model was used to predict the post-grazing sward height of each variety based on year, grazing event, block and pre-grazing sward height. Residual grazed height (RGH) was derived as the difference between the actual and predicted post-grazing sward height and was used as the measure of grazing efficiency. Negative RGH values indicated that the actual herbage removed was greater than that predicted and so indicated a superior grazing efficiency. Varieties differed in their level of grazing efficiency (p < .001), with RGH values ranging from −0.38 to +0.34 cm. Tetraploid varieties exhibited significantly greater grazing efficiency performance than diploids (p < .001), with average RGH values of −0.13 and +0.13 cm respectively. A significant difference in grazing efficiency was found among recommended perennial ryegrass varieties that are not being recorded by mechanically harvested simulated grazing protocols. A variety reappraisal that included grazing efficiency could identify varieties capable of improving on-farm livestock productivity from grass.     

不同饲料效率与绵羊瘤胃组织形态学关系

【目的】利用单栏系统测定个体的饲料效率相关性状与瘤胃组织形态学指标,探讨绵羊饲料效率与瘤胃组织形态的关系,为解析绵羊饲料效率性状的影响因素研究提供基础数据。【方法】随机选取出生日龄相近、系谱信息详细、健康状况良好的187湖羊公羔,56 d断奶后转入单栏饲养,过渡期14 d,预饲期10 d,正试期100 d。正试期内所有羊只仅饲喂颗粒饲料,自由采食及饮水,并在80 d和180 d晨饲前空腹测定其体重（body weight,BW）和80—180 d间的采食量（feed intake,FI）,计算平均日增重（average daily gain,ADG）、中期代谢体重（metabolic body weight, MBW）、饲料转化率（feed conversion rate,FCR）和剩余采食量（residual feed intake,RFI）等饲料效率相关性状并对其进行描述性统计,于180 d饲养结束后屠宰采集瘤胃腹囊组织1 cm²保存于4%甲醛溶液中,用于制作组织切片并观测其瘤胃乳头长度、宽度和肌层厚度。最后将其与饲料效率相关性状进行相关分析和方差分析。【结果】饲料效率相关性状的变异系数均大于10%,且剩余采食量最大与最小的个体每天的剩余采食量之差达0.57 kg。饲料效率相关性状间的表型相关分析表明剩余采食量与饲料转化率（r= 0.68）和采食量（r= 0.48）呈极显著正相关（P<0.01）,与初始体重（r=0）、末期体重（r= -0.01）和平均日增重（r= -0.02）无显著相关（P>0.05）。饲料效率相关性状与瘤胃组织形态相关性分析发现,瘤胃乳头长度与平均日增重、采食量、初始体重和末期体重呈显著或极显著正相关（P<0.05或P<0.01）,肌层厚度与平均日增重、采食量和末期体重呈显著或极显著正相关（P<0.05或P<0.01）,而剩余采食量和饲料转化率与瘤胃组织形态无显著相关。不同RFI组羔羊采食量、饲料转化率和瘤胃肌层厚度存在显著或极显著差异（P<0.05或P<0.01）,瘤胃乳头长、宽无显著差异（P>0.05）,其中High-RFI组羔羊采食量和饲料转化率极显著高于Low-RFI组（P<0.01）,肌层厚度显著高于Medium-RFI组（P<0.05）;不同FCR组羔羊的剩余采食量、采食量、ADG、初始体重、末期体重和乳头长度存在显著或极显著差异（P<0.05或P<0.01）,肌层厚度和乳头宽度差异不显著（P>0.05）,其中High-FCR组羔羊剩余采食量、采食量、ADG、初始体重和末期体重均显著或极显著高于Low-FCR组（P<0.05或P<0.01）,Medium-FCR组羔羊乳头长度显著长于Low-FCR组（P<0.05）;除瘤胃乳头宽度外,不同FI组羔羊的上述指标均存在显著或极显著差异（P<0.05或P<0.01）,且High-FI组羔羊的剩余采食量、饲料转化率、ADG、初始体重、末期体重、肌层厚度和乳头长度均显著或极显著高于Low-FI组（P<0.05或P<0.01）;不同ADG组羔羊采食量、饲料转化率、初始体重、末期体重和肌层厚度均存在显著或极显著差异（P<0.05或P<0.01）,乳头长度和乳头宽度无显著差异（P>0.05）,其中High-ADG组羔羊采食量、剩余采食量、初始体重、末期体重和肌层厚度均显著或极显著高于Low-ADG组,饲料转化率则极显著低于Low-ADG组。【结论】剩余采食量与采食量和饲料转化率等饲料效率性状呈极显著正相关,表明其可作为衡量饲料效率的潜在指标。剩余采食量和饲料转化率与瘤胃组织形态学指标无显著相关,采食量和平均日增重与瘤胃乳头长度和肌层厚度呈显著正相关,表明羔羊瘤胃组织形态对采食量和增重有显著影响,但其进一步的作用机制有待深入研究。     

土壤侵蚀下黑龙江省人地系统适应性研究

为缓解人地关系,以对黑龙江省威胁最大的土壤侵蚀为切入点,从"三生"视角分析区域人地系统适应性,并提出基于不同修复优先级的人地系统修复方案。首先,在总结、梳理适应性内涵,整合适应性理论与方法基础上,从"三生"视角提出了基于风险扰动的适应性分析框架,将系统适应性分解为扰动、影响、响应、能力4方面,并从土壤侵蚀风险扰动出发,构建了系统适应性评价指标体系与评价模型;其次,采用极差标准化法、克里格插值法、蔡崇法法和DEA-CCR模型处理数据,利用土壤侵蚀方程测算土壤侵蚀风险,利用适应性评价模型测算适应性指数,分析土壤侵蚀风险和人地系统适应性分布情况;最后,提出基于不同修复优先级组合模式的人地系统修复方案。结果表明:黑龙江省土壤侵蚀风险区面积为1 366.61万hm2,占区域耕地面积的85.74%,高、中、低级别风险规模分别为324.02、596.33、446.26万hm2。高、较高级别人地系统适宜程度区分布在三江平原东北部和松嫩平原东南部地区,中级别分布在大兴安岭和松嫩平原南部地区,低、较低级别分布在东南部山地和松嫩平原北部地区。形成了基于不同修复优先级组合模式的人地系统修复方案,其中53个地区仅存在1种人地系统修复方案,其余27个地区在不同优先级组合模式下形成了不同的人地系统修复方案,为区域人地系统修复提供了多种选择方案。     

黄麻土工布覆盖对花岗岩红壤表土坡面侵蚀特性的影响

[目的]探究黄麻土工布覆盖条件下花岗岩红壤表土坡面侵蚀特性,为花岗岩红壤区坡面土壤侵蚀防治提供科学依据。[方法]通过室内模拟降雨试验,在2个坡度(5°和15°坡度)、3种密度(无覆盖,6 cm×6 cm及3 cm×3 cm网格)的黄麻土工布覆盖条件下,研究极端降雨条件下(90 mm/h)花岗岩红壤表土的坡面侵蚀特性,并观测径流系数、土壤侵蚀速率、泥沙颗粒变化规律及富集率等指标。[结果]坡面径流随降雨历时增加而增加,土壤侵蚀速率则相反,表明侵蚀过程是一个分离受限的过程。和对照组相比,黄麻土工布覆盖在不同试验条件下都具有明显的减流减沙作用。另外,由侵蚀泥沙的粒径分选规律可知,坡面土壤中的黏粒和粉粒大小的颗粒倾向于被优先选择性搬运,其结果致使坡面石英粗颗粒富集,在缓坡(5°)与高密度黄麻土工布覆盖条件下(3 cm×3 cm网格)尤为突出。坡面石英粗颗粒随降雨历时增加不断富集进一步增加了原位坡面的侵蚀抗性,产生了土壤侵蚀速率随降雨历时不断降低的现象。[结论]高密度黄麻土工布的覆盖能够有效地减流减沙,增加原位坡面抗蚀性,是一种有效的水土保持措施,在今后的土壤侵蚀防治和劣地恢复工作中应该被重视。     

中国东北漫川漫岗典型黑土区沟道侵蚀特征

[目的] 通过对450 km²黑土区进行实测调查，旨在评估研究区沟道侵蚀现状。[方法] 选取沟道侵蚀严重的450 km²的漫川漫岗黑土区为调查区域，首先在谷歌卫星影像上进行侵蚀沟识别和定位，再对侵蚀沟立体形态进行实地测量。[结果] ①研究区土地利用以耕地为主，耕地、建设用地、林地、草地分别占研究区总面积的85%，8%，6%，1%。②研究区坡耕地占86%，坡度0.25°~3.0°占64%，大于5°的占12%。③共有侵蚀沟1 049条，其中耕地中侵蚀沟577条，占总侵蚀沟条数的55%；沟壑密度1.2 km/km²，按沟壑密度衡量沟蚀强度为中度；沟壑面积比例为2.89%，以此界定沟蚀强度为剧烈。④研究区侵蚀沟平均长度、宽度、深度和面积分别为996，13.1，2.7 m和2.4 hm²。[结论] 漫川漫岗黑土区沟道侵蚀严重，主要危害坡耕地，但侵蚀沟相对较小，易于治理。     

华北平原地下水压采区冬小麦种植综合效应探讨

华北平原冬小麦-夏玉米一年两熟种植模式为维护国家粮食安全发挥了重要作用。但冬小麦生长期正处于华北平原降水较少的干旱季节,实现高产依赖于灌溉,是华北平原地下水超采的主导因素之一。随着国家地下水限采政策的实施,在地下水超采区如何稳定冬小麦的种植面积和产量是面临的一个重要问题。本文通过综述以往研究并结合典型地点田间试验结果,从冬小麦种植可减少休闲期土壤蒸发损失、具有的深根系系统可充分利用土壤储水、可利用微咸水替代淡水灌溉、通过限水灌溉发展优质麦生产、冬春形成覆盖层美化和防沙尘效应等方面论述了华北平原种植冬小麦的优势,提出华北平原冬小麦生产需要转变传统高耗水高产量理念,充分发挥冬小麦抗旱、耐盐能力强的特点,在不实施大规模压缩冬小麦种植面积条件下,通过冬小麦限水灌溉和微咸水利用满足对地下水压采需求,充分发挥华北平原冬小麦种植冬春防风沙、美化环境的生态功能,同时满足区域口粮安全的保障功能。